Persistent Coastal Temperature Biases in km‐Scale Climate Models Due To Unresolved Oceanic Tidal Mixing

IF 4.6 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Audrey Delpech, Anne‐Marie Tréguier, Louis Marié, Rohit Ghosh, Malcolm J. Roberts
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引用次数: 0

Abstract

Recent advances in numerical modeling have enabled km‐scale climate simulations, improving global climate representation and local‐scale projections, critical to climate adaptation strategies. In this context, the present study assesses the performance of such models over coastal shelf seas—key climate‐sensitive regions—in their ability to represent the sea surface temperature (SST) and air temperature. Compared to satellite and reanalysis data, the models exhibit systematic warm biases (3°C in SST, 1.5°C in air temperature) in summer across several shelf seas: the European shelf, the Gulf of Maine, the Yellow sea, the Arctic and Patagonian shelves. These biases strongly correlate with tidal mixing fronts, driven by the dissipation of the barotropic tide and identified by the Simpson‐Hunter parameter. These findings suggest that missing tidal mixing is a significant error source on coastal shelves, highlighting the need for improved ocean mixing representations to enhance model accuracy.
由于未解决的海洋潮汐混合,千米尺度气候模式中持续的沿海温度偏差
数值模拟的最新进展使千米尺度的气候模拟成为可能,改善了全球气候表征和局部尺度预测,这对气候适应战略至关重要。在此背景下,本研究评估了这些模式在沿海大陆架海洋(关键的气候敏感区域)上的表现,即它们表示海表温度(SST)和空气温度的能力。与卫星和再分析数据相比,该模式显示出夏季在几个大陆架海域(欧洲大陆架、缅因湾、黄海、北极和巴塔哥尼亚大陆架)的系统性暖偏(海温3°C,气温1.5°C)。这些偏置与潮汐混合锋密切相关,由正压潮汐耗散驱动,并由Simpson - Hunter参数确定。这些发现表明,缺少潮汐混合是沿海大陆架的一个重要误差源,突出了改进海洋混合表示以提高模型精度的必要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geophysical Research Letters
Geophysical Research Letters 地学-地球科学综合
CiteScore
9.00
自引率
9.60%
发文量
1588
审稿时长
2.2 months
期刊介绍: Geophysical Research Letters (GRL) publishes high-impact, innovative, and timely research on major scientific advances in all the major geoscience disciplines. Papers are communications-length articles and should have broad and immediate implications in their discipline or across the geosciences. GRLmaintains the fastest turn-around of all high-impact publications in the geosciences and works closely with authors to ensure broad visibility of top papers.
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