Hydrology of Tierney Creek, Vestfold Hills, Antarctica
Abstract The discharge in Tierney Creek from proglacial Chelnok Lake was recorded during the summer of 1987–1988. In addition, air temperature, water temperature, and radiation were recorded. Multiple linear regressions revealed that discharge could be predicted from recorded radiation and air tempe...
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Cambridge University Press (CUP)
1999
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crcambridgeupr:10.1017/s0032247400026486 2024-03-03T08:37:51+00:00 Hydrology of Tierney Creek, Vestfold Hills, Antarctica Bronge, Christian 1999 http://dx.doi.org/10.1017/s0032247400026486 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400026486 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 35, issue 193, page 139-148 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 1999 crcambridgeupr https://doi.org/10.1017/s0032247400026486 2024-02-08T08:49:17Z Abstract The discharge in Tierney Creek from proglacial Chelnok Lake was recorded during the summer of 1987–1988. In addition, air temperature, water temperature, and radiation were recorded. Multiple linear regressions revealed that discharge could be predicted from recorded radiation and air temperature in late summer. In early summer, other factors such as wind must also be taken into account. Long-term discharge fluctuations displayed response times that decreased during the runoff season due to the opening of the meltwater channels on the ice-margin. During parts of the runoff season, flow variations were modulated by nocturnal freezing in the creek, a phenomenon still more pronounced in Onyx River in the Dry Valleys of Victoria Land. Hydrologically, Tierney Creek resembled Onyx River, but, in the Onyx, the flow pattern was more exclusively determined by low air temperatures than it was in Tierney Creek. In the Dry Valleys, streams whose lengths, gradients, and discharges are of the same magnitude as those of Tierney Creek, also display similar recession coefficients and time lags between flow peak and insolation peak. Article in Journal/Newspaper Antarc* Antarctica Polar Record Victoria Land Cambridge University Press Victoria Land Vestfold Hills Vestfold Onyx River ENVELOPE(162.283,162.283,-77.500,-77.500) Chelnok ENVELOPE(78.367,78.367,-68.633,-68.633) Chelnok Lake ENVELOPE(78.341,78.341,-68.646,-68.646) Tierney Creek ENVELOPE(78.304,78.304,-68.641,-68.641) Polar Record 35 193 139 148 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development Bronge, Christian Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
description |
Abstract The discharge in Tierney Creek from proglacial Chelnok Lake was recorded during the summer of 1987–1988. In addition, air temperature, water temperature, and radiation were recorded. Multiple linear regressions revealed that discharge could be predicted from recorded radiation and air temperature in late summer. In early summer, other factors such as wind must also be taken into account. Long-term discharge fluctuations displayed response times that decreased during the runoff season due to the opening of the meltwater channels on the ice-margin. During parts of the runoff season, flow variations were modulated by nocturnal freezing in the creek, a phenomenon still more pronounced in Onyx River in the Dry Valleys of Victoria Land. Hydrologically, Tierney Creek resembled Onyx River, but, in the Onyx, the flow pattern was more exclusively determined by low air temperatures than it was in Tierney Creek. In the Dry Valleys, streams whose lengths, gradients, and discharges are of the same magnitude as those of Tierney Creek, also display similar recession coefficients and time lags between flow peak and insolation peak. |
format |
Article in Journal/Newspaper |
author |
Bronge, Christian |
author_facet |
Bronge, Christian |
author_sort |
Bronge, Christian |
title |
Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
title_short |
Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
title_full |
Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
title_fullStr |
Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
title_full_unstemmed |
Hydrology of Tierney Creek, Vestfold Hills, Antarctica |
title_sort |
hydrology of tierney creek, vestfold hills, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1999 |
url |
http://dx.doi.org/10.1017/s0032247400026486 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400026486 |
long_lat |
ENVELOPE(162.283,162.283,-77.500,-77.500) ENVELOPE(78.367,78.367,-68.633,-68.633) ENVELOPE(78.341,78.341,-68.646,-68.646) ENVELOPE(78.304,78.304,-68.641,-68.641) |
geographic |
Victoria Land Vestfold Hills Vestfold Onyx River Chelnok Chelnok Lake Tierney Creek |
geographic_facet |
Victoria Land Vestfold Hills Vestfold Onyx River Chelnok Chelnok Lake Tierney Creek |
genre |
Antarc* Antarctica Polar Record Victoria Land |
genre_facet |
Antarc* Antarctica Polar Record Victoria Land |
op_source |
Polar Record volume 35, issue 193, page 139-148 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400026486 |
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Polar Record |
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35 |
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193 |
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139 |
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148 |
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1792502128990748672 |