Articles | Volume 21, issue 11
https://doi.org/10.5194/hess-21-5517-2017
https://doi.org/10.5194/hess-21-5517-2017
Research article
 | 
13 Nov 2017
Research article |  | 13 Nov 2017

Future shift of the relative roles of precipitation and temperature in controlling annual runoff in the conterminous United States

Kai Duan, Ge Sun, Steven G. McNulty, Peter V. Caldwell, Erika C. Cohen, Shanlei Sun, Heather D. Aldridge, Decheng Zhou, Liangxia Zhang, and Yang Zhang

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by Editor and Referees) (09 Sep 2017) by Jan Seibert
AR by Kai Duan on behalf of the Authors (10 Sep 2017)  Manuscript 
ED: Referee Nomination & Report Request started (12 Sep 2017) by Jan Seibert
RR by Brian Finlayson (21 Sep 2017)
RR by Anonymous Referee #1 (26 Sep 2017)
ED: Publish subject to technical corrections (03 Oct 2017) by Jan Seibert
AR by Kai Duan on behalf of the Authors (04 Oct 2017)  Author's response   Manuscript 
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Short summary
We examined the potential roles of major climatic variables (including precipitation, air temperature, solar radiation, specific humidity, and wind speed) in altering annual runoff, which is an important indicator of freshwater supply, in the United States through the 21st century. Increasing temperature, precipitation, and humidity are recognized as three major climatic factors that drive runoff to change in different directions across the country.