Invited Perspective: What Lies Beneath a Changing Arctic?

As permafrost thaws in the Arctic, new subsurface pathways open for the movement of groundwater, energy, and solutes. We identify different ways that these subsurface changes are driving observed surface phenomena, including the potential for increased contaminant transport, modification to water re...

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Main Authors: McKenzie, Jeffrey M., Kurylyk, Barret L., Walvoord, Michelle A., Bense, Victor F., Fortier, Daniel, Spence, Chris, Grenier, Christophe
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-2020-132
https://tc.copernicus.org/preprints/tc-2020-132/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd85545 2023-05-15T14:50:46+02:00 Invited Perspective: What Lies Beneath a Changing Arctic? McKenzie, Jeffrey M. Kurylyk, Barret L. Walvoord, Michelle A. Bense, Victor F. Fortier, Daniel Spence, Chris Grenier, Christophe 2020-06-17 application/pdf https://doi.org/10.5194/tc-2020-132 https://tc.copernicus.org/preprints/tc-2020-132/ eng eng doi:10.5194/tc-2020-132 https://tc.copernicus.org/preprints/tc-2020-132/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-2020-132 2020-07-20T16:22:04Z As permafrost thaws in the Arctic, new subsurface pathways open for the movement of groundwater, energy, and solutes. We identify different ways that these subsurface changes are driving observed surface phenomena, including the potential for increased contaminant transport, modification to water resources, and enhanced rates of infrastructure (e.g. buildings and roads) damage. Further, as permafrost thaws it allows groundwater to transport carbon, nutrients, and other dissolved constituents from terrestrial to aquatic environments via progressively deeper subsurface flow paths. Cryohydrogeology, the study of groundwater in cold regions, must be included in Northern research initiatives to account for this hidden catalyst of environmental and societal change. Text Arctic permafrost Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description As permafrost thaws in the Arctic, new subsurface pathways open for the movement of groundwater, energy, and solutes. We identify different ways that these subsurface changes are driving observed surface phenomena, including the potential for increased contaminant transport, modification to water resources, and enhanced rates of infrastructure (e.g. buildings and roads) damage. Further, as permafrost thaws it allows groundwater to transport carbon, nutrients, and other dissolved constituents from terrestrial to aquatic environments via progressively deeper subsurface flow paths. Cryohydrogeology, the study of groundwater in cold regions, must be included in Northern research initiatives to account for this hidden catalyst of environmental and societal change.
format Text
author McKenzie, Jeffrey M.
Kurylyk, Barret L.
Walvoord, Michelle A.
Bense, Victor F.
Fortier, Daniel
Spence, Chris
Grenier, Christophe
spellingShingle McKenzie, Jeffrey M.
Kurylyk, Barret L.
Walvoord, Michelle A.
Bense, Victor F.
Fortier, Daniel
Spence, Chris
Grenier, Christophe
Invited Perspective: What Lies Beneath a Changing Arctic?
author_facet McKenzie, Jeffrey M.
Kurylyk, Barret L.
Walvoord, Michelle A.
Bense, Victor F.
Fortier, Daniel
Spence, Chris
Grenier, Christophe
author_sort McKenzie, Jeffrey M.
title Invited Perspective: What Lies Beneath a Changing Arctic?
title_short Invited Perspective: What Lies Beneath a Changing Arctic?
title_full Invited Perspective: What Lies Beneath a Changing Arctic?
title_fullStr Invited Perspective: What Lies Beneath a Changing Arctic?
title_full_unstemmed Invited Perspective: What Lies Beneath a Changing Arctic?
title_sort invited perspective: what lies beneath a changing arctic?
publishDate 2020
url https://doi.org/10.5194/tc-2020-132
https://tc.copernicus.org/preprints/tc-2020-132/
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2020-132
https://tc.copernicus.org/preprints/tc-2020-132/
op_doi https://doi.org/10.5194/tc-2020-132
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