まとめ
海洋における乱流動的運動エネルギーの消耗は,太陽熱の際に毎日減少した. このエネルギーの消耗は,地元の風力発電から直接抽出されていることが判明しました.
科学分野:
- 海洋学 海洋学 海洋学
- 流体力学 流体力学とは
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 赤道下流は海洋の重要な特徴である.
- 海洋におけるエネルギー分散メカニズムを理解することは,気候モデリングに不可欠です.
研究 の 目的:
- 赤道下流の上の乱流動的運動エネルギー分散の毎日の変動性を調査する.
- エネルギー消耗と地元の風力発電の関係を見極める.
主な方法:
- 12日間にわたる渦巻運動エネルギー消耗の1749のプロフィールを収集しました.
- 海上110メートルからのデータを分析した.
- 計算された日平均値と,特定の深さの範囲における統合分散.
主要な成果:
- 乱流動的運動エネルギーの消耗は,日々の太陽熱の期間中に著しく減少しました.
- 日平均の消耗量は,地元の風力発電と線形的な関係を示した.
- 統合分散 (10-110m) は風力発電の0.92%であり,中緯度の混合層に似ています.
結論:
- 赤道下流の上に散らばるエネルギーの多くは,地元の風力から直接抽出されている可能性が高い.
- 発見は,海洋エネルギー転送プロセスを理解するのに寄与します.
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