Figure : precipitation-and-humidity-projections

Drying Effect of Warmer Air on Plants and Soils

Figure 21.3

North Carolina State University, University of Illinois at Urbana-Champaign Department of Atmospheric Sciences, U.S. Department of Agriculture Northern Forests Climate Hub, U.S. Forest Service
Kenneth E. Kunkel, Laura Stevens, Liqiang Sun, Todd A. Ontl, Andrew Ballinger

This figure appears in chapter 21 of the Impacts, Risks, and Adaptation in the United States: The Fourth National Climate Assessment, Volume II report.

As air temperature increases in a warming climate, vapor pressure deficit (VPD) is projected to increase. VPD is the difference between how much moisture is in the air and the amount of moisture in the air at saturation (at 100% relative humidity). Increased VPD has a drying effect on plants and soils, as moisture transpires (from plants) and evaporates (from soil) into the air. (a) Cooler air can maintain less water as vapor, putting less demand for moisture on plants, while warmer air can maintain more water as vapor, putting more demand for moisture on plants. (b, c) The maps show the percent change in the moisture deficit of the air based on the projected maximum 5-day VPD by the late 21st century (2070–2099) for (b) lower and \(c) higher scenarios (RCP4.5 and RCP8.5). Sources: U.S. Forest Service, NOAA NCEI, and CICS-NC.

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This figure was created on May 30, 2017.

This figure was submitted on December 03, 2018.


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