Arctic river temperature dynamics in a changing climate

Climate change in the Arctic is expected to have a major impact on stream ecosys-tems, affecting hydrological and thermal regimes. Although temperature is importantto a range of in-stream processes, previous Arctic stream temperature research is lim-ited—focused on glacierised headwaters in summer—w...

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Published in:River Research and Applications
Main Authors: Docherty, Catherine L., Dugdale, Stephen J., Milner, Alexander M., Abermann, Jakob, Lund, Magnus, Hannah, David M.
Format: Article in Journal/Newspaper
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://doi.org/10.1002/rra.3537
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spelling ftzenodo:oai:zenodo.org:7071217 2024-09-15T18:02:13+00:00 Arctic river temperature dynamics in a changing climate Docherty, Catherine L. Dugdale, Stephen J. Milner, Alexander M. Abermann, Jakob Lund, Magnus Hannah, David M. 2019-10-11 https://doi.org/10.1002/rra.3537 unknown Zenodo https://doi.org/10.1002/rra.3537 oai:zenodo.org:7071217 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode River Research and Applications, (2019-10-11) info:eu-repo/semantics/article 2019 ftzenodo https://doi.org/10.1002/rra.3537 2024-07-26T00:51:24Z Climate change in the Arctic is expected to have a major impact on stream ecosys-tems, affecting hydrological and thermal regimes. Although temperature is importantto a range of in-stream processes, previous Arctic stream temperature research is lim-ited—focused on glacierised headwaters in summer—with limited attention to snow-melt streams and winter. This is the first high-resolution study on streamtemperature in north-east Greenland (Zackenberg). Data were collected from fivestreams from September 2013 to September 2015 (24 months). During the winter,streams were largely frozen solid and water temperature variability low. Spring ice-off date occurred simultaneously across all streams, but 11 days earlier in 2014 com-pared with 2015 due to thicker snow insulation. During summer, water temperaturewas highly variable and exhibited a strong relationship with meteorological variables,particularly incoming shortwave radiation and air temperature. Mean summer watertemperature in these snowmelt streams was high compared with streams studied pre-viously in Svalbard, yet was lower in Swedish Lapland, as was expected given latitude.With global warning, Arctic stream thermal variability may be less in summer andincreased during the winter due to higher summer air temperature and elevated win-ter precipitation, and the spring and autumn ice-on and ice-off dates may extend theflowing water season—in turn affecting stream productivity and diversity. Article in Journal/Newspaper Climate change East Greenland Greenland Svalbard Zackenberg Lapland Zenodo River Research and Applications
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description Climate change in the Arctic is expected to have a major impact on stream ecosys-tems, affecting hydrological and thermal regimes. Although temperature is importantto a range of in-stream processes, previous Arctic stream temperature research is lim-ited—focused on glacierised headwaters in summer—with limited attention to snow-melt streams and winter. This is the first high-resolution study on streamtemperature in north-east Greenland (Zackenberg). Data were collected from fivestreams from September 2013 to September 2015 (24 months). During the winter,streams were largely frozen solid and water temperature variability low. Spring ice-off date occurred simultaneously across all streams, but 11 days earlier in 2014 com-pared with 2015 due to thicker snow insulation. During summer, water temperaturewas highly variable and exhibited a strong relationship with meteorological variables,particularly incoming shortwave radiation and air temperature. Mean summer watertemperature in these snowmelt streams was high compared with streams studied pre-viously in Svalbard, yet was lower in Swedish Lapland, as was expected given latitude.With global warning, Arctic stream thermal variability may be less in summer andincreased during the winter due to higher summer air temperature and elevated win-ter precipitation, and the spring and autumn ice-on and ice-off dates may extend theflowing water season—in turn affecting stream productivity and diversity.
format Article in Journal/Newspaper
author Docherty, Catherine L.
Dugdale, Stephen J.
Milner, Alexander M.
Abermann, Jakob
Lund, Magnus
Hannah, David M.
spellingShingle Docherty, Catherine L.
Dugdale, Stephen J.
Milner, Alexander M.
Abermann, Jakob
Lund, Magnus
Hannah, David M.
Arctic river temperature dynamics in a changing climate
author_facet Docherty, Catherine L.
Dugdale, Stephen J.
Milner, Alexander M.
Abermann, Jakob
Lund, Magnus
Hannah, David M.
author_sort Docherty, Catherine L.
title Arctic river temperature dynamics in a changing climate
title_short Arctic river temperature dynamics in a changing climate
title_full Arctic river temperature dynamics in a changing climate
title_fullStr Arctic river temperature dynamics in a changing climate
title_full_unstemmed Arctic river temperature dynamics in a changing climate
title_sort arctic river temperature dynamics in a changing climate
publisher Zenodo
publishDate 2019
url https://doi.org/10.1002/rra.3537
genre Climate change
East Greenland
Greenland
Svalbard
Zackenberg
Lapland
genre_facet Climate change
East Greenland
Greenland
Svalbard
Zackenberg
Lapland
op_source River Research and Applications, (2019-10-11)
op_relation https://doi.org/10.1002/rra.3537
oai:zenodo.org:7071217
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1002/rra.3537
container_title River Research and Applications
_version_ 1810439651799859200