まとめ
1982年のエルニーニョ-南方振動 (ENSO) イベントの前には,珍しい南風帯が先行した. この大気パターンは,主要なエルニーニョ-南方振動 (ENSO) イベントを誘発するために決定的に重要なようです.
科学分野:
- 大気科学 大気科学
- 海洋学 海洋学とは
- 気候科学 気候科学
背景:
- 1982年のエルニーニョ - 南方振動 (ENSO) イベントは,重要な気候異常でした.
- ENSOイベントの先駆者を理解することは,気候予測に不可欠です.
研究 の 目的:
- 1982年のENSOイベントの開始における異常な南側の地表風の役割を調査する.
- ENSOの大規模なイベントに先立つ同様の風のパターンの歴史的な発生を調査する.
主な方法:
- 1982年6月の地表風データを分析した.
- ENSO年 (1957, 1965, 1972) の歴史的な気象記録との比較.
主要な成果:
- 1982年6月,オーストラリアの東に南側の地表風の明確な帯が形成されました.
- この南向きの流れは,赤道西風が始まる前に赤道を横切った.
- これらの西風は,日付線の東に海洋の大幅な温暖化を開始しました.
結論:
- 異常な南のジェットは,1982年のENSOイベントの活発な段階を触発する重要な大気成分として特定されています.
- 歴史的なデータは,この前駆者のパターンが主要なENSOイベントに共通していることを示唆しています.
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