Response of ocean climate to different heat-flux perturbations over the North Atlantic in FAFMIP

IF 6.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Wen-Yu Yin , Xin Gao , Run Guo , Peng Fan , Guang-Qing Zhou
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Abstract

The diversity of surface-flux perturbations, especially for heat-flux perturbations, notably leads to uncertainties surrounding the responses of ocean climate under global warming scenarios projected by climate/Earth system models. However, when imposing heat-flux perturbations on the models, strong feedback persists between the atmosphere and the ocean, resulting in nearly doubled heat-flux perturbation over the North Atlantic (NA). Herein, quantitative evaluation of the influences of magnitude change of heat-flux perturbations over the NA on the changes in the Atlantic Meridional Overturning Circulation (AMOC), ocean heat uptake (OHU) and dynamic sea level (DSL) has been conducted by analysis of eight coupled model responses to the heat-flux perturbation experiments in the Flux-Anomaly-Forced Model Inter-comparison Project. It has been demonstrated that the magnitude of the AMOC change is extremely sensitive to the magnitude change of imposed NA heat-flux perturbation, and the weakening amplitude of the AMOC is nearly halved as the imposed heat-flux perturbation F is halved over the NA. The most remarkable responses of both DSL and OHU to the magnitude changes of NA heat-flux perturbation have been primarily found in the Atlantic and Arctic basins, especially for the NA region. Both the added ocean heat uptake (OHUa) and redistributed ocean heat uptake (OHUr) play key roles in OHU changes among the various NA heat-flux perturbation experiments. The magnitude change of NA-mean OHUa is almost linearly related to the imposed NA heat-flux perturbation, while the magnitude change of NA-mean OHUr, which is primarily caused by AMOC change and redistributed heat flux, is not proportional to the imposed NA heat-flux perturbation. There is a nearly linear relationship between the magnitude of AMOC change and the OHUr in tropical regions, including the regions in the low-latitude South Atlantic, the tropical Pacific Ocean and the Indian Ocean.

FAFMIP中北大西洋海洋气候对不同热通量扰动的响应
表面通量扰动的多样性,特别是热通量扰动,显著地导致了气候/地球系统模型预测的全球变暖情景下海洋气候响应的不确定性。然而,当对模型施加热通量扰动时,大气和海洋之间的强烈反馈持续存在,导致北大西洋上空的热通量扰动几乎翻了一番。本文定量评价了NA上空热通量扰动幅度变化对大西洋经向翻转环流(AMOC)变化的影响,通过对通量异常强迫模型相互比较项目中热通量扰动实验的八个耦合模型响应的分析,对海洋热吸收(OHU)和动态海平面(DSL)进行了研究。已经证明,AMOC变化的幅度对施加的NA热通量扰动的幅度变化非常敏感,并且随着施加的热通量扰动F在NA上减半,AMOC的减弱幅度几乎减半。DSL和OHU对NA热通量扰动幅度变化的最显著响应主要出现在大西洋和北极盆地,尤其是在NA地区。在各种NA热通量扰动实验中,增加的海洋热量吸收(OHUa)和重新分配的海洋热量摄入(OHUr)在OHU变化中起着关键作用。NA平均OHUa的幅度变化与施加的NA热通量扰动几乎线性相关,而NA平均OHUr的幅度变化(主要由AMOC变化和重新分布的热通量引起)与施加的NA热通量扰动不成比例。在热带地区,包括低纬度南大西洋、热带太平洋和印度洋地区,AMOC变化幅度与OHUr之间几乎呈线性关系。
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来源期刊
Advances in Climate Change Research
Advances in Climate Change Research Earth and Planetary Sciences-Atmospheric Science
CiteScore
9.80
自引率
4.10%
发文量
424
审稿时长
107 days
期刊介绍: Advances in Climate Change Research publishes scientific research and analyses on climate change and the interactions of climate change with society. This journal encompasses basic science and economic, social, and policy research, including studies on mitigation and adaptation to climate change. Advances in Climate Change Research attempts to promote research in climate change and provide an impetus for the application of research achievements in numerous aspects, such as socioeconomic sustainable development, responses to the adaptation and mitigation of climate change, diplomatic negotiations of climate and environment policies, and the protection and exploitation of natural resources.
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