Multilevel spatiotemporal validation of snow/ice mass balance and runoff modeling in glacierized catchments

Hanzer, Florian; Helfricht, Kay; Marke, Thomas; Strasser, Ulrich

doi:https://doi.org/10.5194/tc-10-1859-2016

Articles | Volume 10, issue 4

https://doi.org/10.5194/tc-10-1859-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/tc-10-1859-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 10, issue 4

Research article

|

25 Aug 2016

Research article |

| 25 Aug 2016

Multilevel spatiotemporal validation of snow/ice mass balance and runoff modeling in glacierized catchments

Florian Hanzer, Kay Helfricht, Thomas Marke, and Ulrich Strasser

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Final revised paper (published on 25 Aug 2016)
Supplement to the final revised paper
Preprint (discussion started on 05 Apr 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review', Bettina Schaefli, 22 Apr 2016
- AC1: 'Reply to Bettina Schaefli', Florian Hanzer, 13 Jul 2016
RC2: 'Multi-level spatiotemporal validation of snow/ice mass balance and runoff modeling in glacierized catchments.', Anonymous Referee #2, 14 Jun 2016
- AC2: 'Reply to Anonymous Referee #2', Florian Hanzer, 13 Jul 2016

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Florian Hanzer on behalf of the Authors (13 Jul 2016) Author's response Manuscript

ED: Publish as is (07 Aug 2016) by Valentina Radic

AR by Florian Hanzer on behalf of the Authors (10 Aug 2016)

Short summary

The hydroclimatological model AMUNDSEN is set up to simulate snow and ice accumulation, ablation, and runoff for a study region in the Ötztal Alps (Austria) in the period 1997–2013. A new validation concept is introduced and demonstrated by evaluating the model performance using several independent data sets, e.g. snow depth measurements, satellite-derived snow maps, lidar data, glacier mass balances, and runoff measurements.