Articles | Volume 20, issue 3
https://doi.org/10.5194/hess-20-1211-2016
https://doi.org/10.5194/hess-20-1211-2016
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

Viewed

Total article views: 4,082 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,063 1,704 315 4,082 75 86
  • HTML: 2,063
  • PDF: 1,704
  • XML: 315
  • Total: 4,082
  • BibTeX: 75
  • EndNote: 86
Views and downloads (calculated since 28 May 2015)
Cumulative views and downloads (calculated since 28 May 2015)

Cited

Saved (preprint)

Latest update: 20 Apr 2024
Download
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.