海洋模式中中尺度涡参数的物理和生物地球化学综合评估:允许漩涡分辨率下的漩涡诱导平流

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Ocean Modelling Pub Date : 2024-06-08 DOI:10.1016/j.ocemod.2024.102396
X. Ruan , D. Couespel , M. Lévy , J. Li , J. Mak , Y. Wang
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引用次数: 0

摘要

众所周知,允许漩涡机制的海洋总环流模式对中尺度漩涡活动和相关的漩涡-平均值相互作用的分辨率不足。对中尺度涡场的分辨率不足会影响所得到的平均状态,影响模拟的海洋环流和生物地球化学响应,并影响气候预测的质量。关于是否以及如何在涡流允许机制中使用参数化的问题一直存在争论。以基于 Gent-McWilliams(GM)的参数化为重点,我们知道,一方面,不使用参数化会导致涡旋反馈不足并产生偏差。另一方面,使用参数化会导致重复计算涡流反馈,并带来其他偏差。最近提出的一种被称为 "分割 "的方法,改变了基于全球机制的方案在允许涡流情况下的应用方式,并在一个理想化的南大洋航道模型中被证明是有效的。在这项工作中,我们评估了拆分方法能否改善理想化双回旋模式中的物理和生物地球化学响应。与高分辨率中尺度涡解析模型相比,使用基于全球机制的 GEOMETRIC 参数化和在允许涡机制下的分流,在工业化前控制情景和理想化气候变化情景下,比使用和不使用基于全球机制的 GEOMETRIC 参数化的模型都有很大改进。虽然还存在一些不足,特别是在亚热带地区,那里的传输太弱,可能需要动量再注入来减少偏差,但目前的工作提供了进一步的证据,支持在允许涡度分辨率的海洋大气环流模式中使用分裂程序和基于全球机制的参数化。
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Combined physical and biogeochemical assessment of mesoscale eddy parameterisations in ocean models: Eddy-induced advection at eddy-permitting resolutions

Ocean general circulation models at the eddy-permitting regime are known to under-resolve the mesoscale eddy activity and associated eddy-mean interaction. Under-resolving the mesoscale eddy field has consequences for the resulting mean state, affecting the modelled ocean circulation and biogeochemical responses, and impacting the quality of climate projections. There is an ongoing debate on whether and how a parameterisation should be utilised in the eddy-permitting regime. Focusing on the Gent–McWilliams (GM) based parameterisations, it is known that, on the one hand, not utilising a parameterisation leads to insufficient eddy feedback and results in biases. On the other hand, utilising a parameterisation leads to double-counting of the eddy feedback, and introduces other biases. A recently proposed approach, known as splitting, modifies the way GM-based schemes are applied in eddy-permitting regimes, and has been demonstrated to be effective in an idealised Southern Ocean channel model. In this work, we evaluate whether the splitting approach can lead to improvements in the physical and biogeochemical responses in an idealised double gyre model. Compared with a high resolution mesoscale eddy resolving model truth, the use of the GM-based GEOMETRIC parameterisation together with splitting in the eddy-permitting regime leads to broad improvements in the control pre-industrial scenario and an idealised climate change scenario, over models with and models without the GM-based GEOMETRIC parameterisation active. While there are still some deficiencies, particularly in the subtropical region where the transport is too weak and may need momentum re-injection to reduce the biases, the present work provides further evidence in support of using the splitting procedure together with a GM-based parameterisation in ocean general circulation models at eddy-permitting resolutions.

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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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