Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan
We conducted 2 yr (2005–2007) of in situ meteorological and glaciological observations on the Gregoriev Glacier, a flat-top glacier within the Inner Tien Shan, Kyrgyzstan. Relative carrier-phase GPS surveys reveal a vertical lowering at the summit of the glacier. Based on snow density data and an en...
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Copernicus Publications
2011-07-01
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Series: | The Cryosphere |
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doaj-d8d9d10ddd01459c84687645ae7c7de22020-11-24T23:57:50ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242011-07-015353954910.5194/tc-5-539-2011Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien ShanK. FujitaN. TakeuchiS. A. NikitinA. B. SurazakovS. OkamotoV. B. AizenJ. KubotaWe conducted 2 yr (2005–2007) of in situ meteorological and glaciological observations on the Gregoriev Glacier, a flat-top glacier within the Inner Tien Shan, Kyrgyzstan. Relative carrier-phase GPS surveys reveal a vertical lowering at the summit of the glacier. Based on snow density data and an energy-mass balance model, we estimate that the annual precipitation and summer mean temperature required to maintain the glacier in the current state are 289 mm and −3.8 °C at the glacier summit (4600 m a.s.l.), respectively. The good agreement between dynamically derived precipitation and the long-term observed precipitation at a nearby station in the Tien Shan (296 mm at 3614 m a.s.l. for the period 1930–2002) suggests that the glacier has been in a near steady-state in terms of mass supply. The glacier mass-balance, reconstructed based on meteorological data from the Tien Shan station for the past 80 yr, explains the observed fluctuations in glacier extent, particularly the negative mass balance in the 1990s.http://www.the-cryosphere.net/5/539/2011/tc-5-539-2011.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
K. Fujita N. Takeuchi S. A. Nikitin A. B. Surazakov S. Okamoto V. B. Aizen J. Kubota |
spellingShingle |
K. Fujita N. Takeuchi S. A. Nikitin A. B. Surazakov S. Okamoto V. B. Aizen J. Kubota Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan The Cryosphere |
author_facet |
K. Fujita N. Takeuchi S. A. Nikitin A. B. Surazakov S. Okamoto V. B. Aizen J. Kubota |
author_sort |
K. Fujita |
title |
Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan |
title_short |
Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan |
title_full |
Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan |
title_fullStr |
Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan |
title_full_unstemmed |
Favorable climatic regime for maintaining the present-day geometry of the Gregoriev Glacier, Inner Tien Shan |
title_sort |
favorable climatic regime for maintaining the present-day geometry of the gregoriev glacier, inner tien shan |
publisher |
Copernicus Publications |
series |
The Cryosphere |
issn |
1994-0416 1994-0424 |
publishDate |
2011-07-01 |
description |
We conducted 2 yr (2005–2007) of in situ meteorological and glaciological observations on the Gregoriev Glacier, a flat-top glacier within the Inner Tien Shan, Kyrgyzstan. Relative carrier-phase GPS surveys reveal a vertical lowering at the summit of the glacier. Based on snow density data and an energy-mass balance model, we estimate that the annual precipitation and summer mean temperature required to maintain the glacier in the current state are 289 mm and −3.8 °C at the glacier summit (4600 m a.s.l.), respectively. The good agreement between dynamically derived precipitation and the long-term observed precipitation at a nearby station in the Tien Shan (296 mm at 3614 m a.s.l. for the period 1930–2002) suggests that the glacier has been in a near steady-state in terms of mass supply. The glacier mass-balance, reconstructed based on meteorological data from the Tien Shan station for the past 80 yr, explains the observed fluctuations in glacier extent, particularly the negative mass balance in the 1990s. |
url |
http://www.the-cryosphere.net/5/539/2011/tc-5-539-2011.pdf |
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