M.S. in Sustainability Management professor Ben Cook often tells his students that the past can provide critical lessons for how we manage sustainability challenges now and in the future. Thus, it is not surprising that Cook, whose research at the Earth Institute’s Lamont-Dougherty Earth Observatory focuses on drought, hydroclimate, and interactions between the land surface and climate system, recently found that the drought of 1934 was caused in part by an atmospheric phenomenon that may also be the reason for California’s current drought. Cook, along with fellow climate scientists Richard Seager and Jason Smerdon, focus on the 1934 drought in a study that was featured by the American Geophysical Union (AGU). You can read the full article below as well as here.
The 1934 drought was by far the most intense and far-reaching drought of the last 1,000 years in North America, and was caused in part by an atmospheric phenomenon that may have also led to the current drought in California, according to a new study.
Credit: NOAA/George E. Marsh Album
New research finds that the extent of the 1934 drought was approximately seven times larger than droughts of comparable intensity that struck North America between 1000 A.D. and 2005, and nearly 30 percent worse than the next most severe drought that struck the continent in 1580.
“We noticed that 1934 really stuck out as not only the worst drought but far outside the normal range of what we see in the record,” said Benjamin Cook, an environmental scientist at NASA’s Goddard Institute for Space Studies in New York City and lead author of a new paper that has been accepted for publication in Geophysical Research Letters, a journal of the American Geophysical Union.
The new study also finds that the same atmospheric pattern of a high pressure ridge over the West Coast deflecting away storms laden with rain last winter was also present over the area during the winter of 1933-34.
This ridging pattern has preceded some of the worst West Coast droughts, including the 1976 California drought—the beginning of a two-year dry spell which is widely regarded as one of the most severe droughts in the state’s history. The three-year drought currently crippling California will cost the state $2.2 billion in 2014 alone, and will likely continue through 2015, according to a recent report from the University of California, Davis.
Yet the current drought is nothing, so far, compared to what occurred in 1934, the start of a decade-spanning drought that would come to be known as the Dust Bowl and was one of the worst environmental disasters in the history of the United States.
The drought, which afflicted nearly 72 percent of the western United States, was likely made even worse by atmospheric effects from human-created dust storms, according to the new research. The new study suggests that such interactions between the land and the atmosphere may have an important role to play in drought severity, said Cook, who holds a joint appointment at Columbia University’s Lamont-Doherty Earth Observatory.
“These dust storms may have dried things out further and kicked 1934 into a really extreme event,” he said.
The new study used the North American Drought Atlas, a database of drought reconstructions dating back nearly 2,000 years that are based on tree-ring studies. It also analyzed records of air- and sea-surface temperatures and precipitation to show that the 1934 drought was the worst drought since 1000 A.D.
Using climate data and dust simulations, the authors also found that dust storms, which started from a lack of rain and poor agricultural practices could have intensified the 1934 drought and spread it throughout the western United States.
A combination of changes in sea surface temperatures and a lack of rainfall in the Northwest, Southwest, and across the Southern Plains kicked off dry conditions in the fall of 1933 that by the spring of 1934 would spread to the Central Plains and Midwest. Major dust storms – the scale of which had not been seen in North America since the Middle Ages—projected dust from the Central Plains as far east as the Atlantic Ocean, according to the new study.
Credit: Benjamin Cook
Some of the hardest hit areas– Midwestern states like Nebraska and Kansas—were downwind from where the dust storms originated. In these areas, dust particles accumulated in the atmosphere, reflecting incoming energy from the sun back into space. These dust-driven energy changes can disturb normal air circulation patterns, and block cloud formation and precipitation, leading to dry conditions, according to the new study.
California may be in the grips of a devastating drought, but “now we have the (Natural Resources Conservation Service), which helps to limit wind erosion and dust storm erosion,” Cook said. “They can reduce the chance of a 1934 event occurring again.”
The study, one of the first to examine how extreme conditions like dust storms evolve during decades-long dry periods, could help scientists better understand what causes these events and better predict them in the future, said Sigfried Schubert, a meteorologist at NASA’s Global Modeling and Assimilation Office, who was not involved in the study.
“It is such an important problem for society to be able to predict these major droughts,” he said.
This article was first published in the October 14, 2014 edition of the AGU Newsroom. You can view the full version of the article here.
Title: “The Worst North American Drought Year of the Last Millennium: 1934”
Authors:
Benjamin I. Cook: NASA Goddard Institute for Space Studies, New York, New York, USA, and Lamont-Doherty Earth Observatory, Palisades, New York, USA;
Richard Seager and Jason E. Smerdon: Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA.
