Changes in hydrogeologic regimes in permafrost regions due to climatic change

Abstract The general and specific effects of predicted climate change on groundwater systems in permafrost regions are summarized. Besides a general decrease in the thickness and areal distribution of permafrost, a large unfrozen near‐surface aquifer with perennial groundwater flow might develop. Re...

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Published in:Permafrost and Periglacial Processes
Main Authors: Michel, Frederick A., Van Everdingen, Robert O.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1994
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.3430050308
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050308
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050308
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spelling crwiley:10.1002/ppp.3430050308 2024-06-23T07:56:02+00:00 Changes in hydrogeologic regimes in permafrost regions due to climatic change Michel, Frederick A. Van Everdingen, Robert O. 1994 http://dx.doi.org/10.1002/ppp.3430050308 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050308 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050308 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 5, issue 3, page 191-195 ISSN 1045-6740 1099-1530 journal-article 1994 crwiley https://doi.org/10.1002/ppp.3430050308 2024-06-11T04:43:45Z Abstract The general and specific effects of predicted climate change on groundwater systems in permafrost regions are summarized. Besides a general decrease in the thickness and areal distribution of permafrost, a large unfrozen near‐surface aquifer with perennial groundwater flow might develop. Recharge and discharge would become more active and increased groundwater discharge would affect the baseflow of many rivers and the chemistry of their waters. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 5 3 191 195
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The general and specific effects of predicted climate change on groundwater systems in permafrost regions are summarized. Besides a general decrease in the thickness and areal distribution of permafrost, a large unfrozen near‐surface aquifer with perennial groundwater flow might develop. Recharge and discharge would become more active and increased groundwater discharge would affect the baseflow of many rivers and the chemistry of their waters.
format Article in Journal/Newspaper
author Michel, Frederick A.
Van Everdingen, Robert O.
spellingShingle Michel, Frederick A.
Van Everdingen, Robert O.
Changes in hydrogeologic regimes in permafrost regions due to climatic change
author_facet Michel, Frederick A.
Van Everdingen, Robert O.
author_sort Michel, Frederick A.
title Changes in hydrogeologic regimes in permafrost regions due to climatic change
title_short Changes in hydrogeologic regimes in permafrost regions due to climatic change
title_full Changes in hydrogeologic regimes in permafrost regions due to climatic change
title_fullStr Changes in hydrogeologic regimes in permafrost regions due to climatic change
title_full_unstemmed Changes in hydrogeologic regimes in permafrost regions due to climatic change
title_sort changes in hydrogeologic regimes in permafrost regions due to climatic change
publisher Wiley
publishDate 1994
url http://dx.doi.org/10.1002/ppp.3430050308
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430050308
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430050308
genre permafrost
Permafrost and Periglacial Processes
genre_facet permafrost
Permafrost and Periglacial Processes
op_source Permafrost and Periglacial Processes
volume 5, issue 3, page 191-195
ISSN 1045-6740 1099-1530
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/ppp.3430050308
container_title Permafrost and Periglacial Processes
container_volume 5
container_issue 3
container_start_page 191
op_container_end_page 195
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