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過去500万年の間,西南極の氷床の成長と崩壊をモデル化しています
David Pollard1, Robert M DeConto
1Earth and Environmental Systems Institute, Pennsylvania State University, University Park, Pennsylvania 16802, USA. pollard@essc.psu.edu
Nature
|March 20, 2009
まとめ
西南極の氷床 (WAIS) は,過去500万年の間に急速な崩壊と回復を経験してきました. 氷河期と崩壊期間の劇的なシフトは,氷床の動態と海面上昇に関する新しい洞察を提供します.
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
- 気候モデリング
背景:
- 西南極の氷床 (WAIS) は海面上昇の可能性 (~5m) を有しており,壊滅的な崩壊に敏感です.
- 現在の接地線は海面下にあり,床は内陸に深く進み,脱走の撤退のリスクを高めています.
- 過去のWAISの変異とその要因を理解することは,将来の行動を予測する上で極めて重要です.
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