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DOI | 10.1175/JCLI-D-20-0069.1 |
On the role of the Antarctic slope front on the occurrence of the weddell sea polynya under climate change | |
Lockwood J.W.; Dufour C.O.; Griffies S.M.; Winton M. | |
发表日期 | 2021 |
ISSN | 08948755 |
起始页码 | 2529 |
结束页码 | 2548 |
卷号 | 34期号:7 |
英文摘要 | This study investigates the occurrence of the Weddell Sea polynya under an idealized climate change scenario by evaluating simulations from climate models of different ocean resolutions. The GFDL-CM2.6 climate model, with roughly 3.8-km horizontal ocean grid spacing in the high latitudes, forms a Weddell Sea polynya at similar time and duration under idealized climate change forcing as under preindustrial forcing. In contrast, all convective models forming phase 5 of the Coupled Model Intercomparison Project (CMIP5) show either a cessation or a slowdown of Weddell Sea polynya events under climate warming. The representation of the Antarctic Slope Current and related Antarctic Slope Front is found to be key in explaining the differences between the two categories of models, with these features being more realistic in CM2.6 than in CMIP5. In CM2.6, the freshwater input driven by sea ice melt and enhanced runoff found under climate warming largely remains on the shelf region since the slope front restricts the lateral spread of the freshwater. In contrast, for most CMIP5 models, open-ocean stratification is enhanced by freshening since the absence of a slope front allows coastal freshwater anomalies to spread into the open ocean. This enhanced freshening contributes to the slowdown the occurrence of Weddell Sea polynyas. Hence, an improved representation of Weddell Sea shelf processes in current climate models is desirable to increase our ability to predict the fate of the Weddell Sea polynyas under climate change. © 2021 American Meteorological Society. |
英文关键词 | Boundary currents; Climate models; Deep convection; Sea ice; Southern Ocean |
语种 | 英语 |
scopus关键词 | Climate models; Oceanography; Sea ice; Water; Climate change scenarios; Climate warming; Coupled Model Intercomparison Project; Freshwater inputs; High Latitudes; Lateral spread; Pre-industrial; Slope currents; Climate change; boundary current; climate change; climate modeling; CMIP; oceanic convection; prediction; scenario analysis; sea ice; Southern Ocean; Weddell Sea |
来源期刊 | Journal of Climate
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/178597 |
作者单位 | Department of Atmospheric and Oceanic Science, McGill University, Montreal, QC, Canada; National Oceanic and Atmospheric Administration, Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States; Atmospheric and Oceanic Sciences Program, Princeton University, Princeton, NJ, United States |
推荐引用方式 GB/T 7714 | Lockwood J.W.,Dufour C.O.,Griffies S.M.,et al. On the role of the Antarctic slope front on the occurrence of the weddell sea polynya under climate change[J],2021,34(7). |
APA | Lockwood J.W.,Dufour C.O.,Griffies S.M.,&Winton M..(2021).On the role of the Antarctic slope front on the occurrence of the weddell sea polynya under climate change.Journal of Climate,34(7). |
MLA | Lockwood J.W.,et al."On the role of the Antarctic slope front on the occurrence of the weddell sea polynya under climate change".Journal of Climate 34.7(2021). |
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