author_facet Hooke, Roger LeB.
Hooke, Roger LeB.
author Hooke, Roger LeB.
spellingShingle Hooke, Roger LeB.
Quaternary Research
Basal Temperatures in Polar Ice Sheets: A Qualitative Review
General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
author_sort hooke, roger leb.
spelling Hooke, Roger LeB. 0033-5894 1096-0287 Cambridge University Press (CUP) General Earth and Planetary Sciences Earth-Surface Processes Arts and Humanities (miscellaneous) http://dx.doi.org/10.1016/0033-5894(77)90011-4 <jats:p>In recent years glacial geologists have become increasingly interested in the thermal regime at the bases of polar ice sheets, and have attempted to interpret certain Pleistocene glacial features in terms of this thermal regime. This effort has suffered from a lack of a reasonably comprehensive but qualitative review of factors controlling the temperature at the base of a polar glacier; this paper attempts to fill this void. Using the Laurentide Ice Sheet as an example, it is shown that under cold climatic conditions basal melting is likely to occur only beneath the lower part of the ablation area. If the climate is somewhat warmer, or if the accumulation rate is sufficiently low, basal melting may also occur beneath the accumulation area. The zone of greatest basal melt-water production is probably beneath the lower part of the ablation area.</jats:p> Basal Temperatures in Polar Ice Sheets: A Qualitative Review Quaternary Research
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title Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_unstemmed Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_full Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_fullStr Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_full_unstemmed Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_short Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_sort basal temperatures in polar ice sheets: a qualitative review
topic General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
url http://dx.doi.org/10.1016/0033-5894(77)90011-4
publishDate 1977
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description <jats:p>In recent years glacial geologists have become increasingly interested in the thermal regime at the bases of polar ice sheets, and have attempted to interpret certain Pleistocene glacial features in terms of this thermal regime. This effort has suffered from a lack of a reasonably comprehensive but qualitative review of factors controlling the temperature at the base of a polar glacier; this paper attempts to fill this void. Using the Laurentide Ice Sheet as an example, it is shown that under cold climatic conditions basal melting is likely to occur only beneath the lower part of the ablation area. If the climate is somewhat warmer, or if the accumulation rate is sufficiently low, basal melting may also occur beneath the accumulation area. The zone of greatest basal melt-water production is probably beneath the lower part of the ablation area.</jats:p>
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spelling Hooke, Roger LeB. 0033-5894 1096-0287 Cambridge University Press (CUP) General Earth and Planetary Sciences Earth-Surface Processes Arts and Humanities (miscellaneous) http://dx.doi.org/10.1016/0033-5894(77)90011-4 <jats:p>In recent years glacial geologists have become increasingly interested in the thermal regime at the bases of polar ice sheets, and have attempted to interpret certain Pleistocene glacial features in terms of this thermal regime. This effort has suffered from a lack of a reasonably comprehensive but qualitative review of factors controlling the temperature at the base of a polar glacier; this paper attempts to fill this void. Using the Laurentide Ice Sheet as an example, it is shown that under cold climatic conditions basal melting is likely to occur only beneath the lower part of the ablation area. If the climate is somewhat warmer, or if the accumulation rate is sufficiently low, basal melting may also occur beneath the accumulation area. The zone of greatest basal melt-water production is probably beneath the lower part of the ablation area.</jats:p> Basal Temperatures in Polar Ice Sheets: A Qualitative Review Quaternary Research
spellingShingle Hooke, Roger LeB., Quaternary Research, Basal Temperatures in Polar Ice Sheets: A Qualitative Review, General Earth and Planetary Sciences, Earth-Surface Processes, Arts and Humanities (miscellaneous)
title Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_full Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_fullStr Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_full_unstemmed Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_short Basal Temperatures in Polar Ice Sheets: A Qualitative Review
title_sort basal temperatures in polar ice sheets: a qualitative review
title_unstemmed Basal Temperatures in Polar Ice Sheets: A Qualitative Review
topic General Earth and Planetary Sciences, Earth-Surface Processes, Arts and Humanities (miscellaneous)
url http://dx.doi.org/10.1016/0033-5894(77)90011-4