Position of Ice Divides and Ice Centers on Ice Sheets
Model calculations are made of the magnitude of the shift of the portion of an ice divide on a two dimensional ice sheet and of the “center” (the position of highest elevation) of a circular ice sheet when the rate of accumulation is different on different sides or in different sectors of an ice she...
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Language: | English |
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Cambridge University Press (CUP)
1973
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Online Access: | http://dx.doi.org/10.1017/s0022143000031774 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031774 |
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crcambridgeupr:10.1017/s0022143000031774 2024-03-03T08:45:22+00:00 Position of Ice Divides and Ice Centers on Ice Sheets Weertman, J. 1973 http://dx.doi.org/10.1017/s0022143000031774 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031774 en eng Cambridge University Press (CUP) Journal of Glaciology volume 12, issue 66, page 353-360 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1973 crcambridgeupr https://doi.org/10.1017/s0022143000031774 2024-02-08T08:34:04Z Model calculations are made of the magnitude of the shift of the portion of an ice divide on a two dimensional ice sheet and of the “center” (the position of highest elevation) of a circular ice sheet when the rate of accumulation is different on different sides or in different sectors of an ice sheet. It is concluded that gross changes in the accumulation pattern are required to cause an appreciable shift of the position of ice divides or ice centers if the positions of the edge of the ice sheet are fixed. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 12 66 353 360 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Weertman, J. Position of Ice Divides and Ice Centers on Ice Sheets |
topic_facet |
Earth-Surface Processes |
description |
Model calculations are made of the magnitude of the shift of the portion of an ice divide on a two dimensional ice sheet and of the “center” (the position of highest elevation) of a circular ice sheet when the rate of accumulation is different on different sides or in different sectors of an ice sheet. It is concluded that gross changes in the accumulation pattern are required to cause an appreciable shift of the position of ice divides or ice centers if the positions of the edge of the ice sheet are fixed. |
format |
Article in Journal/Newspaper |
author |
Weertman, J. |
author_facet |
Weertman, J. |
author_sort |
Weertman, J. |
title |
Position of Ice Divides and Ice Centers on Ice Sheets |
title_short |
Position of Ice Divides and Ice Centers on Ice Sheets |
title_full |
Position of Ice Divides and Ice Centers on Ice Sheets |
title_fullStr |
Position of Ice Divides and Ice Centers on Ice Sheets |
title_full_unstemmed |
Position of Ice Divides and Ice Centers on Ice Sheets |
title_sort |
position of ice divides and ice centers on ice sheets |
publisher |
Cambridge University Press (CUP) |
publishDate |
1973 |
url |
http://dx.doi.org/10.1017/s0022143000031774 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031774 |
genre |
Ice Sheet Journal of Glaciology |
genre_facet |
Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology volume 12, issue 66, page 353-360 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000031774 |
container_title |
Journal of Glaciology |
container_volume |
12 |
container_issue |
66 |
container_start_page |
353 |
op_container_end_page |
360 |
_version_ |
1792500909100498944 |