The Cryosphere Utility of late summer transient snowline migration rate on Taku
Abstract. On Taku Glacier, Alaska a combination of field observations of snow water equivalent (SWE) from snowpits and probing in the vicinity of the transient snowline (TSL) are used to quantify the mass balance gradient. The balance gradient derived from the TSL and SWE measured in snowpits at 100...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.364.1177 2023-05-15T16:20:32+02:00 The Cryosphere Utility of late summer transient snowline migration rate on Taku M. Pelto The Pennsylvania State University CiteSeerX Archives 2011 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.1177 http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.1177 http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf text 2011 ftciteseerx 2016-01-08T00:57:53Z Abstract. On Taku Glacier, Alaska a combination of field observations of snow water equivalent (SWE) from snowpits and probing in the vicinity of the transient snowline (TSL) are used to quantify the mass balance gradient. The balance gradient derived from the TSL and SWE measured in snowpits at 1000 m from 1998–2010 ranges from 2.6– 3.8 mm m −1. Probing transects from 950 m–1100 m directly measure SWE and yield a slightly higher balance gradient of 3.3–3.8 mm m −1. The TSL on Taku Glacier is identified in MODIS and Landsat 4 and 7 Thematic Mapper images for 31 dates during the 2004–2010 period to assess the consistency of its rate of rise and reliability in assessing ablation for mass balance assessment. For example, in 2010, the TSL Text glacier Alaska Unknown Taku ENVELOPE(-133.854,-133.854,59.633,59.633) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Abstract. On Taku Glacier, Alaska a combination of field observations of snow water equivalent (SWE) from snowpits and probing in the vicinity of the transient snowline (TSL) are used to quantify the mass balance gradient. The balance gradient derived from the TSL and SWE measured in snowpits at 1000 m from 1998–2010 ranges from 2.6– 3.8 mm m −1. Probing transects from 950 m–1100 m directly measure SWE and yield a slightly higher balance gradient of 3.3–3.8 mm m −1. The TSL on Taku Glacier is identified in MODIS and Landsat 4 and 7 Thematic Mapper images for 31 dates during the 2004–2010 period to assess the consistency of its rate of rise and reliability in assessing ablation for mass balance assessment. For example, in 2010, the TSL |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
M. Pelto |
spellingShingle |
M. Pelto The Cryosphere Utility of late summer transient snowline migration rate on Taku |
author_facet |
M. Pelto |
author_sort |
M. Pelto |
title |
The Cryosphere Utility of late summer transient snowline migration rate on Taku |
title_short |
The Cryosphere Utility of late summer transient snowline migration rate on Taku |
title_full |
The Cryosphere Utility of late summer transient snowline migration rate on Taku |
title_fullStr |
The Cryosphere Utility of late summer transient snowline migration rate on Taku |
title_full_unstemmed |
The Cryosphere Utility of late summer transient snowline migration rate on Taku |
title_sort |
cryosphere utility of late summer transient snowline migration rate on taku |
publishDate |
2011 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.1177 http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf |
long_lat |
ENVELOPE(-133.854,-133.854,59.633,59.633) |
geographic |
Taku |
geographic_facet |
Taku |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_source |
http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.364.1177 http://www.the-cryosphere.net/5/1127/2011/tc-5-1127-2011.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766008450933850112 |