Seasonality of snow accumulation at Mount Wrangell, Alaska, USA
We recorded the burial times of temperature sensors mounted on a specially constructed tower to determine snow accumulation during individual storms in the summit caldera of Mount Wrangell, Alaska, USA, (628 N, 1448W; 4100ma.s.l.) during the accumulation year June 2005 to June 2006. The experiment s...
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fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/34707 2023-05-15T16:20:33+02:00 Seasonality of snow accumulation at Mount Wrangell, Alaska, USA Kanamori, Syosaku Benson, Carl S. Truffer, Martin Matoba, Sumito Solie, Daniel J. Shiraiwa, Takayuki http://hdl.handle.net/2115/34707 https://doi.org/10.3189/002214308784886081 eng eng International Glaciological Society http://www.igsoc.org/ http://hdl.handle.net/2115/34707 Journal of Glaciology, 54(185): 273-278 http://dx.doi.org/10.3189/002214308784886081 © 2008 International Glaciological Society 氷河 アラスカ ランゲル山 涵養量 氷コア glacier Alaska Mt. Wrangell Accumulation rate Ice core 452 article fthokunivhus https://doi.org/10.3189/002214308784886081 2022-11-18T01:01:37Z We recorded the burial times of temperature sensors mounted on a specially constructed tower to determine snow accumulation during individual storms in the summit caldera of Mount Wrangell, Alaska, USA, (628 N, 1448W; 4100ma.s.l.) during the accumulation year June 2005 to June 2006. The experiment showed most of the accumulation occurred in episodic large storms, and half of the total accumulation was delivered in late summer. The timing of individual events correlated well with storms recorded upwind, at Cordova, the closest Pacific coastal weather station (200kmsouthsoutheast), although the magnitude of events showed only poor correlation. Hence, snow accumulation at Mount Wrangell appears to be a reflection of synoptic-scale regional weather systems. The accumulation at Mount Wrangell’s summit (>2.5mw.e.) exceeded the precipitation at Cordova. Although the direct relationship between accumulation of individual storms at the summit of Mount Wrangell and precipitation events at Cordova may be unique in the region, it is useful for interpreting ice cores obtained on Mount Wrangell. This is especially the case here because the high rate of accumulation allows high time resolution within the core. Article in Journal/Newspaper glacier ice core Journal of Glaciology Alaska Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Pacific Journal of Glaciology 54 185 273 278 |
institution |
Open Polar |
collection |
Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) |
op_collection_id |
fthokunivhus |
language |
English |
topic |
氷河 アラスカ ランゲル山 涵養量 氷コア glacier Alaska Mt. Wrangell Accumulation rate Ice core 452 |
spellingShingle |
氷河 アラスカ ランゲル山 涵養量 氷コア glacier Alaska Mt. Wrangell Accumulation rate Ice core 452 Kanamori, Syosaku Benson, Carl S. Truffer, Martin Matoba, Sumito Solie, Daniel J. Shiraiwa, Takayuki Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
topic_facet |
氷河 アラスカ ランゲル山 涵養量 氷コア glacier Alaska Mt. Wrangell Accumulation rate Ice core 452 |
description |
We recorded the burial times of temperature sensors mounted on a specially constructed tower to determine snow accumulation during individual storms in the summit caldera of Mount Wrangell, Alaska, USA, (628 N, 1448W; 4100ma.s.l.) during the accumulation year June 2005 to June 2006. The experiment showed most of the accumulation occurred in episodic large storms, and half of the total accumulation was delivered in late summer. The timing of individual events correlated well with storms recorded upwind, at Cordova, the closest Pacific coastal weather station (200kmsouthsoutheast), although the magnitude of events showed only poor correlation. Hence, snow accumulation at Mount Wrangell appears to be a reflection of synoptic-scale regional weather systems. The accumulation at Mount Wrangell’s summit (>2.5mw.e.) exceeded the precipitation at Cordova. Although the direct relationship between accumulation of individual storms at the summit of Mount Wrangell and precipitation events at Cordova may be unique in the region, it is useful for interpreting ice cores obtained on Mount Wrangell. This is especially the case here because the high rate of accumulation allows high time resolution within the core. |
format |
Article in Journal/Newspaper |
author |
Kanamori, Syosaku Benson, Carl S. Truffer, Martin Matoba, Sumito Solie, Daniel J. Shiraiwa, Takayuki |
author_facet |
Kanamori, Syosaku Benson, Carl S. Truffer, Martin Matoba, Sumito Solie, Daniel J. Shiraiwa, Takayuki |
author_sort |
Kanamori, Syosaku |
title |
Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
title_short |
Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
title_full |
Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
title_fullStr |
Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
title_full_unstemmed |
Seasonality of snow accumulation at Mount Wrangell, Alaska, USA |
title_sort |
seasonality of snow accumulation at mount wrangell, alaska, usa |
publisher |
International Glaciological Society |
url |
http://hdl.handle.net/2115/34707 https://doi.org/10.3189/002214308784886081 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
glacier ice core Journal of Glaciology Alaska |
genre_facet |
glacier ice core Journal of Glaciology Alaska |
op_relation |
http://www.igsoc.org/ http://hdl.handle.net/2115/34707 Journal of Glaciology, 54(185): 273-278 http://dx.doi.org/10.3189/002214308784886081 |
op_rights |
© 2008 International Glaciological Society |
op_doi |
https://doi.org/10.3189/002214308784886081 |
container_title |
Journal of Glaciology |
container_volume |
54 |
container_issue |
185 |
container_start_page |
273 |
op_container_end_page |
278 |
_version_ |
1766008476547416064 |