Water table depth tied to droughts in Great Plains

Oct 01, 2008
Dust Bowl farm in Coldwater District, near Dalhart, Texas. This farm is occupied. Others in this area have been abandoned. Photographed by Dorothea Lange in June 1938. Image from the Library of Congress, Farm Security Administration-Office of War Information Collection.

(PhysOrg.com) -- Will there be another “dust bowl” in the Great Plains similar to the one that swept the region in the 1930s? It depends on water storage underground. Groundwater depth has a significant effect on whether the Great Plains will have a drought or bountiful year.

Recent modeling results show that the depth of the water table, which results from lateral water flow at the surface and subsurface, determines the relative susceptibility of regions to changes in temperature and precipitation.

“Groundwater is critical to understand the processes of recharge and drought in a changing climate,” said Reed Maxwell, an atmospheric scientist at Lawrence Livermore National Laboratory, who along with a colleague at Bonn University analyzed the models that appear in the Sept. 28 edition of the journal Nature Geoscience.

Maxwell and Stefan Kollet studied the response of a watershed in the southern Great Plains in Oklahoma using a groundwater/surface-water/land-surface model.

The southern Great Plains are an important agricultural region that has experienced severe droughts during the past century including the “dust bowl” of the 1930s. This area is characterized by little winter snowpack, rolling terrain and seasonal precipitation.

While the onset of droughts in the region may depend on sea surface temperature, the length and depth of major droughts appear to depend on soil moisture conditions and land-atmosphere interactions.

That’s what the recent study takes into account. Maxwell and Kollet created three future climate simulations based on the observed meteorological conditions from 1999. All included an increase in air temperature of 2.5 degrees Celsius. One had no change in precipitation; one had an increase in precipitation by 20 percent; and one had a decrease in precipitation by 20 percent.

“These disturbances were meant to represent the variability and uncertainty in regional changes to central North America under global model simulations of future climate,” Maxwell said.

The models showed that groundwater storage acts as a moderator of watershed response and climate feedbacks. In areas with a shallow water table, changes in land conditions, such as how wet or dry the soil is and how much water is available for plant function, are related to an increase in atmospheric temperatures. In areas with deep water tables, changes at the land surface are directly related to amount of precipitation and plant type.

But in the critical zone, identified here between two and five meter’s depth, there is a very strong correlation between the water table depth and the land surface.

“These findings also have strong implications for drought and show a strong dependence on areas of convergent flow and water table depth,” Maxwell said. “The role of lateral subsurface flow should not be ignored in climate-change simulations and drought analysis.”

The simulations were performed on LLNL’s Thunder supercomputer and the work was supported by the LLNL climate change initiative.

Provided by Lawrence Livermore National Laboratory

Explore further: Global warming 'pause' since 1998 reflects natural fluctuation, study concludes

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Velanarris
2.6 / 5 (5) Oct 01, 2008
This summation is very, very misdirected.

Siegfried Schubert of NASA's Goddard Space Flight Center, Greenbelt, Md., and colleagues used a computer model developed with modern-era satellite data to look at the climate over the past 100 years. The study found cooler than normal tropical Pacific Ocean surface temperatures combined with warmer tropical Atlantic Ocean temperatures to create conditions in the atmosphere that turned America's breadbasket into a dust bowl from 1931 to 1939. The team's data is in this week's Science magazine.

These changes in sea surface temperatures created shifts in the large-scale weather patterns and low level winds that reduced the normal supply of moisture from the Gulf of Mexico and inhibited rainfall throughout the Great Plains.


From http://www.nasa.g...owl.html
axemaster
2 / 5 (4) Oct 01, 2008
"the length and depth of major droughts appear to depend on soil moisture conditions and land-atmosphere interactions"

Wow, I didn't know we were measuring time in meters, unless we decide to convert using the speed of light. The sounds like a square length*depth = area.

Why is grammar so ignored these days...?
superhuman
3.8 / 5 (4) Oct 02, 2008
This summation is very, very misdirected.


Why is it misdirected? What you quote is a completely different article.
gmurphy
4.5 / 5 (4) Oct 02, 2008
Velanarris, this article discusses research on the relationship of water table depth to the dust bowl. The article you reference discusses the development of the dust bowl due to changes in atmospheric conditions.
tkjtkj
1 / 5 (1) Oct 02, 2008
I agree with what seems to be the
point of the article: that low
water-table could be associated
with drought conditions. The fly
in this ointment is the
'direction' of that relationship.
GrayMouser
not rated yet Oct 02, 2008
I would also point out that surface soil moisture isn't directly proportional to the depth of the water table (unless the water table is very close to ground level) it is more of a function of the airborne moisture (since dry air will suck out surface moisture.)
Velanarris
2 / 5 (4) Oct 02, 2008
Velanarris, this article discusses research on the relationship of water table depth to the dust bowl. The article you reference discusses the development of the dust bowl due to changes in atmospheric conditions.


Superhuman and Gmurphy: Which aspect do you think would be of more relevance in determining the cause of a drought -

a) the absence of precipitation and air moisture

or

b) how far you have to dig down to find moisture

I'm pretty sure A would be the winner and would also directly affect B.