Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden
Glacier mass balance is heavily influenced by climate, with responses of individual glaciers to various climate parameters varying greatly. In northern Sweden, Rabots Glaciär’s mass balance has decreased since it started being monitored in 1982. To relate Rabots Glaciär’s mass balance to changes in...
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doaj-cc59394c56d34ff0b7a766c70274afa22021-08-26T13:38:27ZengMDPI AGClimate2225-11542021-08-01912612610.3390/cli9080126Mass Balance Sensitivity and Future Projections of Rabots Glaciär, SwedenMoon Taveirne0Laura Ekemar1Berta González Sánchez2Josefine Axelsson3Qiong Zhang4Department of Physical Geography, Stockholm University, SE-10691 Stockholm, SwedenDepartment of Physical Geography, Stockholm University, SE-10691 Stockholm, SwedenDepartment of Physical Geography, Stockholm University, SE-10691 Stockholm, SwedenDepartment of Physical Geography, Stockholm University, SE-10691 Stockholm, SwedenDepartment of Physical Geography, Stockholm University, SE-10691 Stockholm, SwedenGlacier mass balance is heavily influenced by climate, with responses of individual glaciers to various climate parameters varying greatly. In northern Sweden, Rabots Glaciär’s mass balance has decreased since it started being monitored in 1982. To relate Rabots Glaciär’s mass balance to changes in climate, the sensitivity to a range of parameters is computed. Through linear regression of mass balance with temperature, precipitation, humidity, wind speed and incoming radiation the climate sensitivity is established and projections for future summer mass balance are made. Summer mass balance is primarily sensitive to temperature at −0.31 m w.e. per °C change, while winter mass balance is mainly sensitive to precipitation at 0.94 m w.e. per % change. An estimate using summer temperature sensitivity projects a dramatic decrease in summer mass balance to −3.89 m w.e. for the 2091–2100 period under climate scenario RCP8.5. With large increases in temperature anticipated for the next century, more complex modelling studies of the relationship between climate and glacier mass balance is key to understanding the future development of Rabots Glaciär.https://www.mdpi.com/2225-1154/9/8/126glacier mass balanceclimate sensitivitymass balance predictionRabots Glaciär |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Moon Taveirne Laura Ekemar Berta González Sánchez Josefine Axelsson Qiong Zhang |
spellingShingle |
Moon Taveirne Laura Ekemar Berta González Sánchez Josefine Axelsson Qiong Zhang Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden Climate glacier mass balance climate sensitivity mass balance prediction Rabots Glaciär |
author_facet |
Moon Taveirne Laura Ekemar Berta González Sánchez Josefine Axelsson Qiong Zhang |
author_sort |
Moon Taveirne |
title |
Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden |
title_short |
Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden |
title_full |
Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden |
title_fullStr |
Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden |
title_full_unstemmed |
Mass Balance Sensitivity and Future Projections of Rabots Glaciär, Sweden |
title_sort |
mass balance sensitivity and future projections of rabots glaciär, sweden |
publisher |
MDPI AG |
series |
Climate |
issn |
2225-1154 |
publishDate |
2021-08-01 |
description |
Glacier mass balance is heavily influenced by climate, with responses of individual glaciers to various climate parameters varying greatly. In northern Sweden, Rabots Glaciär’s mass balance has decreased since it started being monitored in 1982. To relate Rabots Glaciär’s mass balance to changes in climate, the sensitivity to a range of parameters is computed. Through linear regression of mass balance with temperature, precipitation, humidity, wind speed and incoming radiation the climate sensitivity is established and projections for future summer mass balance are made. Summer mass balance is primarily sensitive to temperature at −0.31 m w.e. per °C change, while winter mass balance is mainly sensitive to precipitation at 0.94 m w.e. per % change. An estimate using summer temperature sensitivity projects a dramatic decrease in summer mass balance to −3.89 m w.e. for the 2091–2100 period under climate scenario RCP8.5. With large increases in temperature anticipated for the next century, more complex modelling studies of the relationship between climate and glacier mass balance is key to understanding the future development of Rabots Glaciär. |
topic |
glacier mass balance climate sensitivity mass balance prediction Rabots Glaciär |
url |
https://www.mdpi.com/2225-1154/9/8/126 |
work_keys_str_mv |
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1721194183066124288 |