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大気 の 川 は,暖かい 冬 と 極端 な 暑さ を 引き起こし ます
Serena R Scholz1, Juan M Lora2
1Yale University, Department of Earth and Planetary Sciences, New Haven, CT, USA. serena.scholz@yale.edu.
Nature
|December 18, 2024
まとめ
大気川は熱と水分を輸送し,中緯度の地域を大幅に暖める. これらの極端な気象現象は5~10°Cの異常気温と 複合的な熱波に関連しています
科学分野:
- 大気科学
- 気候科学
- 気象学
背景:
- 大気流 (ARs) は,極方向の水分輸送の主要な原動力である.
- ARは降水量と水資源に 世界的に影響を及ぼします
- 地表近くの気温に対するARの影響は,まだ十分に定義されていない.
研究 の 目的:
- ARによる熱輸送が地球上の地表近くの気温に与える影響を調査する.
- ARイベントに関連した温度異常を定量化します.
- 極端な気温や熱波における AR の役割を評価する.
主な方法:
- 大気データを分析して,ARの頻度と関連する温度異常を特定する.
- 異常な水平の熱と水分輸送の定量化
- ARイベント中の表面エネルギー流と放射線の評価.
主要な成果:
- 頻度が高い季節は,平均より高い温度を示します.
- ARは5〜10°Cの温度異常と関連しています.
- 極端な温度の異常の70%以上は,中緯度のAR内で発生します.
- ARは世界中の湿気や複合熱波に関連しています.
結論:
- ARは様々な時間スケールで気温に大きな影響を与える.
- ARは世界のエネルギー輸送に 重要な役割を果たしています
- モデルにARを組み込むことで 極端な熱の予測が改善できます
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