Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations

Several simulations of the surface climate and energy balance of Vatnajökull ice cap, Iceland, are used to estimate the glacier runoff for the period 1980–2015 and the sensitivity of runoff to the spring conditions (e.g., snow thickness). The simulations are calculated using the snow pack scheme fro...

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Published in:Atmosphere
Main Authors: Louise Steffensen Schmidt, Peter L. Langen, Guðfinna Aðalgeirsdóttir, Finnur Pálsson, Sverrir Guðmundsson, Andri Gunnarsson
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/atmos9110450
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spelling ftmdpi:oai:mdpi.com:/2073-4433/9/11/450/ 2023-08-20T04:06:42+02:00 Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations Louise Steffensen Schmidt Peter L. Langen Guðfinna Aðalgeirsdóttir Finnur Pálsson Sverrir Guðmundsson Andri Gunnarsson agris 2018-11-15 application/pdf https://doi.org/10.3390/atmos9110450 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos9110450 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 9; Issue 11; Pages: 450 regional climate models glaciers snowfall snow-albedo feedback runoff sensitivity Text 2018 ftmdpi https://doi.org/10.3390/atmos9110450 2023-07-31T21:50:38Z Several simulations of the surface climate and energy balance of Vatnajökull ice cap, Iceland, are used to estimate the glacier runoff for the period 1980–2015 and the sensitivity of runoff to the spring conditions (e.g., snow thickness). The simulations are calculated using the snow pack scheme from the regional climate model HIRHAM5, forced with incoming mass and energy fluxes from the numerical weather prediction model HARMONIE-AROME. The modeled runoff is compared to available observations from two outlet glaciers to assess the quality of the simulations. To test the sensitivity of the runoff to spring conditions, simulations are repeated for the spring conditions of each of the years 1980–2015, followed by the weather of all summers in the same period. We find that for the whole ice cap, the variability in runoff as a function of varying spring conditions was on average 31% of the variability due to changing summer weather. However, some outlet glaciers are very sensitive to the amount of snow in the spring, as e.g., the variation in runoff from Brúarjökull due to changing spring conditions was on average 50% of the variability due to varying summer weather. Text glacier Ice cap Iceland Vatnajökull MDPI Open Access Publishing Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420) Brúarjökull ENVELOPE(-16.157,-16.157,64.682,64.682) Atmosphere 9 11 450
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic regional climate models
glaciers
snowfall
snow-albedo feedback
runoff sensitivity
spellingShingle regional climate models
glaciers
snowfall
snow-albedo feedback
runoff sensitivity
Louise Steffensen Schmidt
Peter L. Langen
Guðfinna Aðalgeirsdóttir
Finnur Pálsson
Sverrir Guðmundsson
Andri Gunnarsson
Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
topic_facet regional climate models
glaciers
snowfall
snow-albedo feedback
runoff sensitivity
description Several simulations of the surface climate and energy balance of Vatnajökull ice cap, Iceland, are used to estimate the glacier runoff for the period 1980–2015 and the sensitivity of runoff to the spring conditions (e.g., snow thickness). The simulations are calculated using the snow pack scheme from the regional climate model HIRHAM5, forced with incoming mass and energy fluxes from the numerical weather prediction model HARMONIE-AROME. The modeled runoff is compared to available observations from two outlet glaciers to assess the quality of the simulations. To test the sensitivity of the runoff to spring conditions, simulations are repeated for the spring conditions of each of the years 1980–2015, followed by the weather of all summers in the same period. We find that for the whole ice cap, the variability in runoff as a function of varying spring conditions was on average 31% of the variability due to changing summer weather. However, some outlet glaciers are very sensitive to the amount of snow in the spring, as e.g., the variation in runoff from Brúarjökull due to changing spring conditions was on average 50% of the variability due to varying summer weather.
format Text
author Louise Steffensen Schmidt
Peter L. Langen
Guðfinna Aðalgeirsdóttir
Finnur Pálsson
Sverrir Guðmundsson
Andri Gunnarsson
author_facet Louise Steffensen Schmidt
Peter L. Langen
Guðfinna Aðalgeirsdóttir
Finnur Pálsson
Sverrir Guðmundsson
Andri Gunnarsson
author_sort Louise Steffensen Schmidt
title Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
title_short Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
title_full Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
title_fullStr Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
title_full_unstemmed Sensitivity of Glacier Runoff to Winter Snow Thickness Investigated for Vatnajökull Ice Cap, Iceland, Using Numerical Models and Observations
title_sort sensitivity of glacier runoff to winter snow thickness investigated for vatnajökull ice cap, iceland, using numerical models and observations
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/atmos9110450
op_coverage agris
long_lat ENVELOPE(-16.823,-16.823,64.420,64.420)
ENVELOPE(-16.157,-16.157,64.682,64.682)
geographic Vatnajökull
Brúarjökull
geographic_facet Vatnajökull
Brúarjökull
genre glacier
Ice cap
Iceland
Vatnajökull
genre_facet glacier
Ice cap
Iceland
Vatnajökull
op_source Atmosphere; Volume 9; Issue 11; Pages: 450
op_relation Meteorology
https://dx.doi.org/10.3390/atmos9110450
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos9110450
container_title Atmosphere
container_volume 9
container_issue 11
container_start_page 450
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