![]() A dust storm approaches Stratford, Texas on April 18, 1935. Learn more... |
- Meteorological - a measure of departure of precipitation from normal. Due to climatic differences, what might be considered a drought in one location of the country may not be a drought in another location.
- Agricultural - refers to a situation where the amount of moisture in the soil no longer meets the needs of a particular crop.
- Hydrological - occurs when surface and subsurface water supplies are below normal.
- Socioeconomic - refers to the situation that occurs when physical water shortages begin to affect people.
For the continental U.S., the most extensive U.S. drought in the modern observational record occurred from 1933 to 1938, the "Dust Bowl" period. In July 1934, 80% of the U.S. was gripped by moderate or greater drought, and nearly two-thirds (63%) was experiencing severe to extreme drought. During 1953-1957, severe drought covered up to one half of the country.
![Image of dry, cracked earth Image of dry, cracked earth](https://webarchive.library.unt.edu/web/20120913074730im_/http://www.srh.noaa.gov/srh/jetstream/global/images/b.jpg)
There is nothing we can do to prevent droughts since they result from long-term shifts in storm tracks away from the affected region, or persistent wind patterns that reduce the flow of moisture into a region. Often, "blocking weather patterns" that feature persistent, stationary high-pressure regions over an affected area are observed with droughts.
While we can't control these extended dry periods, at NOAA we seek to...
- Understand the causes of long-lived droughts, such as in the 1930s Dust Bowl period.
- Improve our drought monitoring ability, including estimates of soil moisture and snow water storage.
- Determine the relationships between droughts and changes in greenhouse gases, aerosols, and land use.
Through these projects, we seek to improve our forecasts, and your warnings, of these events and the actions you should take to decrease their impacts in your community.