Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing
Abstract Climatic change occurs over a wide range of time scales. Each glacier responds in a unique fashion to this spectrum of climatic forcings. The response of the extent of the Lewis Glacier terminus to sinusoidal fluctuation in the net balance is calculated. The net balance versus elevation pro...
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1984
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Online Access: | http://dx.doi.org/10.1017/s0022143000005943 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005943 |
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crcambridgeupr:10.1017/s0022143000005943 2023-06-11T04:13:28+02:00 Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing Kruss, Phillip 1984 http://dx.doi.org/10.1017/s0022143000005943 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005943 en eng Cambridge University Press (CUP) Journal of Glaciology volume 30, issue 105, page 212-217 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1984 crcambridgeupr https://doi.org/10.1017/s0022143000005943 2023-05-01T18:20:36Z Abstract Climatic change occurs over a wide range of time scales. Each glacier responds in a unique fashion to this spectrum of climatic forcings. The response of the extent of the Lewis Glacier terminus to sinusoidal fluctuation in the net balance is calculated. The net balance versus elevation profile is separately translated along the orthogonal balance and elevation axes. Net balance amplitudes of 0.1 to 0.5 m a −1 of ice and 10 to 50 m elevation, respectively, and periods ranging from 20 to 1000 years are covered. The time lag between forcing and terminus response is dependent on applied period, reaching a maximum of about 30 years at 1000 years period, but is independent of applied amplitude. For the shorter applied periods the response amplitude increases rapidly with period but asymptotically approaches a maximum at periods above approximately 200 years; it is linearly dependent on applied amplitude. Consideration of the Lewis Glacier response taken in perspective with similar results for other alpine glaciers identifies general characteristics of the terminus response. Article in Journal/Newspaper Journal of Glaciology Lewis Glacier Cambridge University Press (via Crossref) Journal of Glaciology 30 105 212 217 |
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Open Polar |
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Cambridge University Press (via Crossref) |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Kruss, Phillip Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
topic_facet |
Earth-Surface Processes |
description |
Abstract Climatic change occurs over a wide range of time scales. Each glacier responds in a unique fashion to this spectrum of climatic forcings. The response of the extent of the Lewis Glacier terminus to sinusoidal fluctuation in the net balance is calculated. The net balance versus elevation profile is separately translated along the orthogonal balance and elevation axes. Net balance amplitudes of 0.1 to 0.5 m a −1 of ice and 10 to 50 m elevation, respectively, and periods ranging from 20 to 1000 years are covered. The time lag between forcing and terminus response is dependent on applied period, reaching a maximum of about 30 years at 1000 years period, but is independent of applied amplitude. For the shorter applied periods the response amplitude increases rapidly with period but asymptotically approaches a maximum at periods above approximately 200 years; it is linearly dependent on applied amplitude. Consideration of the Lewis Glacier response taken in perspective with similar results for other alpine glaciers identifies general characteristics of the terminus response. |
format |
Article in Journal/Newspaper |
author |
Kruss, Phillip |
author_facet |
Kruss, Phillip |
author_sort |
Kruss, Phillip |
title |
Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
title_short |
Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
title_full |
Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
title_fullStr |
Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
title_full_unstemmed |
Terminus Response of Lewis Glacier, Mount Kenya, Kenya, to Sinusoidal Net-Balance Forcing |
title_sort |
terminus response of lewis glacier, mount kenya, kenya, to sinusoidal net-balance forcing |
publisher |
Cambridge University Press (CUP) |
publishDate |
1984 |
url |
http://dx.doi.org/10.1017/s0022143000005943 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000005943 |
genre |
Journal of Glaciology Lewis Glacier |
genre_facet |
Journal of Glaciology Lewis Glacier |
op_source |
Journal of Glaciology volume 30, issue 105, page 212-217 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000005943 |
container_title |
Journal of Glaciology |
container_volume |
30 |
container_issue |
105 |
container_start_page |
212 |
op_container_end_page |
217 |
_version_ |
1768390525032857600 |