In the last four weeks, I’ve been blogging about Hurricane
Sandy and its aftermath- flooding, destruction, and the potential hazards of
flood water. Prior to all of this
hurricane talk, the focus of this summer’s weather was the drought and high
temperatures. Called “the worst U.S.
drought in decades” reports indicate that after a month of improved conditions-
the drought “has deepened again.” Scientists
are unsure of an explanation other than “a simple lack of rain.”
More than half the U.S. has suffered a drought since the
summer of 2012; rain had begun to ease the situation beginning in
September. The U.S. Drought Monitor
reported as of November 21, 2012 that “60.1 percent of the lower 48 states were
in some form of drought.” The areas of
most drought intensity continue to be Texas, the Southwest, the Great Plains,
and almost all of Nebraska. There is
apparently no “clear, scientific explanation for why the drought is lingering.” Nebraska and the Dakotas to the north may see
the drought worsen. So what does this mean in the big picture? Why should we care? Well, drought causes damage to crops and vegetation; thus, food prices increase in an ever struggling economy. Drought also plays a role in the water supply to our communities.
The NC State University has a website that provides Climate
Education for K-12. This site has information and resources concerning all
types of climate and I found information linked to drought. Due to the “reduced amounts of precipitation for an extended period
of time can lead to the loss of plant life and crops. Without needed rainfall,
crops and animals can suffer serious declines, and food and water shortages can
occur.”
Figure A shows the most current picture of
drought in the United States.
There
are several types of drought:
1) Meteorological
drought is a long-term measurement of lower than normal precipitation.
2) Hydrological
drought is a lack of water in subsurface and surface terms. This includes the water supply that is held in
streams, lakes, groundwater and other types of reservoirs. Hydrologic droughts
tend to develop over an extended time period.
3) Agricultural
drought is when there is not enough water to sustain crops. Rainfall
deficits during the critical growth periods of a crop (different from crop to
crop) can result in large yield losses, or even complete crop loss.
Overfarming
techniques and deforestation also have serious consequences. “Overfarming takes
all the nutrients out of the soil that the plants/crops need to survive and
essentially “kills” or desertifies the land.”
Deforestation causes fewer trees to cover ground; thus, less water vapor
is able to saturate the air above the trees in order to form clouds and rain. The long term consequence of this- a
rainforest could “dry out and absorb less carbon dioxide because of reduced
plant growth.” Ultimately, adding “enormous”
amounts of carbon dioxide into the atmosphere, which I believe is the snowball effect of
global warming, extreme weather, and climate change.
Suhr, Jim. (2012, November 22). Drought worsens after weeks of slowly improving conditions. St.
Louis: Associated Press.
http://www.nc-climate.ncsu.edu/edu/k12/.droughteffects