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A Story Of Sleet and Drought

Article from 06 Feb 2009

Despite the recent winter storm and the wettest year on record ending just 13 months ago, much of Oklahoma is now in a drought. North-central Oklahoma thus far has been spared from the abnormally dry conditions.
Oklahoma can be a state of extremes, particularly in the winter, with springlike heat followed just hours later by bitter cold, or torrential, flooding rains followed by literally weeks of sunshine. This month we'll be doing a double-header that pays tribute to these extremes, chronicling two opposite ends of the weather spectrum that we've seen here in Oklahoma over the last month. On one end, a winter storm that left several inches of sleet (or, if you prefer, ice pellets) on the ground. On the other, a developing drought across much of the state.

Let's begin with that winter storm, which moved through central Oklahoma during Jan. 26th and 27th. Though winter storms are not uncommon in this region (as evidenced by last winter's major ice storm ), seeing such a large accumulation almost entirely of sleet is rather rare. To receive long-lasting, accumulating sleet requires atmospheric conditions to remain within a narrow range for a relatively long time. Because atmospheric conditions often change rapidly during the passage of a strong storm system, it is more common to see sleet mixing with other precipitation during a transition from rain (or freezing rain) to snow, or vice-versa.

For sleet to fall, there must be a layer of above-freezing air aloft, but sub-freezing air near the surface. Precipitation which begins as snow melts into rain as it passes through the warm layer. The raindrops then re-freeze as they pass through the cold near-surface layer, forming the small, icy balls characteristic of sleet. Also, the cold air near the surface must be relatively deep (on the order of a kilometer or more), or the raindrops will not have time to re-freeze fully, and freezing rain will result instead of sleet. Relatively deep arctic air was in place over most of Oklahoma at the time of the sleetstorm, with warm air being drawn over it – perfect conditions for sleet.

Though up to three inches of sleet accumulation was observed in regions near and to the south and east of Norman, just 0.43 inches of liquid equivalent was measured in Oklahoma City (OKC). Liquid equivalent is simply the amount of water you get when you melt down frozen precipitation. The liquid equivalent can vary widely – for snow, it can be as little as 1 inch for every 20 inches of snow, while for freezing rain, the ratio is near 1 to 1. This 0.43 inches of liquid is the only precipitation that has been recorded in OKC this year, leading us nicely to our next point – the developing drought.

Looking back, 2007 was the wettest year on record for much of central Oklahoma. OKC, for example, received 56.95 inches of rain during the year – a full 20 inches above normal! Early 2008 was more of the same; by mid-August, OKC was running nearly 10 inches above normal for the year. At this point, the pendulum abruptly swung the other way; in the 6 months since then, only a total of 4 inches of rain have been observed in OKC.

Because of the recent dearth of precipitation, much of central and southern Oklahoma has been thrown from the frying pan into the fire – or in this case, from flood to drought. OKC, which we've been using as an example, is now classified as “D0”, or “abnormally dry”, in the National Drought Mitigation Center's Jan. 29th analysis. Farther to the south, “D1 (Moderate drought)” and “D2 (Severe Drought”) are seen as you approach the red river, as shown in the image above. Under the NDMC system, drought is rated in a manner similar to the F-scale for tornadoes, increasing from D0, the least severe, up to D4 (Exceptional drought), the most severe.

Looking ahead, the future remains uncertain. There is hope to break the drought as the spring storm season approaches, as spring is climatologically the wettest season in Oklahoma. However, the Climate Prediction Center's seasonal outlooks paint a hazy picture, calling for “equal chances” of below normal, normal, or above normal precipitation. One thing is for certain – with the growing season fast approaching, and wildfire danger elevated by the dry conditions, it won't just be thunderstorm enthusiasts who have their eyes to the skies looking for signs of rain this spring.





Story is © Nate Snook, 2009
Title Date Author
A Cool, Wet End to Summer 15 Sept. 2009 Nate Snook, 2009
Can't Beat the Heat 12 Jul. 2009 Nate Snook, 2009
VORTEX 2: Chasing Down the Storm May 29, 2009 Nate Snook, 2009
The Dryline that Set the State Ablaze 14 April 2009 Nate Snook, 2009
Fire Down Under 06 Mar 2009 Nate Snook, 2009
A Story Of Sleet and Drought 06 Feb 2009 Nate Snook, 2009
A Winter Travel Parable 06 Jan 2009 Nate Snook, 2009
Winter in Oklahoma 02 December 2008 Nate Snook, 2008
The Weather and the Election 01 Nov 2008 Nate Snook, 2008
Autumn Arrives 01 October 2008 Nate Snook, 2008
Active Atlantic 03 Sept 2008 Nate Snook, 2008
Clearing the Air for the Olympics 1 August 2008 Nate Snook, 2008
The Canals of… Cedar Rapids? 7 July 2008 Nate Snook, 2008
The Storms of May 2008 2 June 2008 Nate Snook, 2008
The First EF5 – Greensburg: One Year Later 05 May 2008 Nate Snook, 2008
Meltdown 02 April 2008 Nate Snook, 2008
Leap Year: Climate meets Astronomy meets Society 3 March 2008 Nate Snook, 2008
Indecision 2008: Southern Plains Edition February 2008 Nate Snook, 2008
Anatomy of an Ice Storm January 2008 Nate Snook, 2007
Winter starts when? December 2007 Nate Snook, 2007
The Perfect Firestorm November 2007 Nate Snook, 2007
Rainfall Record Ahead? October 2007 Nate Snook, 2007
Erin - An Unusual Tropical Storm September 2007 Nate Snook, 2007
A Slow Start to the NATL TC Season August 2007 Nate Snook, 2007
Tropical Depression Norman? July 2007 Nate Snook, 2007
Spring 2007 Among Wettest Ever in Central Oklahoma June 2007 Nate Snook, 2006
Wet Winter Ahead? Late 2006 Steve Irwin, 2006
Oklahoma: Can't Beat the Heat! August 2006 Kevin Goebbert, 2006
Oklahoma Gets Some Rain May 2006 Kevin Goebbert, 2006
© 2008 Oklahoma Weather Lab
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The University of Oklahoma, School of Meteorology