The Energetics of Fine-Scale Air–Sea Interactions
微細スケールの大気・海洋相互作用のエネルギー学 (AI 翻訳)
Lionel Renault, Jacob Wenegrat, Hyodae Seo, Patrick Marchesiello
🤖 gxceed AI 要約
日本語
海洋のエネルギー循環は多スケールのシステムであり、惑星規模のエネルギー交換は理解が進んでいるが、メソスケールやサブメソスケールの微細な大気・海洋相互作用は未解明の部分が多い。本レビューは熱フィードバックと流動フィードバックが海洋エネルギー収支に与える影響を整理し、観測プラットフォームや次世代モデルの必要性を提唱する。気候変動予測の精度向上に貢献する基礎研究である。
English
This review synthesizes fine-scale air-sea interaction energetics, focusing on thermal and current feedback mechanisms that affect ocean energy budgets. It highlights gaps in understanding mesoscale and submesoscale processes, including wind-wave effects, and proposes future observational and modeling directions. The paper contributes to improving climate models and predictions.
Unofficial AI-generated summary based on the public title and abstract. Not an official translation.
📝 gxceed 編集解説 — Why this matters
日本のGX文脈において
日本は海洋国家であり、気候変動適応策や水産・海洋資源管理に海洋物理の知見が重要である。本レビューは気候モデルの精度向上に役立ち、日本周辺の海況予測や異常気象の理解を深める基礎となる。ただし、直接的なGX政策や企業実務への応用は限定的。
In the global GX context
Fine-scale air-sea interactions are crucial for understanding climate dynamics and improving global climate models, which underpin climate risk assessments and adaptation planning. This review contributes to the scientific basis for climate projections, relevant for ISSB/TCFD-aligned climate risk disclosure and transition planning.
👥 読者別の含意
🔬研究者:Provides a comprehensive synthesis of current knowledge and research gaps in fine-scale air-sea energetics, useful for orienting future research in physical oceanography and climate modeling.
📄 Abstract（原文）
The Earth's oceanic energy cycle is a multiscale system governed by the complex interactions of oceanic, atmospheric, and wave processes. Significant progress has been made in understanding energy exchange at planetary scales. However, challenges remain at the mesoscale and submesoscale levels. Processes such as mesoscale eddies, submesoscale flows, and internal waves drive intricate energy transfers at these scales. These fine-scale interactions influence the oceanic energy budget through two primary feedback mechanisms: thermal feedback and current feedback. Thermal feedback mainly depletes oceanic potential energy, while current feedback induces a sink of kinetic energy, influencing the kinetic energy pathway. Despite recent advancements, the full impacts of these interactions on the ocean, atmosphere, and climate remain poorly understood. This review synthesizes the current understanding of fine-scale air-sea energetics and their associated effects on the ocean, atmosphere, and climate. It also explores the contributions of submesoscale and high-frequency processes and highlights research gaps. We discuss missing pieces of knowledge, particularly regarding wind-wave effects. Finally, we propose future research directions, emphasizing the need for new observational platforms and next-generation modeling frameworks to capture these interactions and their impact on global climate dynamics.
🔗 Provenance — このレコードを発見したソース
- openalex https://doi.org/10.1146/annurev-marine-040425-024449first seen 2026-07-31 05:12:14
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