Wednesday, January 27, 2010

Whitewater GUSHES - January THAW 2010

Misty vapors rise above the rock filled chasm of
Class V+ ( super-extreme ) South Fork Gorge.

January 25, 2010
South Fork Gorge of High Knob Massif
Photograph by Roddy Addington - © All Rights Reserved.

Turbulent, churning whitewater gushed downward through awesome depths of South Fork Gorge as pristine water drained lofty Big Cherry Basin of the High Knob Massif during a break from winter's frozen grip upon its highcountry domain!

Captured by photographer Roddy Addington during January 25, only twelve days removed from 1-2+ FEET of snow depth ( an atypically LONG thaw during what promises to be a HARSH winter amid the southern Appalachians ).

High Knob Massif
South Fork of Powell River
Whitewater & Rocks - January 25, 2010
Photograph by Roddy Addington - © All Rights Reserved.

Dropping 1433 vertical feet in 4 miles
1069 feet during its final 2 miles, and containing two sections having max gradients up to 800+ feet per mile, great South Fork Gorge possesses one SUPER-TIGHT and SUPER-EXTREME steep creek!

[ Its only EYE CANDY for whitewater kayakers at the moment, as even before a MAJOR December 2009 snowstorm downed more trees it was FULL of wood!

But its there, and the POTENTIAL is real, VERY REAL, despite the hold back of large volumes of water by Big Cherry Dam ].

Between 80" and 90" of total precipitation fell across Big Cherry Basin during 2009 to keep water overflowing the Dam nearly all year.

Based upon City of Norton records, the wettest 12-month period since the early 1980s would have produced 90-100" across Big Cherry Basin, so 2009 was NOT a record wet year.

[ The above being gage caught precipitation, as the TRUE moisture budget of this highcountry basin is MUCH greater via FOG DRIP from trees, RIME deposition on trees, and the obvious loss of gage measurable precipitation due to wind driven precip ( reducing what is recorded digitally and by hand ) ].

Gushing thaws from deep winter snowpacks are not uncommon.

Reference the following section of this website for another example:

January 25, 2010
Most Tranquil Stretch In South Fork Gorge?
Photograph by Roddy Addington - © All Rights Reserved.

**For more incredible Roddy Addington WHITEWATER shots please reference:

This most recent rainfall event of Jan 24th, generated 7 to 8 vertical feet of total rise on both the Powell & Clinch rivers ( world-class biodiversity hotspots), downstream of whitewater creeks draining the High Knob Massif in Lee and Scott counties of southwestern Virginia.

Little Stony Basin of Clinch River
Big Falls - Little Stony Gorge of High Knob Massif
Photograph by Johnny Stanley - © All Rights Reserved.

Little Stony Gorge contains one of the most complete whitewater runs in the eastern United States, with Class IV-V+ rapids draining a 16.4 square mile watershed with more than 2100 vertical feet of total relief ( Little Stony Basin ).

[ Little Stony Gorge lies approximately 15 air miles E to ENE of South Fork Gorge, adjacent to majestic Guest River Gorge and the eastern end of the High Knob Massif ].

The Big Stony Basin multi-gorge wonder complex is situated in between South Fork Basin and Little Stony Basin, with 42 square miles of terrain so remote and rugged that few photographs ( of high quality ) even exist to illustrate its nearly 3000 vertical feet of total relief ( it is drained by extremely steep whitewater creeks amid Straight Fork Gorge, Chimney Rock Gorge, and Mountain Fork of Big Stony Gorge ). 

Up to 3.00"+ of rain accumulated along the Cumberland Mountain arm of the High Knob Landform ( HKL ), across Cumberland Gap National Historical Park, during January 24 to help boost the Cumberland River into minor flooding.

Calcareous Core of High Knob Landform
South Fork Gorge from Powell Valley Floor
Photograph by Roddy Addington - © All Rights Reserved.

South Fork Gorge rises upward and twists back behind mountain walls visible in the above scene, themselves being MUCH lower than highcountry crestlines which sprawl outward across the massif, to generate a watershed with nearly 2800 vertical feet of total relief ( South Fork of Powell Basin ).

[ The South Fork of the Powell River drains 41 square miles of the High Knob Massif on the Wise County side of the highcountry.  Collectively, the Big Stony Basin, Little Stony Basin, and South Fork Basin contain 99.3 square miles ( many more basins are present within the domain of the great High Knob Massif ) ].

Rising Into The Heavens - January 22, 2009
Photograph by Roddy Addington - © All Rights Reserved.

The High Knob Massif can handle more total precipitation, without flooding ( rainfall and/or rain + snow melt ), than other locations across western Virginia since most creeks draining its highcountry sink, or partially sink, into the subterranean prior to reaching regional base levels marked by the Clinch and Powell rivers.

Reference "The High Knob Landform" to learn more about these world-class karst systems

Another factor making the High Knob Massif unique to Virginia, and the southern Appalachians, is that many of its higher elevation basins have lakes and wetlands which themselves hold back much water from direct run-off into creeks.

A Few Notable Ones Include:
High Knob Basin Wetland: 3500'+
High Knob Lake: 3490'
Upper Norton Reservoir: 3308'
Lower Norton Reservoir: 3230'
Cliff Mountain Ponds: 3155-3205'
Big Cherry Basin Wetlands: 3125-3200'
Big Cherry Lake: 3120'
Wolf Creek Wetlands of Stock Creek: 3000'
Glady Fork Wetlands of Big Stony Basin: 2900'
Robinson Fork Wetlands: 2740'+
Bark Camp Lake: 2734'

[ There are numerous additional small ponds, wetlands, and seepages within the High Knob Massif on both private and USFS public lands ].

Cloud Vapor Gathering Above Massif - January 25
Photograph by Roddy Addington - © All Rights Reserved.

Once very extensive underground conduit systems become full of water, lakes and wetlands fill and overflow, extremely flashy situations can then develop with excessive rainfall, rapid snow melt, or a combination of rainfall + snow melt.

This makes the High Knob Landform hydrologically complex, with flooding more often than not being associated with rapid water level rises during flashy events ( the obvious exceptions being downstream along the Clinch and Powell rivers, which take longer to reach peak levels, and during historic events like the great floods of February 1862, January 1957, and the benchmark disaster of April 1977 ).

Changing Conditions - January 25, 2010
Photograph by Roddy Addington - © All Rights Reserved.

A distant snow shower obscures part of the lofty highcountry, as a hole opens in the overcast above Powell Valley to reveal PUFFY clouds rising vertically into blue heavens!

[ Some of these clouds generated lightning & thunder, with localized THUNDERSNOW during late afternoon hours of January 25 in parts of Wise and Dickenson counties ].

Rainbow Across The Valley - January 25, 2010
Photograph by Roddy Addington - © All Rights Reserved.

Majestic and unusual looking rainbows were also part of weather conditions observed, as the THAW gave way to returning cold air.

Majestic Double Bows Grace Lee County
Photograph by Harold Jerrell - © All Rights Reserved.

My friend Wayne Riner captured one of the most unusual looking rainbows amid the highlands of southern Dickenson, adjacent to the High Knob Landform.

Burst of Morning Color - January 25, 2010
Photograph by Wayne Riner - © All Rights Reserved.

Wayne described the scene in his own words:

"While in the yard, I noticed a burst of color on a distant ridge. This was the only part of the rainbow that was visible. There were rain showers and sun in the area at the time. I felt it was very odd to see such a bright patch of color and no other sign of the rainbow."

A most glorious ending to January THAW 2010!

This website update is dedicated to the wonderful, beautiful Gladys Stallard, who turns 97 years young today ( January 27 ).

Happy Birthday Gladys!

May you have MANY more.

Rainbow - Cumberland Gap National Historical Park
Photograph by Harold Jerrell - © All Rights Reserved.

Thursday, January 14, 2010

Belated Christmas Present: Winter Beauty

High Knob Massif - January 6, 2010
Photograph by Roddy Addington - © All Rights Reserved.

The High Knob Landform

Given that most in Wise, Dickenson, and adjoining locations did not have much of a Christmas in 2009, I thought we would enjoy some of the majesty of this season!

[ Most would likely rather see sandy beaches and palm trees, at this point, but we are still thankful for what we have and the scenes presented in this update are certainly inspirational ].

At least, you can LOOK at them and ENJOY
without getting out in the COLD!

Although not yet up to the legendary status of late 1970s winters, or some farther back in time, the 2009-10 season will certainly be one to remember!

January 13, 2010
Remnant Massif of The High Knob Landform
High Knob Highcountry Flanking Powell Valley
Photograph by Roddy Addington - © All Rights Reserved.

Great mountain walls of the High Knob Massif tower above Powell Valley in Wise County, Va., as captured by Roddy Addington during afternoon hours of January 13, 2010.

Capped by RIME and DEEP snow, the highcountry spreading outward from the above scene extends 17 air miles eastward until it plunges into depths of rugged Guest River Gorge ( the 40 to 50+ square mile portion of the massif extending southwestward from great South Fork Gorge, sometimes called the Powell Mountain block, not included in the above eastward expansion of the mass ).

[ NOTE: The U.S. Forest Service reports that trails within the Little Stony Gorge, Guest River Gorge, and Roaring Branch Gorge are ALL CLOSED due to the December 18, 2009 winter storm.

Other trails and portions of the National Forest may also need closing once weather conditions improve enough for a complete inspection of the situation ].

The above scene is both striking and educational since it reveals an EXTREME climatic gradient that exists throughout the year, but is most visible to the eyes in winter!

Caked In Multiple Layers Of "Hard Rime"
High Knob Peak - January 6 - Before 14" of New Snow
Photograph by Roddy Addington - © All Rights Reserved.

My friend Joe Fields measured 13" to 16.5" of snow depth at his home in High Chaparral of High Knob during morning hours of January 13, at 3300 feet elevation, amid a location possessing a SOUTHERN exposure ( compare with snow depth on Valley floor above at around 1660 feet elevation ).

My friend Roddy Addington drove across a portion of the High Knob highcountry during the late afternoon of January 13, and reported 12"+ of snow depth still IN THE ROAD.  That from recent fluffy snowfall which has settled over time.

North slope depths in upper portions of the High Knob Lake, Big Cherry Lake, and adjacent lofty northern exposed basins of the massif have consistently been 10" to 12"+ deeper than those possessing southern exposures within the High Chaparral area, ever since the great MEGA-dump snowstorm of December 18, 2009.

Awesome Mountain Walls of High Knob Massif
 Photograph by Roddy Addington - © All Rights Reserved.

[ Snow depths on the morning of December 19, 2009 varied from 2 feet in the Robinson Knob to High Chaparral communities of the highcountry, to around 3 feet ( with 4-5+ foot drifts ) within the Eagle Knob, Camp Rock, Little Mountain, Grindstone Ridge Dome to Thunderstruck Knob corridor of the massif ].

Such HUGE snow depth variations are simply incredible and often hard for those living on the floor of majestic Powell Valley, nestled amid the great calcareous heart of the High Knob Landform, to truly comprehend!

Even within the Valley there has been a distinct and notable snow depth gradient since mid-December, with the Valley Head having MUCH more snow depth than its Big Stone Gap end.

Head of Powell Valley - January 13, 2009
Photograph by Roddy Addington - © All Rights Reserved.

By design or pure magic, the RIME level capping the massif often begins along upper edges of the great belt of calcareous cliffs which ring its steep mountain walls for more than 50 air miles.

Grindstone Ridge Dome - Cliffs & RIME
Photograph by Roddy Addington - © All Rights Reserved.

The vertical drop of Grindstone Ridge Dome ( on right of above picture ) is one of the greatest short-distance descents along the entire western expanse of the Appalachians, with 2000 feet of plunge within only 0.8 air mile!

Such great short-distance vertical changes in elevation are only one of many factors supporting the HUGE climatic gradients of the High Knob Massif, contributing to such unique features as the orographically forced and anchored Thermally Indirect Mesoscale Circulation associated with the MEGA snow dump of December 18, 2009.

Morris Butte of Powell Mountain - High Knob Massif
Photograph by Roddy Addington - © All Rights Reserved.

Miles southwest of Grindstone Dome is another large vertical descent, beneath the very rugged cliff-lined peak of Morris Butte which towers above the great southwestern front of South Fork Gorge.

Although RIME has now dropped off to enrich the melting highcountry snowpack, it built up over time via multiple riming days to thicknesses of more than 6 inches in places.

[ Up through January 15 the highcountry snowpack had settled significantly, with rime input acting to increase its total water content which, via settlement, is becoming more concentrated over time into lesser depths ].

Thick RIME & Deep Snow - January 6
Photograph by Roddy Addington - © All Rights Reserved.

MUCH more rime and snow accumulated across upper elevations in the massif after Roddy took these photographs.

Highcountry Highway - State Route 619
Photograph by Roddy Addington - © All Rights Reserved.

Of all the many amazing things I've learned about the High Knob Landform in the past 22+ years of research, the one thing which stands out most is that EVERYTHING within its natural world is connected in intimate and direct ways!

[ I feel nearly ashamed to state the above, since that should be so OBVIOUS to anyone with keen senses.  Native Americans understood this long before the "white man" came along, which is likely the reason I have such high respect for their cultures ].

High Knob Massif - January 6, 2010
Endemic Southern Appalachian Northern Hardwoods
Photograph by Roddy Addington - © All Rights Reserved.

That upper edges of the great calcareous cliff lines mark a MEAN riming level is no accident since that also marks a major zone of climatic transition into an ecosystem where winters become much more harsh, with deeper snows, higher wind speeds, lower wind chills, and much more stress on living things trying to balance out a heat budget!

The above being especially true in places where the environment has not been GREATLY altered by man, and is the NATURAL tendency of nature in the High Knob Massif when left alone by mankind ].

Jefferson National Forest
RIME Against Highcountry BLUE
Photograph by Roddy Addington - © All Rights Reserved.

While the above could be stated of most major mountain locations on earth, there are important differences amid the High Knob Massif which are driven by its great climatic gradients, themselves a product of unique orographically forced circulations arising on southwesterly and easterly air flow trajectories. 

[ Upslope snowfall enhanced by southwesterly air flows, and occasionally by the Thermally Indirect Mesoscale Circulation most recently highlighted on easterly air flow trajectories, are merely two examples of how the High Knob Massif interacts with the overlying atmosphere to generate special conditions which over the LONG-term make it climatically unique to southwestern Virginia.  This, in turn, impacts its biodiversity ].

WOW - High Knob Massif - January 6, 2010
Photograph by Roddy Addington - © All Rights Reserved.

In the BIG picture, orographically driven gradients in climate work to support and enhance the great biodiversity of the High Knob Landform, from its remnant massif of highcountry & calcareous core to its rugged mountain flanks containing majestic Cumberland Gap National Historical Park and other grand natural features.

DEEP Snow ( Jan 6 ) Prior To 14" of New Snowfall
Photograph by Roddy Addington - © All Rights Reserved.

Reference the High Knob Landform Introduction 
on this website for more information:

In the BIGGER picture, orographically driven climatic gradients across the great High Knob Landform work to enhance those of the entire Upper Tennessee River Basin.

Beartown Mountain Panorama - January 7, 2010
Photograph by Richard Kretz - © All Rights Reserved.

My friend and naturalist Richard Kretz reports that a scattering of Red Spruce ( Picea rubens ) trees, capping the lofty 4672 foot summit of Russell Beartown Mountain, support a small winter population of beautiful Red Crossbills ( Loxia curvirostra ) and White-winged Crossbills ( Loxia leucoptera ) that feed on their pine seeds.

This collectively forms the rarity and richness of biodiversity for which the Upper Tennessee River Basin is renowned, uniting the major High Knob Landform with its Clinch River Valley and upper basin along magnificent Clinch Mountain ( this includes such extraordinary places as The Pinnacle NAP, Brumley Mountain, Beartown Mountain, and Garden Mountain ).

Majestic Elk Garden Road - Russell County
Photograph by Richard Kretz - © All Rights Reserved.

An old weathered barn marks a typical stretch of rolling landscape within the ecologically rich Clinch River Valley of southwestern Virginia.

Increasing Clouds Foreshadow More Snow - Jan 7
Photograph by Richard Kretz - © All Rights Reserved.

Winter 2009-10 has been hard on our feathered friends, but Harold Jerrell found some fine looking guys and gals!

White-throated Sparrow ( Zonotrichia albicollis )
Photograph by Harold Jerrell - © All Rights Reserved.

White-throated Sparrows winter in the mountains
and typically stay until early May, before heading north into the
Great Lakes and Canada for their summer breeding season.

I love their vocalizations!

Blue Jay ( Cyanocitta cristata )
Photograph by Harold Jerrell - © All Rights Reserved.

Rowdy Blue Jays are year-round residents with mass migrations into deep mountain hollows and cold air drainages dominated by American Beech ( Fagus grandifolia ) during autumn to eat beech nuts!

Northern Cardinal - Catching A Breeze
Photograph by Harold Jerrell - © All Rights Reserved.

A female Northern Cardinal ( Cardinalis cardinalis ) catches a stiff breeze from Ole Man Winter.

The Northern Cardinal is Virginia's state bird, and the male of the species struts his stuff for Harold's camera!

Male Northern Cardinal In Snow
Photograph by Harold Jerrell - © All Rights Reserved.

Are they posing for the camera?

Male Cardinal Posing - I'm The Prettiest!
Photograph by Harold Jerrell - © All Rights Reserved.

No I Am - Even With Snow On My Beak!!
Photograph by Harold Jerrell - © All Rights Reserved.

No, I don't think so!

They are strutting for those cute
Ladies, no doubt!

I think that says Harold Jerrell down there!
Photograph by Harold Jerrell - © All Rights Reserved.

We probably take Northern Cardinals for granted since they are such abundant residents; however, they are a gorgeous bird and add greatly to our mountain landscape.

Tufted Titmouse ( Parus bicolor )
Photograph by Harold Jerrell - © All Rights Reserved.

Tufted Titmouses are also common year round residents
which add greatly to our backyards with their territorial singing and fisty behaviors!

American Goldfinch ( Carduelis tristis )
Photograph by Harold Jerrell - © All Rights Reserved.

American Goldfinches are absolutely gorgeous birds, and when their colors brighten its certain that spring has arrived ( but in the mountains, that typically means SNOW is not over ).

Whether it be snow, rime, or even ICE, the winter landscape is truly a wondrous thing.

It can be harsh and cruel, yet so amazingly
beautiful, powerful, and even peaceful at times.

Peaceful Morning Amid The Highlands
Photograph by Wayne Riner - © All Rights Reserved.

Some of the most beautiful winter scenes are created by changing light, near sunrise and sunset, with heavenly reflections altering colors of ice or a snowpack ( as above and below ). 

Awesome Beauty
Along The Tennessee Valley Divide
Shimmering Sky & Pathway - Long Ridge
Photograph by Wayne Riner - © All Rights Reserved.

Roadway To Orchard - Long Ridge - December 2009
Photograph by Wayne Riner - © All Rights Reserved.

Variations In Light - Tennessee Valley Divide
Photograph by Wayne Riner - © All Rights Reserved.

Sometimes, the sunrise itself is purely
the STAR of the show!

Pine & Blue Sunrise With Snow - January 7, 2010
Photograph by Wayne Riner - © All Rights Reserved.

Sunrise Toward High Knob Massif - January 14, 2010
Photograph by Wayne Riner - © All Rights Reserved.

WOW...purely awesome!

Sunday, January 3, 2010

MEGA-Disaster Snowstorm of December 2009

Awesome Beauty Hides The Beast
Photograph by Wayne Riner - © All Rights Reserved.

The High Knob Landform

"Pops, cracks & thunderous crashes began to fill the evening hours as tree limbs and whole trees gave way under the increasing weight of a super-wet snowfall.

Flashes of blue, pink, and green light filled the sky as large snowflakes fell with fury. While some of the colorful light display was attributed to power lines being ripped from electrical transformers, some of it was also the result of lightning as convection ( thunder ) erupted within the potent upward vertical motion field. 

Lightning flashes passing through a multitude of snow crystals acted like millions of tiny prisms to separate the 
white light into its component colors.

A truly beautiful site amid an 
extremely destructive storm."

Wayne Browning - January 1998.
I wrote the above words in the wake of an epic snowstorm which struck the western slopes 
of the Appalachians during January 27-28 in 1998.

That storm unofficially established a new 24-hour snowfall record for the state of Virginia, when 36" to 40"+ of snow depth buried upper elevations of the sprawling High Knob Massif ( Wise-Scott counties ) and adjacent portions of the Tennessee Valley Divide ( southern Dickenson County ).

The January 1998 snow blitz devastated mountain hollows below 2000 feet with a high density snowfall that generated massive tree damage and widespread power outages 
across Wise and Dickenson counties.

Snow densities as great as 3:1 to 4:1 
remain the highest ever observed in Clintwood
( 45+ years of records ).

Above 1800 to 2000 feet in elevation the snowfall became less dense, with a significant decrease in snow densities observed above the 2500 to 3000 foot elevation zone.

So, while MUCH more snow fell across mid-upper elevations, there was not much tree damage 
( with only a few mid-elevation exceptions ).

Initial input data into the ETA terrain based model reveals
the atmospheric setting during January 27-28 in 1998.

ETA Model Initialization for January 27, 1998 at 0700 hours
Image Courtesy of Unisys Weather Processor

ETA Model Initialization for January 27, 1998 at 1900 hours
Image Courtesy of Unisys Weather Processor

ETA Model Initialization for January 28, 1998 at 0700 hours
Image Courtesy of Unisys Weather Processor

The January 1998 storm took an inland track of a Miller A Cyclone, as typified below by a graphic courtesy of the Blacksburg, Va., NWSFO.

Typical Miller A Cyclone Track
Image Courtesy of Blacksburg NWSFO

Fast forward nearly 11 years to December 16-17 in 2009.

Making Of A MEGA-Disaster

Dawn Above Powell Valley - December 16, 2009
Photograph by Roddy Addington - © All Rights Reserved.

No one outside of the hardest hit corridor from northern Scott, across Wise, Dickenson, and Buchanan counties realized the scope of this disaster nor its true impact upon residents.
That included the regional news media.

The following will document the days before, during, and after the great storm episode, to include many personal stories from those struggling to survive day by day in the wake 
of this absolutely incredible MEGA-disaster.

Pre-Storm Setting

The dawn of December 16 was amid a colder air mass in the wake of another wet, wind driven rain across upper elevations of the High Knob Massif.

Rain totals of 1.50" to 2.00" were common in the highcountry during December 12-14, 2009 boosting both whitewater creeks and monthly precipitation totals well above average for mid-month ( 6.08" hand-measured at the home of Otis & Nancy Ward in the Robinson Knob community of High Knob during 
December 1-13, 2009 ). 

By contrast, only 0.52" accumulated in Clintwood on strong downsloping SSE-SE flow into northern Wise and Dickenson counties ( pushing the December 1-15 tally to 3.15" ).

Morning hours of December 16 were marked by an interesting mixture of color and blackness, as captured by photographer Roddy Addington from the floor of Powell Valley
(reference above photograph).

An inspection of morning weather charts did
NOT reveal anything dramatic in the current state.

NAM Model Initialization for December 16, 2009 at 0700 hrs
Image Courtesy of Unisys Weather Processor

The left-hand charts show a large high pressure building into the region, with the southern Appalachians along the periphery of
a cold, dry ( as illustrated by the lower right chart ) air mass.

Of note, however, is the upper right chart which shows a distinct split flow in the upper air, with a polar jet stream extending from the Pacific Northwest across the Great Lakes and a sub-tropical jet stream running from Texas into the Carolina's.

NAM Model Initialization for December 16, 2009 at 1900 hrs
Image Courtesy of Unisys Weather Processor

The situation in the forecast model world was, however, showing a MUCH different setting for coming days, with models printing out some impressive precipitation numbers across the southern Appalachians.

In fact, the setup on paper was analogous in important ways to the great January 1998 snow blitz which I highlighted above ( with a deep isothermal layer showing up in lower levels ).

Personally I became very concerned 
and sent out a mass email to my climate newsletter mailing list around 11:30 PM on December 16 to draw attention to the fact that a significant winter storm was taking shape on forecast models.

The pre-storm setting began to take shape during December 17, with gathering moisture and heavy rains developing across South Texas and the 
Gulf Coast.

NAM Model Initialization for December 17, 2009 at 0700 hrs
Image Courtesy of Unisys Weather Processor

The current state of the atmosphere above, at 7 AM on December 17, shows increasing Gulf of Mexico moisture as high pressure sat on top the Appalachians.

A jetstreak core over the northern Rockies, in the upper right chart, was pointed toward the SOUTH to indicate major TROUBLE ahead
( i.e., cyclogenesis and subsequent destruction ).

NAM Model Initialization for December 17, 2009 at 1900 hrs
Image Courtesy of Unisys Weather Processor

By 7 PM on December 17, as illustrated on the charts above, a defined surface to 850 mb low pressure had closed off over the western Gulf of Mexico ( far E to NE of Brownsville, Texas ).

[ I was personally so concerned about this situation that my father and I traveled to Lowe's in Wise and bought a generator and connection cables on December 17.  I ran out enough water to do us for 
5 days ( we were out of electricity for 4 days and nights during the January 1998 debacle ), and put out enough feed for our horse ( Black Beauty ) 
to also last for approximately 5 days ].

I sent out numerous personal emails on December 17 into December 18 warning of a MAJOR dump of snow and my fears for 
another situation like January 1998.

However, after 13 days without power, I felt it necessary to apologize to my mailing list that I did not send EVERYONE on it a much stronger warning ( even though that is NOT in any way my job or responsibility ).

[You will likely never hear ( how nice it would be to hear ) broadcast news media and official forecasters apologize for a forecast in error, or presented without a strong enough warning of impending danger].

Given what I will highlight below, and the 
life-death situations involved, I cut NO ONE with significant weather knowledge any slack on this one!  They were ALL DEAD WRONG and NEVER HAD A CLUE as to the real and true magnitude of this event upon its unfolding ( and DANGER to everyone impacted ).

At least, no one with LIVE communication capabilities relayed it to the public across far southwestern Virginia in the way it needed 
to be delivered.  Period!

That no slack cutting also includes myself, since I should have sent out a stronger warning and discussed it with those folks responsible for forecasting across this region in the days prior to the event ( reminding everyone of the January 1998 storm ).

Thus, the apology to those on my climatology mailing list!

It is well understood that any given storm or event can be under-forecasted in terms of impact, but once it unfolds itself before the eyes, and reveals its life-threatening nature, some very STRONG and AGGRESSIVE action must then be taken immediately in every way possible.

Some might think such an event could not be anticipated by anyone.  That is simply NOT TRUE, since climatology teaches!

The January 1998 event was the ANALOG 
to this storm.  It was the teacher.  If it happened then, it could happen again and be WORSE.  An event more destructive than what will be shown below CAN occur, but will never be highlighted strong enough in advance IF lessons are not learned.

The STORM Event
of December 18-19, 2009

NAM Model Initialization for December 18, 2009 at 0700 hrs
Image Courtesy of Unisys Weather Processor

Important changes were evident on weather charts by 7 AM on December 18, with a deepening surface to 850 mb low pressure along the northern Gulf of Mexico coastline, and a rapidly growing moisture field being lifted into the RIGHT-REAR quadrant of a phasing jet stream.

Note wind vectors in the upper right panel pointing into higher wind speeds, above a deepening moisture field shown in the lower right chart ( above ).

The simple effect would be like pulling air upward through a chimney, as northern and sub-tropical jet streams phased, or merged together, generating a divergent wind field aloft that had to be compensated for by converging air flows at the surface ( i.e., a winter storm was literally beginning to form right over the southern Appalachians ).

Air above the surface, at the 850 mb level on the upper left chart, was above freezing ( 0 degrees Celsius ) but also relatively dry so that evaporative cooling would occur with precipitation onset.

A key feature of this event was E-ESE winds forecasted above 3000 feet, with E-NE winds across lower and middle elevations.

These ingredients generated an unknown.

How much precipitation would fall as rain across lower elevations before a change to wet snow?

All snow was NEVER in question for mid-upper elevations along windward facing slopes of the High Knob Massif and Tennessee Valley Divide, where upslope cooling rules.

In fact, I expected this event to set the stage for a Thermally Indirect Mesoscale Circulation that is orographically forced and held in place on easterly air flow trajectories by the sprawling expanse of the High Knob Massif, which I first identified post-January 1998.

[ I discovered it during events following the January 1998 blitz, and upon its discovery realized that the circulation had played a critical role in enhancing that state record shattering fall of snow ].

So I was both worried ( about a WET crippling snowfall ) and also excited about getting another opportunity to study and document this unique High Knob Massif circulation!

1140 hours on December 18, 2009
Eagle Knob of High Knob Massif
Image Courtesy of Steve Blankenbecler - © All Rights Reserved.

The first snowflakes began falling atop the High Knob Massif between 1100 and 1200 hours on December 18, rapidly turning the ground and road white on strong easterly winds.  Increasingly large snowflakes were noted, with drifting along the crestlines beginning surprisingly fast on horizontally driven snow.

At the same time, rain was falling leeward of the highcountry on the floor of Powell Valley.

It soon became very evident that the massif was generating an orographically forced melting zone, and IT WAS ON, as snow drifts of 6-12"+ developed in only a couple of hours!

1358 hours on December 18, 2009
Eagle Knob of High Knob Massif
Image Courtesy of Steve Blankenbecler - © All Rights Reserved.

Light rain initially began falling at Clintwood 1 W ( 1560 feet elevation ), amid the Russell Fork Basin of Dickenson County, with 0.17 inches of accumulation before a change to wet snow.

Of particular interest, the snow was extremely slick. My Dad and I went to Browning Farm during the time rain was mixing with and changing to wet snow. It was all snow by the time we got up on the farm ( at 1700-1800 feet elevation ).

Snow became moderate-heavy while we took care of our horse,
Black Beauty, putting out extra hay to last for at least five days.  By departure time for home, snow had only accumulated around 0.3 inches on the ground and road. My Dad was taking the tractor, with snow blade to the house, in our anticipation of future snow plow work. He dropped the tractor blade to "back-blade" the road down to the house. This loosened up gravels and brought some to the surface.  This helped me, since every time I tapped the brakes of our F-150 4x4 truck it would slide. I knew right then, it was going to be one SLICK snow!

Snow quickly accumulated, with very LARGE snowflakes forming amid the isothermal profile of the lower atmosphere ( deep layer in the vertical with near freezing air ).

By 1700 hours ( 5 PM ) a rain gage melted content found 0.40" to nearly match a 0.41" snow core taken off my snowboard.  Snow was falling nearly straight down into the mountain hollow, in rather dramatic contrast to the horizontal fall observed on lofty Eagle Knob of High Knob ( 4196 feet elevation ).

Ground measurements found 3" to 4" of accumulation to match my 3.5" snowboard depth.  This yielded an initial snow density of 8:1 to 9:1 
( it would get higher ).

Snowflakes became absolutely HUGE, with measurements on some flakes finding diameters of 2" to 4"+ .  In fact, the largest clumps would cover the entire palm of your hand and splash over the sides!

Large snowflakes 
became widespread.

Mark Quillen said they became big as baseballs as they fell upon rugged northwest slopes of Little Stone Mountain of the High Knob Massif, at the lovely Appalachia Lake Water Plant of the 
Powell River Basin.

Cal Adams said snowflakes were like tea cup saucers falling from the heavens at his home on Little Mountain of High Knob, amid the upper Devil Fork Basin of the Clinch River Basin.

Photographer Roddy Addington confirmed it, as he left his construction site upon the floor of Powell Valley amid only rain and got up to near Little Stone Mountain Gap on U.S. 23 .

Roddy said the snowflakes were simply incredible,
so big as they would sag downward in the middle.
Like grapefruits falling from the sky!

Others also said they had never seen anything like them, but such snowflakes ( to at least near these sizes ) were also an ominous characteristic of the January 1998 storm.  At that point, I simply felt a gut wrenching sickness in my stomach as I simply knew what was coming, and NO ONE could stop it!

It was at about this point, with 4" of ground depth, that I started to hear pops and cracks of breaking tree limbs.  A sound unlike any you've ever heard, for anyone never having been through it, and a feeling that can not really be described.

[ During the January 1998 storm I began to hear pops and cracks with only 2" of ground depth, indicating that this snowfall was not quite as WET and dense as the 1998 fall since it took 4" of depth to begin the horror this time.  It should be noted that while pops, cracks, and crashes associated with an ice storm can also be very dramatic, they generally come on slower as it takes more time for ice to build up than snow ].

Joe Fields reported more than 8" of snow depth in the High Chaparral community of High Knob ( elevation 3300 feet ) at about this same time of 1700 hours on December 18.

Joe also reported that electricity was already out ( an ominous early warning to all )!

Nearly 1000 vertical feet higher, and 3.7 air miles west on Eagle Knob of High Knob, the snow looked to be much deeper.

1643 hours on December 18, 2009
Deep Snow - Eagle Knob of High Knob Massif
Image Courtesy of Steve Blankenbecler - © All Rights Reserved.

[ Note the large inverted V-shaped mound of snow on back of the cream colored building, and drifting around the thick cement tower support on the ground ].

An earlier image for comparison.

1139 hours on December 18, 2009
Eagle Knob of High Knob Massif
Image Courtesy of Steve Blankenbecler - © All Rights Reserved.

[ Easterly winds were blowing from left to right across these images, so its very interesting how the large mound of snow built up on the backside ( leeside ) of the building.  No doubt due to some vortical motions ( air swirling around the building ) ].

Meanwhile, far beneath the high country, Darlene Fields ( Joe's wife ) was stuck in an ever growing line of traffic backed up on U.S. 23 outside of Norton. She was sitting right on the large bridge near Little Stone Mountain Gap, in the Head of Powell Valley, and making little to no progress.

It eventually took Darlene
3 LONG hours just to get into Norton 
( typically a 5-10 minute drive from there ) as traffic 
backed up all the way to Big Stone Gap!

Darlene was one of the blessed!

City of Norton - December 18, 2009
Unknown Submission to WCYB-TV 5 Archives

Some people spent MUCH longer on the snarled roadway, up to 9+ hours, while many others simply gave up and abandoned their vehicles!

Photographer Roddy Addington captured some of these chaotic scenes through his truck windshield during a drive along U.S. 23 the following day.

Buried & Abandoned - December 19, 2009 on U.S. 23
Photograph by Roddy Addington - © All Rights Reserved.

Post-Storm Chaos on U.S. 23 - December 19, 2009
Photograph by Roddy Addington - © All Rights Reserved.

The problem, at least partly, was a truly dramatic weather change from only rain in Big Stone Gap to heavy, wet snow across the Head of Powell Valley and northern-northwest slopes of the High Knob Massif, such that travelers along U.S. 23 were experiencing a rapid change and deterioration in driving conditions.

Travel along old Route 23-Alt. 58 through the "Big Stone Gap" in the northwestern arm of the High Knob Massif offered little relief, as another dramatic transition zone was encountered upon passing through the water gap to the northwestern slopes of Little Stone Mountain ( going from rain to very heavy snow ).

Roddy Addington confirmed the above, as was previously noted, with just rain at his construction site in the Cracker Neck of Powell Valley through 1500 hours ( around the time he left for his home in Pound and encountered the HUGE snowflakes near Little Stone Mountain Gap ).

But the storm was only starting to CRANK during the 1500-1700 hour period, with the most INTENSE portion yet to come!

Since the High Knob Massif is the BIG DOG ( largest mountain mass ) across southwestern Virginia, it often dominates and controls the precipitation pattern.

This could easily be seen on Doppler radar.

December 18, 2009
KJKL Doppler Radar Base Reflecitivity at 5:58 PM
Image Courtesy of Plymouth State University

[ A series of illustrated Doppler radar images will highlight this section, as personal stories and conditions are told to document this incredible time ].

The 1700-2000 hour ( 5-8 PM ) period on December 18 was dominated by EXTREME snowfall rates, and the notable formation and reformation of higher reflectivity echoes along the W-WNW flanks of the High Knob high country.

For a visual illustration of this awesome high country flank which contributed to formation of this truly amazing mesoscale circulation and Doppler reflectivity pattern, please reference the second
Roddy Addington photograph entitled:

"Big Sky & Big Mountains" in the following section:

All major mountain passes in the High Knob Massif area were essentially shut-down early by this storm, which was also the case farther north along U.S. 23 on Wise Mountain ( Indian Gap ) and Pine Mountain ( Pound Gap ) and on U.S. 119 across Pine Mountain between Whitesburg and Cumberland in Kentucky.

Sandra Earls & Freda Davis reported that it was raining "cats and dogs" on the Kentucky side of Pine Mountain when they left from teaching school in Letcher County. That quickly changed and gave way to another dramatic transition into heavy, wet snow as they climbed upward into Pound Gap along U.S. 23 toward easterly air flow impinging upon eastern slopes of rugged Pine Mountain 
( between Jenkins, Ky., and Pound, Va. ).

Sandra said it took them one LONG hour to get down the Virginia side of the mountain, where they ended up staying the night at the Valero Gas Station near Pound. Electricity went off around midnight, leaving them in darkness!

A scary time as the snow piled up,
trees crashed down, lights and nearly all
communications went out!

December 18, 2009
KJKL Doppler Radar Base Reflecitivity at 6:21 PM
Image Courtesy of Plymouth State University

Sandra and Freda were actually fortunate, as a while later conditions became so bad that no one could travel by vehicle, either up or down, on the Virginia side of the mountain. A young man working in Kentucky told me that he only made it to Pound Gap, where he left his 4-wheel drive truck and walked 8 long hours to get down to his home in Pound ( he could have froze to death if conditions had not been relatively mild ).

Along the way he saw tractor trailer trucks overturned, a sporty Mustang stuck beneath a big rig, vehicles getting stuck trying to go up the wrong side of U.S. 23, and so much falling snow that it was hard to see ( let alone walk ).

It was complete and total chaos!

Such was also the situation along U.S. 119 which crosses Pine Mountain just southwest of Flat Gap, and in the Indian Gap of U.S. 23 just outside the town of Wise.

The U.S. 119 site was frightening for many parents since a couple of school buses became stuck on the mountain ( with a rush of folks trying to rescue them adding to the panic and chaos ).

December 18, 2009
KJKL Doppler Radar Base Reflecitivity at 6:38 PM
Image Courtesy of Plymouth State University

The greatest snowfall rates developed near the back edge 
of highest reflectivities along the rugged Wise-Scott border, where formation and reformation occurred, with simply AWESOME snowfall rates per hour in the Thunderstruck Knob to Eagle Knob corridor of the High Knob high country.

My cousin Meghan Mullins got stranded in that Indian Gap mess, and luckily had a cell phone to call her step father for help.

Carroll Wayne McCoy left the Georges Fork section of Dickenson County to pick up Meghan, with chain saw in back of truck, and would not return home with her for 7.5 hours ( typically it would have taken less than 1-hour ).

The only way home was via State Route 72, from Coeburn to Clintwood, and then it was only possible by using a chain saw to cut falling trees out of the road. One tree, however, fell and busted his truck windshield.

What a truly dangerous experience!

Like in January 1998, but even worse, abandoned vehicles became so numerous along highways across Wise and Dickenson counties that VDOT crews could not even work the roadways.

Of course, the real problem became falling trees and power lines!

Darlene Fields called husband Joe to come pick her up, after the long Friday evening journey into Norton from the Head of Powell Valley.  Joe could not reach her along Alt. 58, from Tacoma, and had to take back roads to finally get to the Hardee's in Norton where Darlene was waiting.

What would typically be a pleasant drive home, simply ended, as they could not make it back up State Route 706 to High Chaparral. The road had become completely blocked, and there was no other roadway into the high country which had not become impassible due either to fallen trees 
and/or drifting snow.

NAM Model Initialization for December 18, 2009 at 1900 hrs
Image Courtesy of Unisys Weather Processor

[ Joe & Darlene stayed with family near the City of Norton, without any electricity, and did not make it back home until Sunday night
( December 20 ) ].

Getting home was not easy, with Joe having an accident when his 4x4 truck slid off the road into an embankment. It had to be left behind, with Darlene following in another 4x4 to pick him up.  Of course, upon returning, they had no electricity, phone, or water, and their typically trusty generator would not start.   

It was a cold Sunday night,
and beginning of a rough week!

KJKL Doppler Radar Base Reflecitivity at 7:01 PM
Image Courtesy of Plymouth State University

Now we come to the STARK
reality of this event.

This had in a matter of 12 hours
become nothing less than a

No main or secondary road, and hardly even a single street or driveway, were passable from the High Knob Massif northward across Wise County, Dickenson County, and Buchanan County.

Roads were blocked by abandoned vehicles in deep snow, power lines and poles, and in some hollows by more than 70 uprooted and fallen trees along single stretches!

People were simply isolated and trapped in place, where ever that may have been at the time, and I DO MEAN ISOLATED.  It literally took many DAYS in some cases to open the worse roads via a collective effort of local residents, VDOT, AEP, and other workers.

To make matters worse, hardly a single light remained on across this entire area with 96 percent of Dickenson County alone losing electricity 
( how 4 percent kept power I am yet to figure out ).

In addition, most folks also lost phone, cable, internet, and water.  It was indeed the start of a very rough period for many residents.

No one, including news media, outside the local area realized the significance of this storm event and the hardships faced by local residents.

For the young and strong it was manageable, but for older residents, those sick, and those alone and isolated it was a tough, scary, and very dangerous time in their lives.

It simply became day to day survival.

December 18, 2009
KJKL Doppler Radar Base Reflecitivity at 7:19 PM
Image Courtesy of Plymouth State University

The evening of December 18 and overnight period of December 19 was a truly HORRID experience for many folks in their homes.  Many simply could not sleep for fear of being killed in bed!

The reason, POPS, CRACKS, CRASHES and BOOMS as limbs were stripped from trees and whole trees uprooted under the weight of the 
deep, HEAVY ( high density ) snowfall.

The entire horizon above Clintwood lit up with an eerie pinkish glow as trees ripped away power lines from transformers & flashed through falling snow crystals.  A scene not seen since, you guessed it, the great January 1998 blitz!

[ Living just outside of town, I told my folks it was coming ( power outage ) to us upon seeing such an amazing PINKISH GLOW over the horizon.  I began running more water.  Darkness soon fell upon Browning Hollow for 13 LONG days as large trees uprooted and crashed across power lines, with rapid flashing and flickering
adjacent to our home ].

Anyone not living in a wooded area, or never going through a storm event like this, simply can not truly understand what I have just stated.  That is what was perhaps most upsetting to me during this event.  The knowing that people would be isolated, lucky to survive the night without injury, and faced with a simply enormous recovery effort which would take a VERY long time.

Most concerning for folks sick, elderly, or caring for those in such conditions, was the fact that there was no way in or out of many locations ( or even along main highways ).  NEVER in the 30+ years since I started recording weather conditions had a storm cut off every roadway with fallen trees.  They had been blocked by snow drifts, but never ALL blocked ( and BLOCKED BADLY ) by so many 
trees and limbs.  It was complete isolation!

NAM Model Initialization for December 19, 2009 at 0700 hrs
Image Courtesy of Unisys Weather Processor

Weather charts by early on December 19 revealed that the cyclone had taken a simply CLASSIC Miller A storm track ( please reference early portion of chronicle ).

Post-Storm Disaster & Recovery
( Storm Reports & Discussion Of Event )

Buried Under 2 FEET Of Snow
Robinson Knob of High Knob Massif - December 19, 2009
Photograph by Otis Ward - © All Rights Reserved.

A snow depth of 24" was measured by Otis & Nancy Ward during the morning of December 19, at their home in the Robinson Knob community of the highcountry ( elevation 3235 feet ). 

[ I will highlight an entire series of pictures taken by my friends Otis & Nancy Ward within this section. More snow fell after these pictures were taken! ].

Otis & Nancy had no electricity, phone, or public water and remained without power for 6 days and nights.

However, living in the High Knob highcountry since April 1974, they had been through such periods many times before.

Johnny Combs also reported deep snow at his home in the Flat Gap of the High Knob Massif, located 1.8 air miles northeast of Robinson Knob.

Johnny said the snow was "well above my knees," and reported significant damage to trees around and below his elevation of 2750 feet.

Trees blocked Pine Camp Branch Road 
( State Route 699 ) up to Flat Gap, with one large tree falling before Johnny could get back home during the evening of December 18.  He had to walk home through the heavy snowfall to get his chain saw.

A couple of 4x4 trucks had gotten stuck trying to cross the trees in the deepening snow and made the situation more complicated.

Chris Sturgill rode a 4-wheeler up the mountain from his father's home in Coeburn and was also blocked by the big tree until Johnny was able to cut it out.  Chris was heading to his home within the East Moore Knob section of the High Knob highcountry ( elevation around 3200 feet ).

The snow accumulated so much that Chris eventually had to abandon his ride and walk the final mile through DEEP & drifting snow to reach his family.

A very dangerous time!

Elevation 3235 feet
December 19, 2009
Robinson Knob of High Knob Massif
Buried Beneath A DUMP Of Wet Snow
Photograph by Otis Ward - © All Rights Reserved.

The deepest snow actually accumulated 4 to 10 air miles to the west and southwest of Robinson Knob, within the main crest zone of the High Knob Massif between Thunderstruck Knob and Eagle Knob, Camp Rock, and the upper Big Cherry Basin.

[ The section of the massif impacted most by its orographically generated and anchored thermally indirect circulation ].

My friend Steve Blankenbecler, of VA-KY Communications, verified the DEEP snow during a trip to the Eagle Knob tower site on December 21.

After Some Settlement - December 21, 2011
DEEP Snow Against TALL Fence - Eagle Knob
Image by Steve Blankenbecler - © All Rights Reserved.

Steve reported snow depths of around 3 feet, with drifts of 4-5 feet.  This after some settlement on the snowpack during the previous 48-72 hours via sheer weight of upper portions of the big snow pressing downward on the first foot or so next to the ground.  Wow!

Cal Adams measured 34" of snow depth at his home in the upper Devil Fork Basin, adjacent to Big Cherry Lake, on the morning of December 19.  Cal's home is located on Little Mountain of the High Knob Massif, SW of Straight Fork Ridge.

The snow depth was not a drift, since Cal measured it in three different places and it was all "straddle" deep and up to his truck bed!  
Cal measured local depths up to 42" .

This was an important report given Cal's home is significantly lower in elevation than the head of majestic Big Cherry Basin and the adjacent Eagle Knob summit to indicate that a massive dump of snow had buried the crest zone for miles!

[ Cal reported that his Beagle dog was like a mole in the deep snow, as it would completely disappear and tunnel through it ].

A dozer was eventually brought in to open up the road into Little Mountain, and the Eagle Knob communications area ( shown above ), where electrical engineer Terry Surface had to haul in extra diesel fuel to keep the generator going for Blue Ridge Public Television ( WSBN-TV ). 

An Old Dominion Power worker confirmed the deep depths within the Big Cherry Lake area, where he said it was "over his knees."  The snow, which was between knee and waist deep, had actually settled quite a bit by that point as well.

December 19, 2009
Robinson Knob of High Knob Massif - Snow depth of 24"
Photograph by Otis Ward - © All Rights Reserved.

David Sturgill confirmed these reports upon a visit to his cabin located at the northeastern end of what was once known as Johnson's Pasture on Little Mountain.  His wife Ann reported that David found snow depths more than 2 feet deep, with 4-5 foot drifts, some 5 days after the storm event.  The snow was still deep enough to stick his 4x4 truck. 

Robinson Knob of High Knob Massif - December 19, 2009
Photograph by Otis Ward - © All Rights Reserved.

My friend Gary Hampton, Superintendent of the Big Stone Gap Water Plant sitting within the mouth of South Fork Gorge of the High Knob Massif, indirectly verified these HUGE snowfall reports with a 2.85" rain gage water content on his 4"-diameter NWS gage ( elevation 1915 feet ).

The rain gage location sits 2308 vertical feet lower in elevation than the High Knob peak ( and head of Big Cherry Basin ).

Robinson Knob of High Knob Massif - December 19, 2009
Photograph by Otis Ward - © All Rights Reserved.

The significance of the 2.85" rain gauge total in the mouth of South Fork Gorge of High Knob is that it all fell as snow up above the Plant, where water contents were likely well over 3.00" and the density of snow lower ( please reference my later snowfall density discussion ).

It was also 1.12" more than the NWS rain gage measurement at the Big Stone Gap Wastewater Treatment Plant, located 6.0 air miles to the west, on the sinking side of the orographically created and anchored circulation ( measurement made with an official 8"-diameter NWS gauge ).

Jim Davis reported that the Big Stone Gap WWTP total included mostly rain, with only around 2" of total snow depth along the Powell River ( near the Wise-Lee border ).

Frank Gentry verified this report and said he did not lose electricity, kept phone service, and had only around 2" of snow depth at his home not far from the Big Stone Gap WWTP.

My friends Otis & Nancy Ward measured 3.27" during the December 14-24 period, which included some December 14-15 rainfall. This was prior to 0.85" of additional rainfall measured into Christmas day.

MUCH moisture was lost by the 4"-diameter NWS gage in the big snow since it could only hold around half the 2 feet of depth ( assuming perfect catch, which was NOT realistic given winds during this event in upper elevations above 3000 feet ). 

So while the 10.20" Robinson Knob total for December 1-25 is impressive, it is very likely more than 1.00" below what actually accumulated during that period.

Wetter portions of the High Knob Massif had at least 11.00" to 12.00"+ of total precipitation during December 2009 ( with additional rain & snow being measured at month's end ).

From 2-3 feet of MEAN snow depth,
with drifts of 4-5+ feet, to just 2" of depth
in only a relatively short distance of 5-10+ air miles on the morning of December 19.

Simply incredible!

Most impressive of all, however, is the fact that much of this HUGE depth of snow accumulated between NOON and MIDNIGHT on December 18 via simply AMAZING snowfall rates!

NOTE: Max snow depths which accumulated 
in the High Knob Massif, within LESS THAN 
24-hours, during this event would once again "unofficially" break the 24-hour snowfall record 
for Virginia, of 33.0" observed on March 6, 1962 
in Big Meadows of Madison County 
( in Shenandoah National Park ).

The 36" to 40"+ of snow depth which accumulated within the High Knob Massif during the January 1998 storm also broke the state 24-hour snowfall record ( unofficially ).

It is most interesting to note that both of these great MEGA-dump events were associated with an orographically forced and anchored Thermally Indirect Mesoscale Circulation on easterly air flow trajectories crossing the High Knob highcountry.

Of the 46" of snow hand-measured by Joe & Darlene Fields within High Chaparral of High Knob during the great blizzard of March 1993, 30" were measured within 24-hours at 3300 feet elevation.

That implied the 24-hour state snowfall record was again broken above 3300 feet, where final snow depths reached 58" near the 4223 foot summit level.  That occurred without development of the Thermally Indirect Mesoscale Circulation noted during the January 1998 and December 2009 events.

All of these above reports have been verified by MULTIPLE individuals during each storm episode noted, with March 1993 & December 2009 events being especially well documented.

Robinson Knob of High Knob Massif - December 19, 2009
Photograph by Otis Ward - © All Rights Reserved.

Mark Quillin illustrated the nature of conditions found early on December 19 as he worked hard to get into Appalachia Lake WP on Little Stone Mountain of the High Knob Massif.

Mark, who lives amid the Head of Powell Valley, had a journey just getting out of the Valley.

After a night spent amid constant pops, cracks, and crashes, with even a few trees rolling down the steep mountain slope above his home, he headed south through the Valley with numerous trees across the road ( he had a chain saw, which would soon get plenty more use! ).

[ A significant snowfall gradient developed within Powell Valley itself, from the noted 2" of depth near the Powell River in Big Stone Gap to a foot or more of depth in the Valley Head.

The entire Valley had a significant amount of rain, with air flow downslope off the massif, prior to the change into WET snow ].

Robinson Knob of High Knob Massif - December 19, 2009
Photograph by Otis Ward - © All Rights Reserved.

Once reaching the base of Little Stone Mountain in Appalachia, Mark had NO CHOICE but to walk with chain saw.  It took him nearly 8 hours to walk up the mountain, cutting trees out of the road as he went to reach the Water Plant ( Appalachia Lake WP sits at 2360 feet, 1024 vertical feet lower than the summit which rises above the Lake ).

Walking is NOT the proper word.  This snow was like trying to MOVE IN CEMENT, making even getting around on FLAT ground ( rare in this area ) difficult.

Snow depths were knee deep in places, with 16" to 22" of general snow depth around and below Appalachia Lake.

Like most everywhere electricity was OUT and the Water Plant had to be run off generator power via much hard work by Superintendent Jack Pitts and Mark.

Although snow had stopped falling heavily before dawn on December 19, what most everyone outside of this GROUND ZERO impact zone did not realize was that trees continued to fall.  The dense snow continued to lay upon trees, bringing more and more down through daylight hours of December 19 into the next day!

POPS, CRACKS, and even a few THUNDEROUS CRASHES could be heard for SEVERAL DAYS after the real storm ended.

Mark returned to the Little Stone Mountain base with a 4-Wheeler early on December 20, thinking he would be able to just ride up to the Water Plant.  NO WAY!!

He had to cut some 30 more trees out of his way, making more than 50 trees cut along this single section of roadway.  Many of the trees were large, since they fell over from their roots.

Some trees uprooted and fell over against standing trees ( as many remain RIGHT NOW ), while MANY limbs were stripped and left bent down or hanging in other standing trees.

Mark's story exemplifies the severe conditions endured from the High Knob Massif northward across Wise and Dickenson counties.

December 19, 2009
Deep Snow Long Ridge - Highlands of Dickenson
Photograph by Wayne Riner - © All Rights Reserved.

Another aspect of this initial post-storm period was low clouds that obscured higher elevations, continued light snow, and absolutely NOT a single PEEP of any sunshine for 3 days.

Along The Tennessee Valley Divide
Snow Laden - December 19, 2009 - Long Ridge
Photograph by Wayne Riner - © All Rights Reserved.

Abandoned vehicles remained along most roads 
for DAYS after the storm, with Roddy Addington illustrating more scenes along U.S. 23 between Norton and Big Stone Gap.

Trees Swaying Under Weight Of Heavy Snow
Almost to Powell Valley Overlook - Dec 19, 2009
Photograph by Roddy Addington - © All Rights Reserved.

VDOT did an exceptional job working through this disaster, with my friend Harmon Kilgore noting that it was the most difficult situation he had ever experienced ( VDOT in Wise & Dickenson counties are NO rookies when it comes to winter ).

Post-Storm Conditions near Little Stone Mountain Gap
Photograph by Roddy Addington - © All Rights Reserved.

For many living away from MAIN interstates, like U.S. 23, it was either easier or just plain necessary to WALK during and after this storm!

Says It All - Walking Along Library Hill in Wise
Photograph by Roddy Addington - © All Rights Reserved.

Finding a place to put all the snow was simple, just pile it up against the house to hold in some HEAT with NO electricity for MILES around in the vast majority of locations!

December 20, 2009
Snowbound At Home In Wise, Virginia
Photograph by Roddy Addington - © All Rights Reserved.

At the Browning Home we had GREAT SLABS of snow that gradually slid down off the roof, but would not break loose until they nearly blocked the entire view from the windows.  Then, with a force that would literally shake the ground, BOOM, a slab would drop by day or night into a massive pile.

This is illustrated below by a Jimmy Stidham photograph, taken of Lighthouse Church in Wise.

Lighthouse Family Worship Center Draped In Snow
Photograph by Jimmy Stidham - © All Rights Reserved.

Jimmy Stidham measured 14" of snow depth on Stephens Road in Wise, with 14" also measured by his pastor at Lighthouse Church in Wise ( shown above on Lake Street ).

Local snow depths as great as 22" were reported on Dale Branch Road, in the Hurricane section of the Wise Plateau.

Whether within rural mountains, or in town, 
this snowfall generated postcard scenes in the
DAYS before Christmas 2009.

Storm Generates Postcard Scene - Pretty In Wise
Photograph by Roddy Addington - © All Rights Reserved.

Rod Addington Photography

For many thousands in Wise and Dickenson counties, as well as northern Scott and Buchanan, it would be a Christmas spent in darkness.

Another day to survive, warmed only by the love of family and friends and the knowing that we were still alive!

The Town of Wise
Mantle of WET Snow on Christmas Wreath
Photograph by Roddy Addington - © All Rights Reserved.

Sending out Christmas Cards, getting presents, and decorating the home all became pushed WAY back on the list of daily chores.  Life was different now.  MUCH different.  In important ways it brought back what was truly most precious!

Town of Wise Christmas Tree
Photograph by Jimmy Stidham - © All Rights Reserved.

The renovated Wise Courthouse stood stately amid the DEEP snow in downtown Wise ( officially, the snowiest town in Virginia ).

Wise Courthouse on December 20, 2009
Photograph by Roddy Addington - © All Rights Reserved.

This great MEGA-disaster snowstorm came a week or so too late to disrupt examinations & final grades at UVA in Wise, but it made the entrance look nice!

The University Of Virginia's College At Wise
Photograph by Jimmy Stidham - © All Rights Reserved.

Mountain farms along the lofty Guest Mountain portion of the Tennessee Valley Divide, near the town of Wise, looked picturesque with deep snow set against the darkness of a mid-December sky!

Guest Mountain of The Wise Plateau
Tennessee Valley Divide - Coeburn Mountain Rd
 Photograph by Jimmy Stidham - © All Rights Reserved.

Once sunshine FINALLY returned it was a very WELCOMED and most gorgeous sight across the highlands!!

Sunshine RETURNS - Long Ridge - December 22, 2009
Photograph by Wayne Riner - © All Rights Reserved.

No one could deny the beauty of this snowfall, despite its great destructive wrath, with time taken to ponder how Mother Nature RULES even amid this MODERN age!

In many homes without electricity, cable, internet, satellite, or any other modern convenience, nights were spent listening to battery powered radios.

Only glimpses of the "outside" world could be caught at times, with regional and national news being limited by poor signals filled with static, jiggling the radio dial and antenna to try and occasionally pick up a better reception ( signals amid deep mountain hollows are not like ones clearly received upon mountain ridges, or within large, open valleys ).

[ Batteries became as "scarce as hens teeth," as my Grandpa used to say, and hardly could be found anywhere.  Ditto for candles, lamp oil, and the other common necessities of such living.  Some traveled all the way to the Tri-Cities, in northeastern Tennessee, or northward to Pikeville, Ky., in order to find supplies ].    

December 22, 2009
Gorgeous Majesty on Tennessee Valley Divide
Photograph by Wayne Riner - © All Rights Reserved.

A great deal of low-level moisture lingered in the wake of this incredible event, even after sun returned to shine upon the snowy landscape.

This was just beautifully illustated in an American Electric Power ( AEP ) photograph as workers poured into this devastated area from far away, no doubt amazed by awesome beauty of the High Knob highcountry spreading outward from Powell Valley.

Abundant Low-Level Moisture
Powell Valley of the High Knob Massif
AEP Photograph - © All Rights Reserved.

Workers heading north into GROUND ZERO!

Head of Powell Valley - U.S. 23 - High Knob Massif
AEP Photograph - © All Rights Reserved.

The amazing biodiversity of the
High Knob Landform ( HKL ) is perhaps
matched ( and actually generated ) only by the
often incredible diversity of its climate!

As all of the above is pondered, and much more presented below, it is hard and simply unreal to discover that southwestern parts of the HKL, downstream of the remnant massif of its lofty highcountry on E-NE winds, had increasingly limited impacts from a winter storm of such great fury and destruction!

In the Cumberland Gap National Historical Park section this was partly due to downsloping across the lofty backbone of its highlands into Virginia, on NE low-level winds, which greatly reduced snow amounts on valley floors in southwestern parts of Lee County. 

[ Some significant damage was produced by the storm across mid-upper elevations of the National Park as will be later illustrated ].

My friend & photographer Harold Jerrell reported that hardly any snow accumulated on valley floors of Lee County, southwest of The Cedars.

Wilderness Road State Park was a perfect example, with the BLAZING white mass of the Cumberland Mountain arm of the HKL standing like a GREAT WHITE WALL in the background.

What a BOLD & dramatically
majestic contrast to its green valley. 


Wilderness Road State Park - December 22, 2009
Photograph by Harold Jerrell - © All Rights Reserved.

Significant snow and rime extended along the rugged Cumberland Mountain arm ( northwestern flank of the HKL ) until near Rose Hill, southwest of which it became limited on the Virginia side of the mountain.

Rugged White Rocks in Rime & Snow - Dec 22
Photograph by Harold Jerrell - © All Rights Reserved.

The Rose Hill Cemetery looked as if it was IN A DIFFERENT WORLD on December 22.

December 22, 2009
Rose Hill Cemetery in Lee County
Photograph by Harold Jerrell - © All Rights Reserved.

Although snow limited on the Virginia side, the great White Rocks still dominated the landform above Lee County with a sereal, breathtaking beauty.

White Rocks of Cumberland Gap NHP - Misty Haze & Rime
Photograph by Harold Jerrell - © All Rights Reserved.

A bowed orographic wave cloud formed just beyond the White Rocks, mimicking the crestline, to add an interesting feature to this majestic scene.

Bowed Orographic Wave Cloud - Cumberland Mountain
Photograph by Harold Jerrell - © All Rights Reserved.

Carol Borneman, Supervisory Interpretive Ranger, of Cumberland Gap National Historical Park reported that they had to close trails and roads within the Park due to fallen trees.

Cumberland Gap National Historical Park
Cumberland Gap National Historical Park - © All Rights Reserved.

The backbone of the National Park had by far the most snow, where rugged Cumberland and Brush mountains come together to form the lofty highlands of Bailes Meadows and Hensley Flats.

Hensley Settlement - Highcountry Cumberland Gap NHP
Cumberland Gap National Historical Park - © All Rights Reserved.

White Rocks of Cumberland Gap NHP
Photograph by Harold Jerrell - © All Rights Reserved.

Ranger Carol, recent winner of the prestigious Freeman Tilden Award for field interpretation and education within the National Park Service, said storm damage within the Park has initially been estimated at 60,000 dollars.  Trees fell across several buildings within the National Park.

Tree Damage in Sugar Run of Cumberland Gap NHP
Cumberland Gap National Historical Park - © All Rights Reserved.

Trees Blocking Road - December 2009 Storm
Photograph by Harold Jerrell - © All Rights Reserved.

Harold also had some trees topple on his farm, where rain and sleet turned to heavy, wet snow at his location some 6 miles west of the Flatwoods of Lee County.

Silver Leaf Community
Rain & Sleet Turn To WET Snow
Photograph by Harold Jerrell - © All Rights Reserved.

Although his family only lost electricity for around 30 hours, it was a rough December 18 as his father had to be taken to the hospital after the storm began.  Due to bad conditions it took the rescue squad almost 2 hours to reach Pennington Gap, normally only a 30-minute drive.

Misty In Rose Hill
 Photograph by Harold Jerrell - © All Rights Reserved.

Now, back to GROUND ZERO!

Typical Roadway In Dickenson County
AEP Photograph - © All Rights Reserved.

A link to an AEP slide show of photographs is inserted below, while a few other selected images will be shown here.

Many HUNDREDS of power poles were broken and damaged in just Dickenson County, with literally MILES of downed lines across Wise, Dickenson, and Buchanan counties.

Power Pole Replacement - Coeburn Road
AEP Photograph - © All Rights Reserved.

Some locations were left hanging, literally, by localized damage that would leave them sitting in darkness LONG after lights returned to surrounding locales.

Clintwood Area Home - Obvious Damage
AEP Photograph - © All Rights Reserved.

In most cases, localized damage at homes was only part of a much bigger, widespread array of damage along connecting power lines.

Tree Across Line - Clintwood Area
AEP Photograph - © All Rights Reserved.

This disaster exposed some critical concerns and issues which should be addressed before another one strikes!

The following are only a few suggestions.

1 ).  All poles need to be GPS marked, so workers not familiar with the area will have an exact and precise way to pinpoint where they need to go.

2 ).  The general GRID SYSTEM needs to be made more efficient with respect to routing of power.
3 ).  More money needs to be put back into upkeep of the local system, regarding replacement of aging power poles and annual trimming of line corridors.

4 ).  All new construction projects need to have electrical lines buried UNDER ground, with a plan put in place to gradually work toward the BURIAL of ALL existing power lines.

[ Although certainly of enormous cost, just think how MUCH it would SAVE in the long-term to have all electrical lines buried underground.  No snowstorm, ice storm, or wind storm could ever take out power via destruction of trees and breakage of power poles ].

County governments need to adopt a resolution supporting such actions as above, and present it to higher authorities.

AEP workers and those contracted to help did extraordinary work, given the magnitude of this disaster, and they are greatly thanked for their efforts.

Many had to work under simply brutal conditions, in rugged terrain and life risking situations.

PUBLIC outrage in the aftermath of this disaster should be directed at the improvements which NEED to be made, such as those noted above, that clearly rest upon the AEP and ODP corporations ( not those out in the field doing the GRUNT work ).

Little Stone Mountain Gap - December 22, 2009
AEP Photograph - © All Rights Reserved.

I'm no politician, so BACK to Climatology!

What Made This Storm
Worse Than January 1998?

Post-Storm Damage on Caney Ridge of Wise-Dickenson counties
Heather Ring Photograph - WCYB Picture Archive

It will take some time to study this event in detail, but one fact JUMPS out immediately which clearly shows what made this storm more damaging than January 27-28, 1998.

Depth of the ISOTHERMAL Layer!

I noted it in an email to my friend Steve Blankenbecler at 1:42 AM on December 18, some 9-10 hours before the first flakes started to fall during the 2009 event:

"Worrisome vertical temp profile always can be problematic, with close to 32 degrees from surface up to near High Knob summit ( above which it gets cooler ).

So snow density could be high for lower-middle elevations ( increasing danger of power outages and tree damage ), with somewhat lower density snow across upper elevations ( increasing total amounts and drifting up there )."

Forecast models were showing a DEEP layer near 32 degrees, which in meteorology is known as an isothermal layer ( vertical temperature profile with nearly the same value ).

When that value is near the freezing point, and heavy precip is predicted, you've got some BIG problems at hand.

The depth of the isothermal layer ultimately sets SNOW DENSITY bounds, which are simply critical to snowfall impacts. 

No one should be allowed to forecast winter events without an EXCELLENT understanding of SNOW DENSITY, and its general variations across space and time in the MEAN.

Significant Damage on Caney Ridge
Heather Ring Photograph - WCYB Picture Archive

During January 1998 the isothermal layer was relatively shallow, with EXTREMELY HIGH snow densities below 1800-2000 feet in Dickenson County ( as noted previously ).

This devastated deep mountain hollows in northern Wise, Dickenson, and Buchanan counties.

During December 2009 the isothermal layer was MUCH deeper in the vertical, with HIGH snow densities extending upward into the 2500-3000 foot elevation zone.

Large Tree Uprooted Across Road - Caney Ridge
Heather Ring Photograph - WCYB Picture Archive

The size of the area impacted by HIGH to EXTREMELY high snow densities was MUCH larger during the December 2009 storm, with lower-middle elevation zones ( below 3000 feet ) being devastated by WET snowfall in many locations ( exceptions being, as noted below, exposed crestlines where gusty winds helped to blow some of the WET snow off trees ).

Nearly all of northern Wise & Dickenson counties 
( the Russell Fork Basin ) lies below 3000 feet in elevation, as well as nearly all of Buchanan County ( Levisa Fork Basin ), so that a HIGH impact event developed across a large corridor during December 18-19 which extended into adjoining portions of southeast Kentucky and West Virginia.

Snapped Like A Toothpick
Photograph by Roddy Addington - © All Rights Reserved.

[ Deep mountain hollows had a high impact during January 1998,
with only a few exceptions into some middle elevation settings ].

Snow density data from the National Weather Service Cooperative Stations in Clintwood, and on Long Ridge of Sandy Ridge, illustrate this well.

At Clintwood 1 W, just outside of town, the morning of December 19 found a foot of snow having fallen with 1.92" of melted water content.  Since 0.17" of this initially fell as rain, that meant 12.0" of snowfall contained 1.75" of water ( about 0.15" of water per 1.0" of snow ). 

The snow to water ratio, or snow density, 
at Clintwood 1 W on this event was between 
6:1 and 7:1 .

Snow cores taken at the height of the event, found the SNOW DENSITY reached 6:1, while the mean through December 21 was near 7:1 ( 13.5" of snowfall yielded 1.90" of total water content ).

[ As water became concentrated, following rain, a snow core on 5" of snow depth generated 1.22" of water content on December 30 at Clintwood 1 W.  This generated a density of approximately 4:1, 
with 0.24" of water content per 1.0" of snow. 

Such concentrations are common over time, with 0.42" of water content per 1.0" of snow being at one point obtained in the wake of the Jan 1998 event ].

Long Ridge of the Tennessee Valley Divide
National Weather Service MMTS Temp Sensor at Nora 4 SSE
Photograph by Wayne Riner - © All Rights Reserved.

Wayne & Genevie Riner at Nora 4 SSE, on beautiful Long Ridge of Sandy Ridge, got 1.97" of melt water out of 15.5" of snowfall ( 16" ground depth ) into morning hours of December 19.

This generated a snow density of about 8:1 at their elevation of 2650 feet above sea level ( 1090 feet higher than Clintwood 1 W ).

On the entire event, 17.1" of snowfall generated 2.12" of total melt for a snow density of just over 8:1 ( i.e., 1.00" of water in 8" snow ).

Magical Colors on Long Ridge - December 22, 2009
Photograph by Wayne Riner - © All Rights Reserved.

However, due to more wind blowing across Long Ridge there was not as much damage as occurred just off the crest ( the gusty wind helping to blow some of the WET snow off trees ).

In locations around the elevation of Long Ridge, but not having as much wind, more damage was reported.

During January 1998 snow densities lowered above 2000 feet, into the 10:1 to 15:1 range, which translated to a MEGA snow dump and little tree damage across mid-upper elevations.

During December 2009 snow densities appear to have lowered into the 10:1 to 12:1 range above 3000 feet, with again a MEGA snow dump across the High Knob highcountry and much less tree damage than within lower elevations.

[ Snow densities appeared to lower significantly within the 2500-3000 foot elevation zone of the High Knob Massif, toward the side impacted most by its Thermally Indirect Mesoscale Circulation ]. 

For reference, while snow densities can vary greatly during any given storm at the same location, or between locations, large variations seen in data are often the result of measurement errors or rain gauge undercatches.

The Snow Booklet, from the Colorado 
State University Climate Center, says:

"regardless of location, latitude, and elevation, most new snow densities fall in the range from 0.04" ( 25:1 ) to 0.10" ( 10:1 ), with peak frequencies centered between 0.06" ( 17:1 ) and 0.09" ( 11:1 )."

While that is true in the MEAN, there are notable and important exceptions such as occurred during the great January 1998 and December 2009 storm events.

Smith Cemetery on Long Ridge - December 22, 2009
Photograph by Wayne Riner - © All Rights Reserved.

Opposite EXTREME
LOW Density Snow

Roddy Addington said a drive upward into the High Knob highcountry during afternoon hours of January 6 was like driving through a great tunnel! 

A tunnel of heavily RIME laden trees standing amid a deep and highly varied snowpack.

Frozen HIGH DENSITY snow on the 
bottom + LOW DENSITY (fluffy) on top! 

For more great photographs please visit:

High Knob Massif - January 6, 2010
Photograph by Roddy Addington - © All Rights Reserved.

[ NOTE: Conditions in the High Knob Massif are EXTREMELY bad, with only the MAIN roads being opened. 

NO ONE should drive up there unless absolutely necessary and equipped with 4x4, chains, winter survival gear, cell phone, and notification of destination.

The storm coming in during January 7-9 could make travel impossible across the highcountry, with heavy snow, significant drifting, and life-threatening wind chill factors ].

Recent Example: Snowfall received during the January 1-6 period of 2010 has been RADICALLY different in nature from that observed during the Mega-disaster event.

It offers another example, at the other end of the snow density spectrum, which departs from the MEAN range noted by Colorado State Climate Lab studies.

On Long Ridge at Nora 4 SSE, a total of 10.7" of snow up through 7 AM on January 6 generated a total water content of just 0.28" ( 38:1 density ).  That translated to only 0.03" of water per 1.0" of snow.

EXTREMELY LOW density snowfall
( FLUFFY, broome sweeping snow )!

[ Max densities observed across lower elevations during December 18 contained 0.28" of water in just 1.7" of snowfall ]. 

Snowfall totals of 12" to 15" have been common in upper elevations of the High Knob Massif during January 1-6, but significant settlement has left much less total FLUFF covering the still DEEP pack of OLD SNOW ( especially across northern slopes ).

Darlene Fields measured 13" of snow depth on her back deck during the afternoon of January 5, before a couple more inches fell into early on January 6.  Snow depths across upper north slopes of the massif, west to southwest of High Chaparral where the biggest Dec 18-19 hit occurred, are around twice as deep as in High Chaparral 
( amid the worst or ''best'' places ).

Snow densities at times, during early January 2010, have been as low as 50:1 ( 0.02" of water 
in 1.0" of snow ).

The good news, one can literally have FEET of very low density snowfall without weighing down trees and causing power outages!

Case in point, the great SUPERSTORM Blizzard of March 1993, with
2 to 5 FEET of snow, caused VERY few power outages due to its LOW DENSITY ( high snow to water ratios ).

The Bottom Line: Snow Density is EXTREMELY Important!

The lower density of snowfall across upper elevations of the High Knob Massif ( above 3000 feet ) during the December 2009 MEGA-dump, like in January 1998, was again testified to by a distinct lack of significant tree damage ( compared to that which occurred across lower-middle elevations of the massif area ).

Meanwhile, the greater depth of the isothermal layer below 3000 feet, verses that observed during January 1998, accounted for the MUCH more widespread damage.

However, it is a bit more complex, with another important aspect to be considered.

The same amount of water equivalent will produce MUCH more snow depth in LOW DENSITY verses HIGH DENSITY snowfall.

The above fact accounts for a couple of additional factors, since the overall snow density observed during December 18-19, 2009 was somewhat lower at all elevations vs. January 27-28, 1998.

1 ).  Snow depths became greater during December 2009 within the isothermal layer vs. January 1998, resulting in more weight per unit area and MORE SIGNIFICANT damage across a MUCH larger area ( i.e., a MEGA-disaster ). 

2 ).  Snow depths remained less across upper elevations of the High Knob Massif vs. January 1998; although, they were still the greatest depths reported across the region into morning hours of December 19 and were associated with truly EXTREME RATES of snowfall ( up to 6"+ per hour ).

So now two factors emerge which clearly illustrate why this was a greater disaster than January 1998:

Depth of the Isothermal Layer
( greatly increased size of impact zone )

Lower but still HIGH Snow Density,
within the isothermal layer itself
( more total WET snow = more weight per unit area ).

A heavy, wet snow across a much larger portion of the mountain region, impacting a much greater proportion of the population than in 1998.

Regional Snowfall Totals

The December 18-20 period brought significant snow to much of the region, with a few graphics from National Weather Service Forecast Offices 
( NWSFO ) highlighting the distributions.

Graphic Courtesy of the Jackson, Kentucky NWSFO

Eastward across Virginia storm total snowfall amounts were very heavy, but generally less to much less than those observed within upper elevations of the High Knob Massif.

Storm Snowfall Totals Across Blacksburg, VA CWA

A recap of the storm, including animated surface and satellite images, can be found at the following link courtesy of the Blacksburg NWSFO:

Doug Niemi and Maureen Thompson, of Grayson Highlands State Park, reported 14" to 15" of mean snow depth in the Park.  Electricity was out for around 2.5 days, with lots of tree damage due also to a Christmas ice storm ( when power was lost again ) which followed the December 18-19 event along eastern slopes of the Blue Ridge.

Richard Kretz, photographer & naturalist, shared some nice photographs he took in the Pinnacle Natural Area Preserve ( NAP ) after sunshine returned on December 22, 2009.

Cedar Bent By Snow
Photograph by Richard Kretz - © All Rights Reserved.

[ Ecologically rich Pinnacle NAP is located in Russell County, where Big Cedar Creek cuts downward through calcareous stratas to join the magnificent Clinch River ].

Pinnacle NAP - Big Cedar Creek - December 22, 2009
Photograph by Richard Kretz - © All Rights Reserved.

Richard reported 6-8" of snow depth at his 
home on Green Valley Road, with a general 4-6" of depth left at majestic Pinnacle NAP on December 22.

Decorated Pitch Pine ( Pinus rigida )
Photograph by Richard Kretz - © All Rights Reserved.

Richard's report was close to the official tally measured at the Lebanon NWS Cooperative Station, where the December 18-20 period generated 8.6" of snowfall and 1.10" of 
total water.

Panorama of Big Falls of Cedar Creek - Dec 22
 Photograph by Richard Kretz - © All Rights Reserved.

In upper elevations of the Burkes Garden Basin, 
at 3300 feet, the official December 18-20 snowfall total was 13.4" ( 1.37" of water equivalent ).

Red Fox ( Vulpes vulpes ) Track at Pinnacle NAP
Photograph by Richard Kretz - © All Rights Reserved.

The December 18-20 storm event followed long-term climatology, in generating MUCH less precipitation across the upper Clinch River Basin than within the High Knob Massif.

In this case, however, with easterly winds, 
moisture extraction leeward of the High Knob high country only impacted locations to the west and southwest of its massif ( helping reduce snowfall from Big Stone Gap southwestward into Lee County of the HKL ).

Great Blue Heron ( Ardea herodias )
Photograph by Richard Kretz - © All Rights Reserved.

The main factor boosting High Knob Massif snow depths above those observed eastward in Virginia being formation of the unique circulation described previously, which worked with air rising across its high country from the east to enhance upward vertical motion along the cold side of the orographically created and anchored 
melting zone.

[ With strongest lift being generated above 
W-NW sections of the main massif ]. 

This increased snow depths from 24" in the Robinson Knob and High Chaparral section of the massif to around 36" within the main crest zone, from Eagle Knob and Camp Rock southwest across Little Mountain and the Big Cherry Basin into upper portions of the Stock-Cove Creek basins ( approximate storm snowfall totals of 27" to 38" ). 

The only other locations that approached these depths in the southern Appalachians were the highest elevations of the Great Smokies, on Mount LeConte, Tn., ( 32" depth ), and the summit level of Mount Mitchell, Nc., ( 28" ), with build-up into December 21 via a continuation of upslope snow showers.

Storm Snowfall Totals - NWS Greenville-Spartanbrug SC

Snow densities were generally lower toward the east, where some cold air wedging along eastern flanks of the Blue Ridge supported a cooler vertical column.  While damage still occurred during the December 18-19 event, it was MUCH less significant than what occurred within the MEGA-disaster zone chronicled on this website.

[ Kenneth Batty, climate historian extraordinaire, of the Charleston, West Virginia NWSFO, taught me years ago that snow DEPTH is what the general public most relates too.  Therefore, in this storm chronicle I have focused most upon the depth of snow, especially as it related to observations within upper elevations of the High Knob Massif.

In reality, however, it should be noted that the 24" of snow depth shown in the pictures by my friend Otis Ward, for example, was actually associated with a greater FALL of snow, since such a heavy mass of wet snow will compress and pack down the first inches which accumulated.

If it had been possible to observe the snow fall 
by "official" methods, of measuring the snow and sweeping it off of a board every 6 hours, the TOTAL FALL would have been greater than the 2 feet seen in the pictures.

Snow settles, compresses, sublimates, melts, and blows to alter the DEPTH on the ground over time, such that the official method described ( designed and adopted by Colorado State University Snow Lab Studies ) strives to reduce these factors to yield a more accurate value for the true fall of snow.

Low density snowfall, such as observed during January 1-12 of 2010, develops the most extreme differences over time between what actually FALLS and subsequent DEPTHS due to a very large settlement factor with time on FLUFFY snow 
( the sometimes called FLUFF factor ).

Due to rapid settlement with time on fluffy, low density snow, MUCH more often falls than is observed later on the ground after settlement 
( sublimation in sub-freezing air and melting in above freezing air enhancing the observed differences )].

Final Comments

This was a storm event of historic proportions 
with respect to its impact upon residents of Dickenson, Wise, and Buchanan counties, 
as well as the MASSIVE damage it caused.

The true impact of the December 18-19, 2009 event may never be fully known, with regard to the stress and strain placed upon our elderly, sick, and those isolated in homes and rural mountain locations for long periods of time.

[ As of January 22, 2010 some remain without 
phone service in Wise & Dickenson counties ].

Pre-storm forecasts for counties across far southwestern Virginia placed too little emphasis on snow density, and the possibility of a crippling fall of wet snow with massive power outage potential, given the analog event of January 1998 as a guide.

Perhaps no one could have known this event would be so destructive, but upon its unfolding stronger and more aggressive actions needed to be taken immediately by everyone with LIVE communication capabilities.

I sent several emails out during the late afternoon of December 18 to news media and the NWSFO to relay how quickly conditions were deteriorating in Wise County, and gave a phone report to the NWSFO, upon their request, for Dickenson County (by that point, however, it was simply becoming frantic here with trees cracking, poping, falling, and communications going out).

The remainder of the evening was then spent by candle and flash lights, as I worked to put two 8 foot long 2 x 2 boards together as tree limb shakers.

Of special concern was a large white pine in the back yard beneath which sat our generator.  I would reach upward as high as possible amid the whiteout of snow to shake limbs vigorously in order to lessen their load.

It worked for limbs facing the house, which I could reach, and may have prevented the tree from overturning into the house itself.  Otherwise, the snow stripped most of its other limbs, with large piles of broken limbs on each side of the generator by the next morning. 

The first of MANY jobs ahead was clearing snow and debris to get into the generator (having a generator was not as good as it may sound, as a MAJOR problem with respect to it became one of finding FUEL).

I dug a hole into a small stream which runs outward from an isolated mountain hollow behind our home, where no one lives, and used it for filling gallon jugs to flush the toilet.

I know my family was blessed since we had made some preparations for a disaster in advance, and had this source of water.

The greatest blessing of all for EVERYONE, however, was the fact that this Miller A Cyclone did NOT tap arctic air and pull it across the mountains in its wake!

If an air mass like experienced during January 2010 had hit, there would have been MANY deaths (i.e., many more than may ever be either directly or indirectly attributed to this event).

It was a MEGA-disaster, which will take a long time to yet recover from, but it could have been worse!

[ NOTE: Given all the debris left in the wake of this event, future weather related concerns include high wind settings and high water events ( with MUCH debris along and within creeks ) ].

Awesome Photograph
Along The Tennessee Valley Divide
Snowbound In The Highlands - December 22, 2009
Photograph by Wayne Riner - © All Rights Reserved.

Update - NOAA Ranks Storm:
But Leaves Local Mountains OUT?

December 18-21 Storm: Category 3 ( MAJOR )

The new Northeast Snowfall Impact Scale 
( NESIS ) recently ranked the December 2009 storm barely within the "MAJOR" category, with 
a 4.03 rating.  The minimum rating for a MAJOR winter storm is 4.00 .

Most interesting, the NOAA preliminary snowfall map places the High Knob Massif, Wise Plateau, and Tennessee Valley Divide in the same snowfall total range as the Tri-Cities of northeastern Tennessee!

[ Note this is snowFALL totals, not snow DEPTHS, with snowfall totals on the entire event being greater than observed depths ].

The only portion of the High Knob Landform that reached into the 10-20" snowfall range was that which covers parts of northeastern Lee County into the Powell River Valley to Big Stone Gap!

[ Recall the 2" depth along the Powell River in Big Stone Gap ].

Of course, the REALITY of what happened locally has been completely missed on both the snowfall map and the storm ranking ( and has been on EVERY storm ranked by this system which I have reviewed ).

[ The rebuttal would be, this is a REGIONAL scale system that is not designed to depict local conditions which may vary over short distances.  That is all very good and well, as long as the locality in question is not named Boston, New York, D.C., or some other large population center! ].

The NESIS System is designed to rank winter storms in a manner somewhat like hurricanes, but clearly is heavily biased toward large population centers that get hit with storms producing snowfall totals of 10" or more.

Since this is a small population center, relative to large cities like Washington, D.C., Philly, Boston, and New York, EVERYONE here could be taken out by a winter storm and it would not make a blip on the map if other large regional population centers were NOT impacted.

The high snowfall amounts well documented across the High Knob Massif are UNKNOWN to this system.

The March 12-14, 1993 Blizzard was a Category 5 ( the highest ranking ) winter storm, due to its impact across such a large region with high total population.

March 1993 Blizzard - Category 5 ( EXTREME )

While that ranking can indeed be agreed upon by everyone in this region, the 46" to 58" of snowfall and depth across the High Knob Massif ( and 30" to 34" in Clintwood to Wise ) is again unknown to this system, and the above map ( not to mention the 10-25 foot drifts documented by VDOT ).

A storm ranking system with good intentions, but CLEARLY biased and lacking for folks like US!

[ Some in Wise and Dickenson counties still DO NOT have phone service more than A MONTH after this event ].

My views as a climate researcher on the NESIS System:

1 ).  Hurricanes are ranked according to atmospheric parameters, often BEFORE they impact any human population centers, and without regard to human population centers.

2 ).  Winter Storms should also be ranked according to atmospheric parameters, in order to PREVENT the blatant discrimination which arises due to the current population bias.

While a winter storm which impacts Boston is clearly more disruptive to the NATION as a whole, in terms of air travel, for example, than one which only strikes the rural Appalachians, we should not as scientists be in the business of establishing rankings based upon human suffering and total population size.

For example, millions may suffer from a winter storm in Boston ( or along an elongated corridor ) but who should say that they suffered MORE than folks in rural mountain locations with a population in the tens of thousands, or even less?

It might therefore be better to rank Winter Storms like Hurricanes, based solely upon their atmospheric parameters, name them, and then RETIRE those names of the great ones which end up causing massive damage and/or suffering ( after the fact ).

[ Only naming the winter storms which meet specific atmospheric criteria, such as minimal hurricane status or greater, and skipping the "tropical storm" naming stage for winter storms ].

My views.