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- 仲山 智子
- 北海道大学低温科学研究所
書誌事項
- タイトル別名
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- Numerical estimation of the permafrost variation on the Daisetsu Mountains,Hokkaido,since the Last Glacial Maximum.
- ホッカイドウ ダイセツザン ニ オケル サイシュウ ヒョウキ イコウ ノ エイ
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The objective of this study is to estimate the response of the permafrost at the Daisetsu Mountains, central Hokkaido to a continuous climatic change. A one-dimensional, nonsteady state, heat conduction model with phase change is used to calculate the change of permafrost thickness during the last 20, 000 years. The result of simulation shows that the permafrost responded quickly to the surface temperature change and it has remained without thaw since the Last Glacial Maximum. The minimum permafrost thickness is estimated at 11.5 m at about 5 kyr B. P. and reached to 30.1 m at present. The simulation also indicates that the permafrost thickness is sensitive to soil water content and ground heat flow.
収録刊行物
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- 雪氷
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雪氷 57 (2), 125-132, 1995
公益社団法人 日本雪氷学会
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詳細情報 詳細情報について
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- CRID
- 1390282681437659008
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- NII論文ID
- 10002381636
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- NII書誌ID
- AN00131221
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- ISSN
- 18836267
- 03731006
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- NDL書誌ID
- 3624231
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
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- 抄録ライセンスフラグ
- 使用不可