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dc.contributor.authorObryk, Maciej K.
dc.contributor.authorDoran, Peter T.
dc.contributor.authorHicks, J A
dc.contributor.authorMcKay, C P
dc.contributor.authorPriscu, John C.
dc.date.accessioned2017-02-21T15:51:23Z
dc.date.available2017-02-21T15:51:23Z
dc.date.issued2016-10
dc.identifier.citationObryk, M K, P T Doran, J A Hicks, C P McKay, and John C Priscu. "Modeling the thickness of perennial ice covers on stratified lakes of the Taylor Valley, Antarctica." Journal of Glaciology 62, no. 235 (October 2016): 825-834. DOI:https://dx.doi.org/ 10.1017/jog.2016.69.en_US
dc.identifier.issn0022-1430
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/12643
dc.description.abstractA 1-D ice cover model was developed to predict and constrain drivers of long-termice thickness trends in chemically stratified lakes of Taylor Valley, Antarctica. The model is driven by surface radiative heat fluxes and heat fluxes from the underlying water column. The model successfully reproduced 16 a (between 1996 and 2012) of ice thickness changes for the west lobe of Lake Bonney (average ice thickness = 3.53 m) and Lake Fryxell (average ice thickness = 4.22 m). Long-term ice thickness trends require coupling with the thermal structure of the water column. The heat stored within the temperature maximum of lakes exceeding a liquid water column depth of 20 m can either impede or facilitate ice thickness change depending on the predominant climatic trend (cooling or warming). As such, shallow (<20 m deep water columns) perennially ice-covered lakes without deep temperature maxima are more sensitive indicators of climate change. The long-term ice thickness trends are a result of surface energy flux and heat flux from the deep temperature maximum in the water column, the latter of which results from absorbed solar radiation.en_US
dc.description.sponsorshipOffice of Polar Programs (9810219, 0096250, 0832755, 1041742, 1115245); National Science Foundationen_US
dc.language.isoen_USen_US
dc.titleModeling the thickness of perennial ice covers on stratified lakes of the Taylor Valley, Antarcticaen_US
dc.typeArticleen_US
mus.citation.extentfirstpage825en_US
mus.citation.extentlastpage834en_US
mus.citation.issue235en_US
mus.citation.journaltitleJournal of Glaciologyen_US
mus.citation.volume62en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doihttps://dx.doi.org/ 10.1017/jog.2016.69en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.data.thumbpage3en_US


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