Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake

Although perennially ice‐covered Antarctic lakes have experienced variable ice thicknesses over the past several decades, future ice thickness trends and associated aquatic biological responses under projected global warming remain unknown. Heat stored in the water column in chemically stratified An...

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Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Obryk, Maciej K., Doran, Peter T., Priscu, John C.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2019
Subjects:
Online Access:https://scholarworks.montana.edu/xmlui/handle/1/15638
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spelling ftmontanastateu:oai:scholarworks.montana.edu:1/15638 2023-05-15T13:54:59+02:00 Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake Obryk, Maciej K. Doran, Peter T. Priscu, John C. 2019-02 application/pdf https://scholarworks.montana.edu/xmlui/handle/1/15638 unknown Obryk, M. K., P. T. Doran, and J. C. Priscu. “Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake.” Journal of Geophysical Research: Earth Surface 124, no. 2 (February 2019): 686–694. doi:10.1029/2018jf004756. 2169-9003 https://scholarworks.montana.edu/xmlui/handle/1/15638 This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s). http://rightsstatements.org/vocab/InC/1.0/ Article 2019 ftmontanastateu https://doi.org/10.1029/2018jf004756 2022-06-06T07:28:19Z Although perennially ice‐covered Antarctic lakes have experienced variable ice thicknesses over the past several decades, future ice thickness trends and associated aquatic biological responses under projected global warming remain unknown. Heat stored in the water column in chemically stratified Antarctic lakes that have middepth temperature maxima can significantly influence the ice thickness trends via upward heat flux to the ice/water interface. We modeled the ice thickness of the west lobe of Lake Bonney, Antarctica, based on possible future climate scenarios utilizing a 1D thermodynamic model that accounts for surface radiative fluxes as well as the heat flux associated with the temperature evolution of the water column. Model results predict that the ice cover of Lake Bonney will shift from perennial to seasonal within one to four decades, a change that will drastically influence ecosystem processes within the lake. Article in Journal/Newspaper Antarc* Antarctic Antarctica Montana State University (MSU): ScholarWorks Antarctic Bonney ENVELOPE(162.417,162.417,-77.717,-77.717) Lake Bonney ENVELOPE(-25.588,-25.588,-80.361,-80.361) Journal of Geophysical Research: Earth Surface 124 2 686 694
institution Open Polar
collection Montana State University (MSU): ScholarWorks
op_collection_id ftmontanastateu
language unknown
description Although perennially ice‐covered Antarctic lakes have experienced variable ice thicknesses over the past several decades, future ice thickness trends and associated aquatic biological responses under projected global warming remain unknown. Heat stored in the water column in chemically stratified Antarctic lakes that have middepth temperature maxima can significantly influence the ice thickness trends via upward heat flux to the ice/water interface. We modeled the ice thickness of the west lobe of Lake Bonney, Antarctica, based on possible future climate scenarios utilizing a 1D thermodynamic model that accounts for surface radiative fluxes as well as the heat flux associated with the temperature evolution of the water column. Model results predict that the ice cover of Lake Bonney will shift from perennial to seasonal within one to four decades, a change that will drastically influence ecosystem processes within the lake.
format Article in Journal/Newspaper
author Obryk, Maciej K.
Doran, Peter T.
Priscu, John C.
spellingShingle Obryk, Maciej K.
Doran, Peter T.
Priscu, John C.
Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
author_facet Obryk, Maciej K.
Doran, Peter T.
Priscu, John C.
author_sort Obryk, Maciej K.
title Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
title_short Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
title_full Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
title_fullStr Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
title_full_unstemmed Prediction of Ice-Free Conditions for a Perennially Ice-Covered Antarctic Lake
title_sort prediction of ice-free conditions for a perennially ice-covered antarctic lake
publishDate 2019
url https://scholarworks.montana.edu/xmlui/handle/1/15638
long_lat ENVELOPE(162.417,162.417,-77.717,-77.717)
ENVELOPE(-25.588,-25.588,-80.361,-80.361)
geographic Antarctic
Bonney
Lake Bonney
geographic_facet Antarctic
Bonney
Lake Bonney
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation Obryk, M. K., P. T. Doran, and J. C. Priscu. “Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake.” Journal of Geophysical Research: Earth Surface 124, no. 2 (February 2019): 686–694. doi:10.1029/2018jf004756.
2169-9003
https://scholarworks.montana.edu/xmlui/handle/1/15638
op_rights This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
http://rightsstatements.org/vocab/InC/1.0/
op_doi https://doi.org/10.1029/2018jf004756
container_title Journal of Geophysical Research: Earth Surface
container_volume 124
container_issue 2
container_start_page 686
op_container_end_page 694
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