Modelling annual mass balances of eight Scandinavian glaciers using statistical models
Mass balances of Scandinavian glaciers are mainly influenced by winter precipitation and summer temperature. We used simple statistical models to assess the relative importance of summer temperature and winter precipitation for annual balances of eight glaciers in Scandinavia. Winter precipitation w...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:842764637ec14ef2abb5d1b19d580a28 2023-05-15T17:34:04+02:00 Modelling annual mass balances of eight Scandinavian glaciers using statistical models M. Trachsel A. Nesje 2015-07-01 https://doi.org/10.5194/tc-9-1401-2015 http://www.the-cryosphere.net/9/1401/2015/tc-9-1401-2015.pdf https://doaj.org/article/842764637ec14ef2abb5d1b19d580a28 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-9-1401-2015 http://www.the-cryosphere.net/9/1401/2015/tc-9-1401-2015.pdf https://doaj.org/article/842764637ec14ef2abb5d1b19d580a28 undefined The Cryosphere, Vol 9, Iss 4, Pp 1401-1414 (2015) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/tc-9-1401-2015 2023-01-22T19:23:35Z Mass balances of Scandinavian glaciers are mainly influenced by winter precipitation and summer temperature. We used simple statistical models to assess the relative importance of summer temperature and winter precipitation for annual balances of eight glaciers in Scandinavia. Winter precipitation was more important for maritime glaciers, whereas summer temperature was more important for annual balances of continental glaciers. Most importantly relative importances of summer temperature and winter precipitation were not stable in time. For instance, winter precipitation was more important than summer temperature for all glaciers in the 25-year period 1972–1996, whereas the relative importance of summer temperature was increasing towards the present. Between 1963 and 1996 the Atlantic Multidecadal Oscillation (AMO) index was consistently negative and the North Atlantic Oscillation (NAO) Index was consistently positive between 1987 and 1995, both being favourable for glacier growth. Winter precipitation was more important than summer temperature for annual balances when only considering subsets of years with high NAO-index and negative AMO-index, respectively, whereas the importance of summer temperature was increased analysing subsets of years with low NAO-index and positive AMO-index, respectively. Hence, the relative importance of precipitation and temperature for mass balances was probably influenced by the state of the AMO and the NAO, as these two indexes are associated with changes in summer temperature (AMO) and winter precipitation (NAO). Article in Journal/Newspaper North Atlantic North Atlantic oscillation The Cryosphere Unknown The Cryosphere 9 4 1401 1414 |
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envir geo M. Trachsel A. Nesje Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
topic_facet |
envir geo |
description |
Mass balances of Scandinavian glaciers are mainly influenced by winter precipitation and summer temperature. We used simple statistical models to assess the relative importance of summer temperature and winter precipitation for annual balances of eight glaciers in Scandinavia. Winter precipitation was more important for maritime glaciers, whereas summer temperature was more important for annual balances of continental glaciers. Most importantly relative importances of summer temperature and winter precipitation were not stable in time. For instance, winter precipitation was more important than summer temperature for all glaciers in the 25-year period 1972–1996, whereas the relative importance of summer temperature was increasing towards the present. Between 1963 and 1996 the Atlantic Multidecadal Oscillation (AMO) index was consistently negative and the North Atlantic Oscillation (NAO) Index was consistently positive between 1987 and 1995, both being favourable for glacier growth. Winter precipitation was more important than summer temperature for annual balances when only considering subsets of years with high NAO-index and negative AMO-index, respectively, whereas the importance of summer temperature was increased analysing subsets of years with low NAO-index and positive AMO-index, respectively. Hence, the relative importance of precipitation and temperature for mass balances was probably influenced by the state of the AMO and the NAO, as these two indexes are associated with changes in summer temperature (AMO) and winter precipitation (NAO). |
format |
Article in Journal/Newspaper |
author |
M. Trachsel A. Nesje |
author_facet |
M. Trachsel A. Nesje |
author_sort |
M. Trachsel |
title |
Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
title_short |
Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
title_full |
Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
title_fullStr |
Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
title_full_unstemmed |
Modelling annual mass balances of eight Scandinavian glaciers using statistical models |
title_sort |
modelling annual mass balances of eight scandinavian glaciers using statistical models |
publisher |
Copernicus Publications |
publishDate |
2015 |
url |
https://doi.org/10.5194/tc-9-1401-2015 http://www.the-cryosphere.net/9/1401/2015/tc-9-1401-2015.pdf https://doaj.org/article/842764637ec14ef2abb5d1b19d580a28 |
genre |
North Atlantic North Atlantic oscillation The Cryosphere |
genre_facet |
North Atlantic North Atlantic oscillation The Cryosphere |
op_source |
The Cryosphere, Vol 9, Iss 4, Pp 1401-1414 (2015) |
op_relation |
1994-0416 1994-0424 doi:10.5194/tc-9-1401-2015 http://www.the-cryosphere.net/9/1401/2015/tc-9-1401-2015.pdf https://doaj.org/article/842764637ec14ef2abb5d1b19d580a28 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-9-1401-2015 |
container_title |
The Cryosphere |
container_volume |
9 |
container_issue |
4 |
container_start_page |
1401 |
op_container_end_page |
1414 |
_version_ |
1766132763202682880 |