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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 20, issue 3
Hydrol. Earth Syst. Sci., 20, 1211–1223, 2016
https://doi.org/10.5194/hess-20-1211-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 20, 1211–1223, 2016
https://doi.org/10.5194/hess-20-1211-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Mar 2016

Research article | 21 Mar 2016

Creating long-term gridded fields of reference evapotranspiration in Alpine terrain based on a recalibrated Hargreaves method

Klaus Haslinger and Annett Bartsch

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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 (27 Aug 2015) by Jan Seibert
AR by Klaus Haslinger on behalf of the Authors (08 Oct 2015)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Oct 2015) by Jan Seibert
RR by Anonymous Referee #1 (28 Oct 2015)
RR by Anonymous Referee #3 (21 Dec 2015)
RR by Anonymous Referee #4 (03 Feb 2016)
ED: Reconsider after major revisions (08 Feb 2016) by Jan Seibert
AR by Klaus Haslinger on behalf of the Authors (22 Feb 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (26 Feb 2016) by Jan Seibert
RR by Anonymous Referee #4 (29 Feb 2016)
ED: Publish subject to minor revisions (Editor review) (01 Mar 2016) by Jan Seibert
AR by Klaus Haslinger on behalf of the Authors (01 Mar 2016)  Author's response    Manuscript
ED: Publish subject to technical corrections (02 Mar 2016) by Jan Seibert
Publications Copernicus
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Short summary
Gridded fields of daily max. and min. temperatures for the Austrian domain are used to calculate ET0 based on a re-calibrated Hargreaves method. Newly derived, station-based calibration parameters, with Penman–Monteith ET0 as a reference, show a distinct altitude and seasonal dependence. Theses features are used to interpolate the new calibration values in space and time onto the temperature grids. The ET0 is then calculated based on the entire gridded temperature data starting back in 1961.
Gridded fields of daily max. and min. temperatures for the Austrian domain are used to calculate...
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