永久凍った湖の氷の厚さ
C P McKay1, G D Clow, R A Wharton
1Solar System Exploration Office, NASA-Ames Research Center, Moffett Field, California 94035, USA.
Nature
|February 14, 1985
まとめ
南極の乾燥渓谷湖は,熱伝導,潜在的熱放出,太陽光によるバランスのために一貫した氷の厚さを持っています. エネルギーバランスモデルは,測定された消去率を使用してこの現象を説明します.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- リムテクノロジーとは
- 極地科学は,極地科学である.
背景:
- 南極の乾燥谷には,恒常的な氷の覆いを持つユニークな湖があります.
- 氷の覆いは,これらの湖のユニークな物理的および生物学的性質に影響します.
- 湖の氷の厚さは,水の性質の変動にもかかわらず,著しく一貫しています.
研究 の 目的:
- 南極の湖で観察された一貫した氷の厚さを説明するために.
- 湖の氷の厚さのエネルギーバランスモデルを提示する.
主な方法:
- シンプルなエネルギーバランスモデルを開発した.
- 利用した測定された表面除去率は30cm/年-1.1でした.
主要な成果:
- このモデルは,観察された湖の氷の厚さをうまく説明しています.
- 氷の厚さは,主に氷と水の界面でのエネルギーバランスによって決定されます.
- 太陽光の伝達と吸収は,氷の厚さにも影響を与えます.
結論:
- エネルギーバランスモデルは,南極の乾燥した渓谷における一貫した湖氷の厚さの明確な説明を提供します.
- 溶解速度は,潜在的熱放出を制御する重要な要因であり,したがって氷の厚さです.
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