Articles | Volume 24, issue 3
Hydrol. Earth Syst. Sci., 24, 1131–1143, 2020
https://doi.org/10.5194/hess-24-1131-2020
Hydrol. Earth Syst. Sci., 24, 1131–1143, 2020
https://doi.org/10.5194/hess-24-1131-2020

Research article 11 Mar 2020

Research article | 11 Mar 2020

Response of global evaporation to major climate modes in historical and future Coupled Model Intercomparison Project Phase 5 simulations

Thanh Le and Deg-Hyo Bae

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Interactive discussion

Status: closed
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: Reconsider after major revisions (further review by editor and referees) (08 Dec 2019) by Ryan Teuling
AR by Thanh Le on behalf of the Authors (09 Dec 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Jan 2020) by Ryan Teuling
RR by Jasper Denissen (08 Jan 2020)
RR by Brecht Martens (28 Jan 2020)
ED: Publish subject to minor revisions (review by editor) (28 Jan 2020) by Ryan Teuling
AR by Thanh Le on behalf of the Authors (08 Feb 2020)  Author's response    Manuscript
ED: Publish as is (10 Feb 2020) by Ryan Teuling
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Short summary
Here we investigate the response of global evaporation to main climate modes, including the Indian Ocean Dipole (IOD), the North Atlantic Oscillation (NAO) and the El Niño–Southern Oscillation (ENSO). Our results indicate that ENSO is an important driver of evaporation for many regions, while the impacts of NAO and IOD are substantial. This study allows us to obtain insight about the predictability of evaporation and, hence, may help to improve the early-warning systems of climate extremes.