Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?

Abstract Global change is predicted to increase temperature substantially in the North as well as altering run‐off regimes with less synchronicity as the importance of snow melt declines. River biota and ecosystem processes will be influenced across all levels of organization, both in concert and in...

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Published in:Hydrological Processes
Main Authors: Friberg, Nikolai, Bergfur, Jenny, Rasmussen, Jes, Sandin, Leonard
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2013
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.9598
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spelling crwiley:10.1002/hyp.9598 2024-06-02T08:07:34+00:00 Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes? Friberg, Nikolai Bergfur, Jenny Rasmussen, Jes Sandin, Leonard 2013 http://dx.doi.org/10.1002/hyp.9598 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9598 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9598 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 27, issue 5, page 734-740 ISSN 0885-6087 1099-1085 journal-article 2013 crwiley https://doi.org/10.1002/hyp.9598 2024-05-03T11:16:46Z Abstract Global change is predicted to increase temperature substantially in the North as well as altering run‐off regimes with less synchronicity as the importance of snow melt declines. River biota and ecosystem processes will be influenced across all levels of organization, both in concert and individually. It is of vital importance that the impacts, and their likely magnitude, can be identified in order to deploy suitable adaptation strategies at the catchment scale. In this paper, we re‐analyse four data sets from studies conducted in Greenland (66–69 o N), Iceland (64 o N), Sweden (60 o N) and Denmark (55–57 o N) to try and tease out the likely impacts of water temperature and hydrology in shaping the stream communities and ecosystem processes in high‐latitude catchments. Water temperature was the environmental variable that best explained macroinvertebrate community composition across latitudes. In contrast, no significant relationship between macroinvertebrate community composition and measures of hydraulic stability (or nutrients) was found. We found a strong linear relationship between decay rate of leaf litter and water temperature ( r 2 = 0.68; p < 0.0001) independent of latitudes. Our study suggests that temperature could be the primary driver of ecosystem change in future with northern catchments likely to be especially vulnerable. Copyright © 2012 John Wiley & Sons, Ltd. Article in Journal/Newspaper Greenland Iceland Wiley Online Library Greenland Hydrological Processes 27 5 734 740
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Global change is predicted to increase temperature substantially in the North as well as altering run‐off regimes with less synchronicity as the importance of snow melt declines. River biota and ecosystem processes will be influenced across all levels of organization, both in concert and individually. It is of vital importance that the impacts, and their likely magnitude, can be identified in order to deploy suitable adaptation strategies at the catchment scale. In this paper, we re‐analyse four data sets from studies conducted in Greenland (66–69 o N), Iceland (64 o N), Sweden (60 o N) and Denmark (55–57 o N) to try and tease out the likely impacts of water temperature and hydrology in shaping the stream communities and ecosystem processes in high‐latitude catchments. Water temperature was the environmental variable that best explained macroinvertebrate community composition across latitudes. In contrast, no significant relationship between macroinvertebrate community composition and measures of hydraulic stability (or nutrients) was found. We found a strong linear relationship between decay rate of leaf litter and water temperature ( r 2 = 0.68; p < 0.0001) independent of latitudes. Our study suggests that temperature could be the primary driver of ecosystem change in future with northern catchments likely to be especially vulnerable. Copyright © 2012 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Friberg, Nikolai
Bergfur, Jenny
Rasmussen, Jes
Sandin, Leonard
spellingShingle Friberg, Nikolai
Bergfur, Jenny
Rasmussen, Jes
Sandin, Leonard
Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
author_facet Friberg, Nikolai
Bergfur, Jenny
Rasmussen, Jes
Sandin, Leonard
author_sort Friberg, Nikolai
title Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
title_short Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
title_full Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
title_fullStr Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
title_full_unstemmed Changing Northern catchments: Is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
title_sort changing northern catchments: is altered hydrology, temperature or both going to shape future stream communities and ecosystem processes?
publisher Wiley
publishDate 2013
url http://dx.doi.org/10.1002/hyp.9598
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.9598
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.9598
geographic Greenland
geographic_facet Greenland
genre Greenland
Iceland
genre_facet Greenland
Iceland
op_source Hydrological Processes
volume 27, issue 5, page 734-740
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.9598
container_title Hydrological Processes
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