The increasing importance of atmospheric demand for ecosystem water and carbon fluxes

Kimberly A. Novick (), Darren L. Ficklin, Paul C. Stoy, Christopher A. Williams, Gil Bohrer, A. Christopher Oishi, Shirley A. Papuga, Peter D. Blanken, Asko Noormets, Benjamin N. Sulman, Russell L. Scott, Lixin Wang and Richard P. Phillips
Additional contact information
Kimberly A. Novick: Indiana University, School of Public and Environmental Affairs
Darren L. Ficklin: Indiana University
Paul C. Stoy: Montana State University
Christopher A. Williams: Clark University, Graduate School of Geography
Gil Bohrer: The Ohio State University, Environmental & Geodetic Engineering
A. Christopher Oishi: USDA Forest Service, Southern Research Station, Coweeta Hydrologic Laboratory
Shirley A. Papuga: University of Arizona, School of Natural Resources and the Environment
Peter D. Blanken: University of Colorado
Asko Noormets: North Carolina State University
Benjamin N. Sulman: Princeton University
Russell L. Scott: Southwest Watershed Research Center, USDA-ARS
Lixin Wang: Indiana University-Purdue University Indianapolis (IUPUI)
Richard P. Phillips: Indiana University

Nature Climate Change, 2016, vol. 6, issue 11, 1023-1027

Abstract: During periods of hydrologic stress, vegetation productivity is limited by soil moisture supply and atmospheric water demand. This study shows that atmospheric demand has a greater effect in many biomes, with implications for climate change impacts.

Date: 2016
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DOI: 10.1038/nclimate3114

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