Articles | Volume 25, issue 9
https://doi.org/10.5194/hess-25-5175-2021
https://doi.org/10.5194/hess-25-5175-2021
Research article
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24 Sep 2021
Research article | Highlight paper |  | 24 Sep 2021

Relative humidity gradients as a key constraint on terrestrial water and energy fluxes

Yeonuk Kim, Monica Garcia, Laura Morillas, Ulrich Weber, T. Andrew Black, and Mark S. Johnson

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Status: closed
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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) (25 Apr 2021) by Anke Hildebrandt
AR by Yeonuk Kim on behalf of the Authors (05 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Jun 2021) by Anke Hildebrandt
RR by Anonymous Referee #2 (16 Jul 2021)
RR by Anonymous Referee #1 (27 Jul 2021)
ED: Publish subject to revisions (further review by editor and referees) (11 Aug 2021) by Anke Hildebrandt
AR by Yeonuk Kim on behalf of the Authors (23 Aug 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (24 Aug 2021) by Anke Hildebrandt
AR by Yeonuk Kim on behalf of the Authors (30 Aug 2021)  Manuscript 
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Short summary
Here, we present a novel physically based evaporation model to demonstrate that vertical relative humidity (RH) gradients from the land surface to the atmosphere tend to evolve towards zero due to land–atmosphere equilibration processes. Collapsing RH gradients on daily to yearly timescales indicate an emergent land–atmosphere equilibrium, making it possible to determine evapotranspiration using only meteorological information, independent of land surface conditions and vegetation controls.