21世紀の海面上昇に対する氷河の貢献に対する運動的制約
W T Pfeffer1, J T Harper, S O'Neel
1Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. pfeffer@tintin.colorado.edu
まとめ
2100年までに海面が2メートル以上上昇することは,物理的に不可能です. 合理的で加速された条件では,海面上昇は約0.8mの上昇を示唆し,将来の海面上昇予測のベースラインを提供している.
科学分野:
- 氷河学 氷河学とは
- 気候科学 気候科学
- 海面上昇に関する研究
背景:
- 気候モデルと過去の状況は,2100年までにマルチメーターの海面上昇の可能性を示唆しています.
- 以前の予測は,極端な海面上昇のシナリオのための氷河学的条件を完全に制限しませんでした.
研究 の 目的:
- 2100年までにマルチメーターの海面上昇の氷河学的実現可能性を評価する.
- 海面上昇予測のための物理的に妥当なシナリオを確立する.
主な方法:
- 氷床の質量損失を大きくするために必要な氷河学的条件の分析.
- 氷の流れ動力の物理的限界に基づく制約されたシナリオの開発.
- 様々な加速率の下でのモデル化された海面上昇の比較.
主要な成果:
- 2100年までに海面上昇が2メートルを超えると,現在の理解では物理的に維持できないと考えられています.
- 2100年までに海面が2メートル上昇することは,すべての変数の極端で急速な加速の下でのみ可能である.
- もっと妥当で加速された条件は,2100年までに海面が合計で約0.8メートル上昇することを示しています.
結論:
- 2100年までに海面上昇が物理的に妥当であることの上限は,いくつかの提案されたシナリオよりも著しく低い.
- この結果は,気候モデルの精錬に不可欠な海面上昇の"最も可能性が高い"範囲を提供します.
- 将来の海平面予測には,詳細な氷の流れ動態と現実的な氷河学的制約が含まれなければならない.
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