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斜率のペースのプレオセンの西南極氷床の振動は,斜率のペースのプレオセンの西南極氷床の振動です
1Antarctic Research Centre, Victoria University of Wellington, Kelburn Parade, PO Box 600, Wellington 6012, New Zealand. tim.naish@vuw.ac.nz
Nature
|March 20, 2009
まとめ
軌道サイクルにより,西南極の氷床は,より暖かいプレオセンの時期に繰り返し崩壊した. これは,将来の氷床の行動と海面上昇を予測するための重要なデータを提供します.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 氷河学 氷河学とは
- 海洋地質学 海洋地質学
背景:
- 軌道周期は地球の氷河期に影響を及ぼすことが知られているが,南極の氷床の反応は不明である.
- 西南極の氷床 (WAIS) がより暖かいプレオセンの時代にどのように振る舞ったかを理解することは,将来の地球温暖化の影響を予測するために不可欠です.
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