Dust Bowl ESS Analysis


 Discussion Home | Volcano | Dust BowlHurricane | Ocean | Final Project

 

 

Click here for Dust Bowl Discussion

 

 

DUST BOWL ESS Analysis

 

Problem Statement: 

The population of the American Southwest relies heavily on the Ogallala Aquifer as a primary water source, but water levels continue to decline. In the event of a prolonged drought affecting the area, what can scientists, farmers, and citizens do to effectively manage the limited water resources and avoid serious water shortages and dust bowl conditions in the area?

 

Opening Statement:

The Dust Bowl of the 1930s had serious effects on the atmosphere, hydrosphere, biosphere, and lithosphere. The consequences of a second dust bowl would be similar but magnified because the region supplies more people with water and crops than ever before. In addition, with increasing temperatures predicted well into the future for the area, the climate could change to include permanent or very long term drought conditions, as shown in the following graphic.

 

 

 

 

Recommendations/Possible Solutions:

         Cloud seeding, while controversial, is a potential solution to the lack of rain.  Possible techniques include inserting ice particles or inserting   

          water droplets in warm clouds that have the potential to rise and become larger droplets    

          

 

Relationships

 

Atmosphere

E>L>A>H>B

An excessively dry lithosphere was easily lifted by normal winds into the atmosphere, causing changes in weather patterns.

The dust formed large clouds, which blocked sunlight and further impacted weather conditions.

Dust in the air provided more substance for water molecules to cling to; as a result, the dust storms influenced weather conditions. However, precipitation may not have occurred in the area it was most needed, but rather downwind of that area.  

With more sediment in water sources, evaporation was reduced, leading to less water in the atmosphere. 

The area affected by the Dust Bowl is marked by a semi-arid climate.  It is believed that elevated sea temperatures and a change in the atmosphere known as El Nino further impacted/limited the amount of precipitation, exacerbating an already dry area.

 

 

E>A>B

Extreme amounts of dust put unprecedented amounts of contaminants into the atmosphere. This pollution can lead to respiratory complications for humans and animals in the affected area. Dust clouds could lead to bronchitis, ashtma, and chronic upper respiratory infections with effects being apparent for the long term. Complications will affect younger and older individuals more, as well as those already suffering from respiratory ailments.

 

E>A>B>B

Extreme amounts of dust in the atmosphere blocks out sunlight which leads to detrimental conditions for vegetation by not having sufficient sun to provide the energy needed for photosynthesis. A lower amount of vegetation equals a lesser food supply for both animals ands humans.

 

Hydrosphere

Dust fell into rivers, lakes, streams, and creeks, and wound up at shorelines. Some water sources became clogged or cloudy as a result; the shoreline took on a new shape and appearance. 

The addition of sediment caused a decrease in the water available for evaporation, leading to even drier conditions.

With a significant addition of sediment in water sources in a short period of time, the habitat of organisms changed faster than the organisms living in the hydrosphere could adapt. Some relocated. Others perished.  

Water patterns changed with the addition of sediment. The sediment influenced new formations along the banks and larger river deposits.

 

E>H>B

Excessive amounts of dust in the air will eventually settle into water sources, killing marine life that live in these waters as well as polluting drinking sources for animals and humans. Humans might be able to overcome this with our technology and water treatment plants, however animals will be at great risk.

  

Biosphere

Dust coated plants making photosynthesis and gas exchanges difficult. Plants suffered and some died.

Humans and other animals moved out of the area, possibly in hurry and without regard to further degradation of the soil.

With heavy particulates floating in the air, organisms likely experienced respiratory problems and even respiratory failures. As a result, some organisms died and others relocated. 

A reduction of oxygen-producing plants on land and algae in water reduced the amount of oxygen produced in the area. This altered the chemistry of the atmosphere and influenced changing weather patterns.  

A reduction of more vulnerable organisms (lower elements on the food chain) in the hydrosphere led to a reduction in the organisms that depended upon them. Such effects and consequences effectively represented natural selection. The reduction in more vulnerable organisms also influenced the chemistry of the water as it contained more decaying matter and less living matter.

Organisms that could not live in the dusty conditions relocated. Those organisms that depended upon the evacuees also left the area or perished. 

Dust coated plants and filled the lungs of animals, making photosynthesis and respiration difficult. Plants and animals suffered and some died.

  

Lithosphere

Excessive use of land for farming depleted the soil of water and minerals. Plants would not grow effectively, so roots were not holding down the soil. Normal winds easily picked up topsoil and carried it into the atmosphere. Much lithosphere was relocated from croplands to shorelines.

The normal process of composition and decomposition (where animals and plants would grow and eventually decay, enriching the soil) did not proceed normally. Where soils would be enriched by this cycle, instead they were blown away.

Topsoil is the most valuable part of the lithosphere for farming. As topsoil was transported from croplands to shorelines, it no longer became available for farming. The land left behind was harder and lower in the valued minerals. As a result, it was more difficult to farm. 

This “blank slate” created the conditions for primary succession to occur. 

Dust removed from one area was deposited in other areas by wind patterns. Some of that dust ended up in cities and towns where it was not needed. Other dust ended up clogging rivers.   

An excessively dry lithosphere was easily lifted by normal winds into the atmosphere, causing changes in weather patterns. 

Dust fell into rivers, lakes, streams, and creeks, and wound up at shorelines. Some water sources became clogged or cloudy as a result; the shoreline took on a new shape and appearance.

 

E>L>B>B

As dust settled into surrounding areas, it changed the makeup of the soil. Once nutrient rich soil now is mixed with dust that contains little to no valuable minerals. This new soil makeup affects local vegetation by providing less than ideal conditions. Lower vegetation levels means less food sources for animals and humans inhabiting the area.

 

Evidence

Dust Affecting Soil

http://www.erosioncontrol.com/march-april-2009/dust-control-stabilization.aspx 

 

Dust Affecting Respiratory Conditions

http://www.health.nsw.gov.au/factsheets/environmental/dust_storms.html 

 

Environmental Effects of Groundwater Depletion

http://web.mit.edu/12.000/www/m2012/finalwebsite/problem/groundwater.shtml#enveffects

 

Crop Rotation as a Possible Solution

http://www.telegraph.co.uk/earth/8359076/US-farmers-fear-the-return-of-the-Dust-Bowl.html

 

Purposeful Planting to Maximize Irrigation

http://www.telegraph.co.uk/earth/8359076/US-farmers-fear-the-return-of-the-Dust-Bowl.html

 

Cloud Seeding as a Possible Solution

 http://www.wdtinc.com/posts/2011/8/18/could_cloud_seeding_help_drought_stricken_areas  

 

El Nino as Cause of Dust Bowl in 1930's

http://weather.about.com/od/weatherfaqs/f/dustbowl.htm 

http://www.gsfc.nasa.gov/topstory/2004/0319dustbowl.html

 

Sea Surface Temperatures' Role in Creating Dust Bowl

http://weather.about.com/od/weatherfaqs/f/dustbowl.htm 

http://www.gsfc.nasa.gov/topstory/2004/0319dustbowl.html