シミュレートされた温室気候におけるエピソード的洪水
Jacob T Seeley1, Robin D Wordsworth2,3
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA. jacob.t.seeley@gmail.com.
Nature
|November 4, 2021
まとめ
温室気候は,低熱帯圏の放射性加熱を示し,水循環が
科学分野:
- 気候科学
- 大気物理学
- 地球システム科学
背景:
- 温室気候は,典型的な冷却とは異なり,低熱圏の放射性加熱によって特徴付けられます.
- 以前のモデルでは,コンベクティブスケールの動きが解明できず,温室大気の振る舞いはよくわかっていなかった.
研究 の 目的:
- 温室気候状態における大気動態を調査する.
- 水循環と雲の覆いに対する下層熱圏の放射性加熱の影響を理解する.
主な方法:
- 気候シミュレーションを行い,コンベクションを明示的に解決しました.
- 模擬温室条件下での水循環と雲の振る舞いを分析した.
主要な成果:
- 水循環が準安定状態から"リラックスオシレータ"状態に変化した.
- 干ばつによって隔てられた激しい降雨の爆発を観測した.
- 局所的な降水量が増加し 雲の覆いが増加し 暫定的に不安定な気候フィードバックのパラメータが見つかりました
結論:
- 温室気候は"時間的な"コンベクティブ自己組織化を示し得る.
- これらの発見は,極端な温暖な気候における雲の動態と侵食プロセスに意味を持っています.
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