固い地球と海面のフィードバックによる南極の大量損失の減速
E Larour1,2, H Seroussi3, S Adhikari3
1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA. eric.larour@jpl.nasa.gov.
まとめ
固い地球の上昇は 極地の氷床を安定させます 新しいシミュレーションは,この効果がスワイツ氷河を縮小することを示しています.
科学分野:
- 固体地球物理学
- 氷河学
- 南極の気候科学
背景:
- 地質学的な研究は 固体地質の上昇が 極地の氷床を安定させることを示しています
- 接地線近くの短波上昇の影響は未評価のままである.
研究 の 目的:
- 南極の氷床の進化をシミュレートする
- 短期的な固体地球の上昇が 接地線の移動に与える影響を評価する.
主な方法:
- 南極の氷床の進化を 高解像度でシミュレーションした
- 氷床に影響を与える全ての固体地球過程を組み込んだ.
主要な成果:
- Thwaites Glacierのグラウンドラインの移動に38%のネガティブなフィードバックが予測されています.
- このフィードバックは海面上昇の 26.8%の減少に相当します
結論:
- 短波の固体地球上昇は,接地ラインの安定性に大きく影響します.
- このメカニズムは 南極の氷床の安定化に 重要なフィードバックをもたらします
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