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  1. 防災科研関係論文

Numerical simulation of extreme snowmelt observed at the SIGMA-A site, northwest Greenland, during summer 2012

https://nied-repo.bosai.go.jp/records/5915
https://nied-repo.bosai.go.jp/records/5915
04383297-dc0b-4e0b-89b8-3af956309418
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Numerical simulation of extreme snowmelt observed at the SIGMA-A site, northwest Greenland, during summer 2012
言語
言語 eng
著者 M. Niwano

× M. Niwano

en M. Niwano

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T. Aoki

× T. Aoki

en T. Aoki

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S. Matoba

× S. Matoba

en S. Matoba

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S. Yamaguchi

× S. Yamaguchi

en S. Yamaguchi

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T. Tanikawa

× T. Tanikawa

en T. Tanikawa

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K. Kuchiki

× K. Kuchiki

en K. Kuchiki

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H. Motoyama

× H. Motoyama

en H. Motoyama

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抄録
内容記述タイプ Other
内容記述 The surface energy balance (SEB) from 30 June to 14 July 2012 at site SIGMA (Snow Impurity and Glacial Microbe effects on abrupt warming in the Arctic)-A, (78 degrees 03'N, 67 degrees 38'W; 1490 ma.s.l.) on the northwest Greenland Ice Sheet (GrIS) was investigated by using in situ atmospheric and snow measurements as well as numerical modeling with a one-dimensional multi-layered physical snowpack model called SMAP (Snow Metamorphism and Albedo Process). At SIGMA-A, remarkable near-surface snowmelt and continuous heavy rainfall (accumulated precipitation between 10 and 14 July was estimated to be 100 mm) were observed after 10 July 2012. Application of the SMAP model to the GrIS snowpack was evaluated based on the snow temperature profile, snow surface temperature, surface snow grain size, and shortwave albedo, all of which the model simulated reasonably well. Above all, the fact that the SMAP model successfully reproduced frequently observed rapid increases in snow albedo under cloudy conditions highlights the advantage of the physically based snow albedo model (PBSAM) incorporated in the SMAP model. Using such data and model, we estimated the SEB at SIGMA-A from 30 June to 14 July 2012. Radiation-related fluxes were obtained from in situ measurements, whereas other fluxes were calculated with the SMAP model. By examining the components of the SEB, we determined that low-level clouds accompanied by a significant temperature increase played an important role in the melt event observed at SIGMA-A. These conditions induced a remarkable surface heating via cloud radiative forcing in the polar region.
言語 en
書誌情報 en : The Cryosphere

巻 9, 号 3, p. 971-988, 発行日 2015-05-11
出版者
言語 en
出版者 Copernicus {GmbH}
ISSN
収録物識別子タイプ EISSN
収録物識別子 1994-0424
DOI
関連識別子 10.5194/tc-9-971-2015
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