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温暖化に起因する雪の減少は,極端な降雨量を増大させる
Mohammed Ombadi1,2, Mark D Risser3, Alan M Rhoades3
1Earth and Environmental Sciences Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USA. ombadi@lbl.gov.
Nature
|June 28, 2023
まとめ
北半球の高層地域では 温暖化による雪から雨への変化により 極端な降雨が予想より速く増えています この増加は 洪水に対する脆弱性を強調し 緊急に気候変動への適応計画が必要です
科学分野:
- 気候科学
- 水学
- 環境科学
背景:
- 極端な降雨は水資源の持続可能性に 大きな課題をもたらします
- 極端な降雨は特に衝撃的で 洪水や山崩れを引き起こします
- 以前の研究では,液体 (雨) と固体 (雪) の極端な降雨を区別していなかった.
研究 の 目的:
- 高度地域での極端な降雨の増大を調査する.
- 降水段階 (雨と雪) が極端な降雨予測に影響するかどうかを判断する.
- 気候モデルの不確実性における雪雨分割の役割を理解する.
主な方法:
- 気候再分析データセットの分析
- 将来の気候モデルの予測を利用する.
- 雪と雨の分断の変化を調べる
主要な成果:
- 北半球の高地地域では 極端な降雨が増加し 温暖化1度当たり15%増加します
- この増幅は 温暖化による 雪から雨への変化によって引き起こされています
- 雪と雨の分割の変化は,極端な降雨の予測におけるモデル間不確実性の重要な部分を説明します.
結論:
- 高地地域は,極端な降雨に関連する危険性のある"ホットスポット"として特定されています.
- 脆弱な高地地域に対する 強力な気候適応計画が必要です
- この研究は,将来の極端な降雨予測の不確実性を減らす方法を提供します.
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