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DOI | 10.1029/2018MS001544 |
Connecting Direct Effects of CO2 Radiative Forcing to Ocean Heat Uptake and Circulation | |
Menzel M.E.; Merlis T.M. | |
发表日期 | 2019 |
ISSN | 19422466 |
起始页码 | 2163 |
结束页码 | 2176 |
卷号 | 11期号:7 |
英文摘要 | The ocean's response to direct atmospheric effects of increased carbon dioxide's (CO2) radiative forcing is examined. These direct effects are defined as the climate changes that result from forcing on a fast time scale of about a year, independent of the slower surface warming that the forcing also provokes. To evaluate how these direct effects impact ocean heat uptake and circulation, output of atmospheric general circulation model (GCM) simulations are used to force an ocean GCM with comprehensive boundary conditions. Perturbation simulations with the prescribed response to a quadrupling of atmospheric CO2 include altered surface winds, freshwater fluxes, downwelling shortwave radiation, and downwelling longwave cloud radiative effect. The perturbation simulations show that the intensification and poleward shift of surface winds, particularly in the Southern Ocean, strengthen the shallow overturning circulation in the tropical Pacific and deep overturning in the Atlantic. This, in turn, has a cooling effect on the global ocean at shallow depths. A two-layer energy balance model, designed to capture transient global mean climate change, is adapted to account for the altered ocean heat uptake from direct effects. The direct change in global mean ocean heat uptake is a decrease of about 0.3 W/m2 for quadrupling of CO2, offsetting about 5% of the surface longwave forcing. © 2019. The Authors. |
语种 | 英语 |
scopus关键词 | Atmospheric radiation; Carbon dioxide; Climate models; Oceanography; Atmospheric effects; Atmospheric general circulation models; Cloud radiative effects; Energy balance models; Ocean heat uptake; Overturning circulation; Radiative forcings; Short-wave radiation; Climate change; atmosphere-ocean coupling; atmospheric general circulation model; carbon dioxide; climate change; climate forcing; global warming; heat transfer; ocean; oceanic circulation; perturbation; radiative forcing; timescale |
来源期刊 | Journal of Advances in Modeling Earth Systems |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/156964 |
作者单位 | Department of Atmospheric and Oceanic Sciences, McGill University, Montreal, QC, Canada; Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, MD, United States |
推荐引用方式 GB/T 7714 | Menzel M.E.,Merlis T.M.. Connecting Direct Effects of CO2 Radiative Forcing to Ocean Heat Uptake and Circulation[J],2019,11(7). |
APA | Menzel M.E.,&Merlis T.M..(2019).Connecting Direct Effects of CO2 Radiative Forcing to Ocean Heat Uptake and Circulation.Journal of Advances in Modeling Earth Systems,11(7). |
MLA | Menzel M.E.,et al."Connecting Direct Effects of CO2 Radiative Forcing to Ocean Heat Uptake and Circulation".Journal of Advances in Modeling Earth Systems 11.7(2019). |
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