南半球の大気循環の大規模な周期的な変動
David W J Thompson1, Elizabeth A Barnes
1Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA.
まとめ
南半球の大気循環は,バロクリニック環状モードに関連した20〜30日周期を示しています. この気候の振動は,熱,エネルギー,降雨に影響を与え,中緯度の変動に影響を与えます.
科学分野:
- 気候科学 気候科学
- 大気ダイナミクス 大気ダイナミクス
- 気象学 気象学 気象学
背景:
- 気候システムの周期性は,天気予報と気候の変動性の理解に不可欠です.
- 南半球の大気循環パターンは,世界の気象システムに影響を与えます.
研究 の 目的:
- 南半球の大気循環における周期的な行動を特定し,特徴づけること.
- この観察された周期性を駆動する物理的メカニズムを調査する.
主な方法:
- 大気データの半球スケール平均の分析.
- 熱の渦流,渦の運動エネルギー,降雨の渦流の調査.
- 気候ダイナミクスの観察的および理論的分析.
主要な成果:
- 南半球の大気循環で顕著な周期性 (20〜30日) を示した.
- この周期性を南半球のバロクリニック環状モードと関連付けました.
- 熱流,運動エネルギー,降水における周期性の出現を観測した.
結論:
- 20〜30日間の振動は,熱帯域外のバロクリニシティ,波の熱流,放射性ダッピングの間のフィードバックによって引き起こされます.
- この振動は,南半球中緯度の気候の変動に大きく影響する.
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