Southeastern Section - 62nd Annual Meeting (20-21 March 2013)

Paper No. 4
Presentation Time: 8:00 AM-5:30 PM

RECORD SPRING 2012 HEAT WAVE ACCENTUATES A HISTORIC TREND TOWARD EARLIER ICE LOSS AND INCREASED TEMPERATURES IN WEST VIRGINIA COLD-AIR TRAPS


KITE, J. Steven, Geology and Geography, West Virginia University, P. O. Box 6300, 330 Brooks Hall, Morgantown, WV 26506-6300 and SMITH, Michael A., WV DNR, Droop Mountain Battlefield State Park, HC 64 Box 189, Hillsboro, WV 24946, jkite@wvu.edu

Historical accounts reveal many Central Appalachian cold-air traps regularly held seasonal ice several months later in the 19th and early 20thcenturies than during the last three decades. This ice decline and concurrent growing-season temperature increase are potentially lethal risks to boreal species living at many of these sites. Studies at the Little Beartown rock city at Beartown State Park and the algific talus slope at Ice Mountain National Natural Landmark suggest that ice has disappeared even sooner during the last 10-15 years. A record spring 2012 heat wave led to the loss of ice much earlier than any previous record, along with unusually warm spring and early summer temperatures in the cold-air traps.

A journal of annual holiday ice-cream making has shown Little Beartown ice persisted until after July 4th every year between 1985 and 1999, but only about half of the years since 2000. Hobo Pendant data and field observations show the disappearance of near-surface ice approximately correlates to the date when temperatures rise above +1˚C for the season. This +1˚C threshold has been crossed earlier in each of the last four years, punctuated by ice loss at Little Beartown on or about May 17thin 2012.

Nearly 10 years of continuous Hobo measurements at Ice Mountain shows a mean July 4thtemperature increase of ~1.8˚C between 2003-2009 and 2010-2012. Temperatures rose above +1˚C at two cold air vents in April 2012, a full 27 days earlier than any of the preceding nine years. Early June 2012 temperatures were 4.3˚C warmer than average, and 3.1˚C warmer than the previous record high.

Although accounts of ice lasting into September were common over a century ago, 21st Century measurements show both sites have cave-like (9 to11˚C) temperatures with little variability at the end of the water year. In 2012 temperatures approached seasonal averages through summer, and by September were only 0.2˚C and 0.3˚C above average at Little Beartown and Ice Mountain, respectively.