Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic

We present a Seasonal Sensitivity Characteristic (SSC) of Vatnajökull (Iceland), which consists of the sensitivity of the mean specific mass balance to monthly perturbations in temperature and precipitation. The climate in Iceland is predominantly maritime (high precipitation) although often the pol...

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Main Authors: Ruyter de Wildt, Martijn Sybren de, Klok, E.J., Oerlemans, J.
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/22696
id ftunivutrecht:oai:dspace.library.uu.nl:1874/22696
record_format openpolar
spelling ftunivutrecht:oai:dspace.library.uu.nl:1874/22696 2023-07-23T04:19:23+02:00 Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic Ruyter de Wildt, Martijn Sybren de Klok, E.J. Oerlemans, J. 2003-03 image/pdf https://dspace.library.uu.nl/handle/1874/22696 en eng 0435-3676 https://dspace.library.uu.nl/handle/1874/22696 info:eu-repo/semantics/ClosedAccess Natuur- en Sterrenkunde Article 2003 ftunivutrecht 2023-07-01T23:21:32Z We present a Seasonal Sensitivity Characteristic (SSC) of Vatnajökull (Iceland), which consists of the sensitivity of the mean specific mass balance to monthly perturbations in temperature and precipitation. The climate in Iceland is predominantly maritime (high precipitation) although often the polar air mass influences the area. This results in temperature sensitivities that are high in summer and nearly zero during the winter months. In contrast, precipitation sensitivities are high in winter and low in summer. We use the SSC of Vatnajökull as a reduced mass balance model, with which we reconstruct the mass balance of Vatnajökull since 1825. The reduced model shows that changes in temperature and precipitation like the ones observed both have a significant impact upon the mass balance. The reconstructed mass balance records for two Icelandic glaciers correlate very well with mass balance records that are extracted from length records with a linear inverse model. This places confidence in both the reduced (forward) mass balance model and in the inverse model, although the forward method produces larger mass balance variations than the inverse method. For the south of Vatnajökull we find that after 1900, the length record is well explained by temperature variations alone, while another Icelandic glacier (Sólheimajökull) was also influenced by precipitation variations. Article in Journal/Newspaper glacier Iceland Vatnajökull Utrecht University Repository Sólheimajökull ENVELOPE(-19.303,-19.303,63.557,63.557) Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420)
institution Open Polar
collection Utrecht University Repository
op_collection_id ftunivutrecht
language English
topic Natuur- en Sterrenkunde
spellingShingle Natuur- en Sterrenkunde
Ruyter de Wildt, Martijn Sybren de
Klok, E.J.
Oerlemans, J.
Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
topic_facet Natuur- en Sterrenkunde
description We present a Seasonal Sensitivity Characteristic (SSC) of Vatnajökull (Iceland), which consists of the sensitivity of the mean specific mass balance to monthly perturbations in temperature and precipitation. The climate in Iceland is predominantly maritime (high precipitation) although often the polar air mass influences the area. This results in temperature sensitivities that are high in summer and nearly zero during the winter months. In contrast, precipitation sensitivities are high in winter and low in summer. We use the SSC of Vatnajökull as a reduced mass balance model, with which we reconstruct the mass balance of Vatnajökull since 1825. The reduced model shows that changes in temperature and precipitation like the ones observed both have a significant impact upon the mass balance. The reconstructed mass balance records for two Icelandic glaciers correlate very well with mass balance records that are extracted from length records with a linear inverse model. This places confidence in both the reduced (forward) mass balance model and in the inverse model, although the forward method produces larger mass balance variations than the inverse method. For the south of Vatnajökull we find that after 1900, the length record is well explained by temperature variations alone, while another Icelandic glacier (Sólheimajökull) was also influenced by precipitation variations.
format Article in Journal/Newspaper
author Ruyter de Wildt, Martijn Sybren de
Klok, E.J.
Oerlemans, J.
author_facet Ruyter de Wildt, Martijn Sybren de
Klok, E.J.
Oerlemans, J.
author_sort Ruyter de Wildt, Martijn Sybren de
title Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
title_short Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
title_full Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
title_fullStr Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
title_full_unstemmed Reconstruction of the mean specific balance of Vatnajokull (Iceland) with a seasonal sensitivity characteristic
title_sort reconstruction of the mean specific balance of vatnajokull (iceland) with a seasonal sensitivity characteristic
publishDate 2003
url https://dspace.library.uu.nl/handle/1874/22696
long_lat ENVELOPE(-19.303,-19.303,63.557,63.557)
ENVELOPE(-16.823,-16.823,64.420,64.420)
geographic Sólheimajökull
Vatnajökull
geographic_facet Sólheimajökull
Vatnajökull
genre glacier
Iceland
Vatnajökull
genre_facet glacier
Iceland
Vatnajökull
op_relation 0435-3676
https://dspace.library.uu.nl/handle/1874/22696
op_rights info:eu-repo/semantics/ClosedAccess
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