Articles | Volume 22, issue 1
https://doi.org/10.5194/hess-22-567-2018
https://doi.org/10.5194/hess-22-567-2018
Research article
 | 
23 Jan 2018
Research article |  | 23 Jan 2018

Dominant effect of increasing forest biomass on evapotranspiration: interpretations of movement in Budyko space

Fernando Jaramillo, Neil Cory, Berit Arheimer, Hjalmar Laudon, Ype van der Velde, Thomas B. Hasper, Claudia Teutschbein, and Johan Uddling

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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: Publish subject to revisions (further review by Editor and Referees) (30 Aug 2017) by Sally Thompson
AR by Fernando Jaramillo on behalf of the Authors (09 Oct 2017)  Manuscript 
ED: Referee Nomination & Report Request started (17 Oct 2017) by Sally Thompson
RR by Anonymous Referee #1 (15 Nov 2017)
RR by Anonymous Referee #3 (17 Nov 2017)
ED: Publish subject to minor revisions (review by editor) (17 Nov 2017) by Sally Thompson
AR by Fernando Jaramillo on behalf of the Authors (21 Nov 2017)  Author's response   Manuscript 
ED: Publish as is (05 Dec 2017) by Sally Thompson
AR by Fernando Jaramillo on behalf of the Authors (07 Dec 2017)
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Short summary
Which is the dominant effect on evapotranspiration in northern forests, an increase by recent forests expansion or a decrease by the water use response due to increasing CO2 concentrations? We determined the dominant effect during the period 1961–2012 in 65 Swedish basins. We used the Budyko framework to study the hydroclimatic movements in Budyko space. Our findings suggest that forest expansion is the dominant driver of long-term and large-scale evapotranspiration changes.