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NASA Explains 'Dust Bowl' Drought

This illustration shows how cooler than normal tropical Pacific Ocean temperatures (blues) and warmer than normal tropical Atlantic Ocean temperatures (red and orange) contributed to a weakened low level jet stream and changed its course.

The jet stream normally flows westward over the Gulf of Mexico and then turns northward pulling up moisture and dumping rain onto the Great Plains. During the 1930s, this low level jet stream weakened, carrying less moisture, and shifted further south. The Great Plains land dried up and dust storms blew across the U.S.


This is the standard definition version Dust Bowl Climate Conceptual animaiton MPEG.    This is the standard definition version Dust Bowl Climate Conceptual animaiton MPEG.
Duration: 10.0 seconds
Available formats:
  320x240 (30 fps) MPEG-1   1 MB
  320x240     JPEG         11 KB
  720x486     Frames
  720x480 (29.97 fps) MPEG-2   4 MB
  640x480 (29.97 fps) MPEG-4   3 MB
  320x240 (30 fps) X-FLV       549 KB
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This is the high resolution still illustrating abnormal climate during Dust Bowl in the 1930's.    This is the high resolution still illustrating abnormal climate during Dust Bowl in the 1930's.

Available formats:
  3000 x 2025     TIFF 5 MB
  150 x 101         JPEG       3 KB
  320 x 216         JPEG     10 KB
  75 x 50             JPEG       1 KB


This is the high resolution still illustrating the normal climate of the region.    This is the high resolution still illustrating the normal climate of the region.

Available formats:
  3000 x 2025     TIFF 4 MB
  320 x 216         JPEG     10 KB

Animation Number:10033
Completed:2004-03-18
Animator:Susan Twardy (HTSI) (Lead)
Scientist:Siegfried D. Schubert (NASA/GSFC)
Writer:Rani Chohan (NASA/GSFC)
Goddard TV Tape:G2004-020
Keywords:
SVS >> Byrne
SVS >> Drought
SVS >> Earth Science
SVS >> Gonnelli
SVS >> Precipitation
SVS >> Sea Surface Temperature
 
 
Please give credit for this item to
NASA/Goddard Space Flight Center Conceptual Image Lab


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