Forces behind Devastating 'Dust Bowl' Drought Explained















Share on Tumblr

dust bowl drought

Image: COURTESY OF NOAA/HISTORIC NWS COLLECTION

The eight-year drought that plagued the central U.S. in the 1930s, immortalized in The Grapes of Wrath, wracked the Great Plains with devastating dust storms and affected two thirds of this country as well as parts of Mexico and Canada. Paramount to determining why the conditions were so severe and long-lasting is discerning what caused the drought to begin with. Findings published today in the journal Science suggest that unusual sea surface temperatures could be to blame.

"The 1930s drought was the major climatic event in the nation¿s history," explains lead study author Siegfried Schubert of the NASA Goddard Space Flight Center. "Just beginning to understand what occurred is really critical to understanding future droughts and the links to global climate change issues we¿re experiencing today."

Previous research had demonstrated a link between some droughts and peculiar patterns of sea surface temperatures in different parts of the world. Schubert and his colleagues used a computer climate model to analyze conditions during the past 100 years. They found that ocean temperatures, particularly in the tropics, heavily influenced the dry conditions experienced in North America. In the early 1930s, the waters of the tropical Pacific were cooler than normal, and those of the tropical Atlantic were warmer than normal. Those conditions, the scientists say, weakened the jet stream, a strip of fast-moving air that typically flows westward over the Gulf of Mexico before turning northward and depositing rain onto the Great Plains. In its altered state, the jet stream traveled farther south than usual, lessening precipitation over the central U.S. and compounding the drought conditions.


Other droughts that struck the U.S. also correspond to cooler tropical Pacific temperatures, the researchers report, but only the so-called Dust Bowl drought combined these condition with a warmer Atlantic Ocean. A better understanding of the conditions that caused severe climatic events of the past should help scientists better recognize and forecast potentially dangerous conditions in the future.



Comments

Add Comment
Leave this field empty

Add a Comment

You must sign in or register as a ScientificAmerican.com member to submit a comment.
Click one of the buttons below to register using an existing Social Account.

More from Scientific American

See what we're tweeting about

Scientific American Editors

Tweets could not be retrieved at this time

Free Newsletters


Get the best from Scientific American in your inbox

Solve Innovation Challenges

Powered By: Innocentive

  SA Digital
  SA Digital

Science Jobs of the Week

Email this Article

Forces behind Devastating 'Dust Bowl' Drought Explained

X
Scientific American MIND iPad

Tap into your MIND

Get Both Print & Tablet Editions for one low price!

Subscribe Now >>

X

Please Log In

Forgot: Password

X

Account Linking

Welcome, . Do you have an existing ScientificAmerican.com account?

Yes, please link my existing account with for quick, secure access.



Forgot Password?

No, I would like to create a new account with my profile information.

Create Account
X

Report Abuse

Are you sure?

X

Institutional Access

It has been identified that the institution you are trying to access this article from has institutional site license access to Scientific American on nature.com. To access this article in its entirety through site license access, click below.

Site license access
X

Error

X

Share this Article

X