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広範囲にわたる北東グリーンランド氷河の薄化と加速
Shfaqat A Khan1, Youngmin Choi2, Mathieu Morlighem3,4
1DTU Space, Technical University of Denmark, Kongens Lyngby, Denmark. abbas@space.dtu.dk.
Nature
|November 9, 2022
まとめ
グリーンランド
科学分野:
- 氷河学 と 気候 科学
- 地球システム科学
背景:
- グリーンランドの氷床は 融解と氷の放出によって 質量を失っています
- 北東グリーンランド氷河流 (NEGIS) は,急速な後退に脆弱な重要な地域です.
- 将来の氷の減少の加速とその規模は不明である.
研究 の 目的:
- NEGISの氷の流れに対する正面の変化の影響を調査する.
- NEGISからの将来の海面上昇の貢献を予測する.
- 氷床の質量バランスの数値モデルを改良する
主な方法:
- グローバル・ナビゲーション・サテライト・システム (GNSS) の観測を活用した.
- 衛星による地表の上昇と速度の変化を分析した.
- ベース条件を更新した数値モデルを使用した.
主要な成果:
- 2012年のフロントの変化から200km内陸に広がる加速と薄まりを観測した.
- 2100年までに世界の海面上昇に 13.5~15.5mmのNEGISの貢献が予測されている.
- 内陸の氷のダイナミクスが 将来の質量バランスの予測を制限することを示した.
結論:
- NEGISは急速に変化しており,将来の海面上昇に重大な影響を及ぼします.
- 内陸の氷の動態は 海面上昇の正確な予測に不可欠です
- 微妙な内陸の変化は 氷床モデルを改良するために 重要なデータを提供します
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