海洋の混合に利用できるエネルギーの再分配は,内部波の長距離伝播によって行われます
1Applied Physics Laboratory and School of Oceanography, University of Washington, 1013 NE 40th Street, Seattle, Washington 98105, USA. malford@apl.washington.edu
Nature
|May 9, 2003
まとめ
内部重力波は海洋の混合を促し,気候と海洋生態系に影響を与えます. この研究は,それらの伝播をマッピングし,年間を通して地球全体の混合パターンに影響を与えるエネルギーフローを明らかにします.
科学分野:
- 海洋学 海洋学とは
- 流体力学 流体力学
- 気候科学 気候科学
背景:
- 海洋の混合は,汚染物質の分散,海洋の生産性,そして地球規模の気候規制にとって極めて重要です.
- 海洋層分化に沿って広がる内部重力波は,海洋の混合の主要な原動力である.
- 気候モデルを改善するために,内部波散乱のグローバルマップが必要です.
研究 の 目的:
- 歴史的なモアリングデータから水平の内部波の伝播を計算する.
- 内部波の伝播を,そのエネルギー源の条件と関連付けること.
- グローバルな混合のために利用可能なエネルギーの時空分布を理解するために.
主な方法:
- 60の歴史的なモアリングからのデータを活用して,水平の内部波の拡散を計算した.
- 分析されたエネルギー周波数範囲は,近慣性および半日間の潮周波数です.
- これらの内部波に関連した量化されたエネルギーフロー.
主要な成果:
- 近慣性帯と半日間の潮帯の両方のエネルギーフローは,約1kW×m−1です.
- これらの流れは,エネルギー投入総量の15~50%を占め,エネルギー源地域から遠ざかっています.
- 近惰性波のエネルギー流は冬にはより強く,潮流は年中一貫している.
結論:
- 内部重力波は,海洋における混合エネルギーの空間的および時間的な分布を大きく影響する.
- 近惰性および潮波の伝播を理解することは,海洋の混合とその気候への影響を予測する鍵です.
- この発見は,気候モデルを改良し,海洋の動態を理解するために不可欠なデータを提供します.
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