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Study Finds Less Gloomy Outlook for Subtropical Rainfall


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    Rosenstiel School researchers challenge previous understanding of drying projections for the climatic region

    rainfall-studyMIAMI, Fla. (November 14, 2016)—A new study found that rainfall over land in the subtropics—including in the southeastern U.S.—will not decline as much as it does over oceans in response to increased greenhouse gases. The study challenges our previous understanding of the drying that will occur in subtropical regions and suggests its impact on people living in these regions could be less severe than initially thought.

    “The lack of rainfall decline over subtropical land is caused by the fact that land will warm much faster than the ocean in the future—a mechanism that has been overlooked in previous studies about the subtropical precipitation change,” said Jie He, a postdoc in Princeton University’s Program in Atmospheric and Oceanic Sciences and former graduate student at the Rosensteil School of Marine and Atmospheric Science who was the lead author of the study.

    In the study, He and Rosenstiel School Professor Brian Soden used an ensemble of climate models to show that the rainfall decreases occur faster than global warming and, therefore, another mechanism must be at play. They found that direct heating from increasing greenhouse gases is causing the land to warm faster than the ocean and that the associated changes in atmospheric circulation are driving the rainfall decline over the oceans, rather than land.

    Previously, subtropical rainfall changes have been attributed to two mechanisms related to global warming: greater moisture content in air that is transported away from the subtropics, and a pole-ward shift in circulation. While both mechanisms are present, this study shows that neither one is responsible for the rainfall decline.

    “It has been long accepted that climate models project a large-scale rainfall decline in the future over the subtropics. Since most of the subtropical regions are already suffering from rainfall scarcity, the possibility of future rainfall decline is of great concern,” said Soden, the co-author of the study. “However, most of this decline occurs over subtropical oceans, not land, due to changes in the atmospheric circulation induced by the more rapid warming of land than ocean.”

    Most of the reduction in subtropical rainfall occurs instantaneously with an increase of greenhouse gases, independent of the warming of the earth’s surface, which occurs much more slowly. According to the authors, this indicates that emission reductions would immediately mitigate subtropical rainfall decline, even though the surface will continue to warm for a long time.

    The study, titled “A re-examination of the projected subtropical precipitation decline,” was published in the November 14 issue of the journal Nature Climate Change. He is currently at the NOAA Geophysical Fluid Dynamics Laboratory in Princeton, New Jersey.

     

     

    Fast rainfall decline vs. slow surface warming

    Image shows the clear difference in the rate of global surface warming (left panel) and the rate of subtropical rainfall decline (indicated by the brown shading in the right panel) when forced with an instantaneous increase of CO2. This is the main evidence to show that the subtropical rainfall decline is unrelated to the global surface warming.

    Credit: Jie He, Ph.D., Princeton University and Brian J. Soden, Ph.D., University of Miami Rosenstiel School of Marine and Atmospheric Science

     

     

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