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DOI | 10.1029/2019JC015522 |
The Atlantic Meridional Overturning Circulation in High-Resolution Models | |
Hirschi J.J.M.; Barnier B.; Böning C.; Biastoch A.; Blaker A.T.; Coward A.; Danilov S.; Drijfhout S.; Getzlaff K.; Griffies S.M.; Hasumi H.; Hewitt H.; Iovino D.; Kawasaki T.; Kiss A.E.; Koldunov N.; Marzocchi A.; Mecking J.V.; Moat B.; Molines J.-M.; Myers P.G.; Penduff T.; Roberts M.; Treguier A.-M.; Sein D.V.; Sidorenko D.; Small J.; Spence P.; Thompson L.; Weijer W.; Xu X. | |
发表日期 | 2020 |
ISSN | 21699275 |
卷号 | 125期号:4 |
英文摘要 | The Atlantic meridional overturning circulation (AMOC) represents the zonally integrated stream function of meridional volume transport in the Atlantic Basin. The AMOC plays an important role in transporting heat meridionally in the climate system. Observations suggest a heat transport by the AMOC of 1.3 PW at 26°N—a latitude which is close to where the Atlantic northward heat transport is thought to reach its maximum. This shapes the climate of the North Atlantic region as we know it today. In recent years there has been significant progress both in our ability to observe the AMOC in nature and to simulate it in numerical models. Most previous modeling investigations of the AMOC and its impact on climate have relied on models with horizontal resolution that does not resolve ocean mesoscale eddies and the dynamics of the Gulf Stream/North Atlantic Current system. As a result of recent increases in computing power, models are now being run that are able to represent mesoscale ocean dynamics and the circulation features that rely on them. The aim of this review is to describe new insights into the AMOC provided by high-resolution models. Furthermore, we will describe how high-resolution model simulations can help resolve outstanding challenges in our understanding of the AMOC. ©2020. The Authors. |
英文关键词 | Atlantic Meridional Overturning; high-resolution modeling; mesoscale |
语种 | 英语 |
来源期刊 | Journal of Geophysical Research: Oceans
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/186927 |
作者单位 | National Oceanography Centre, Southampton, United Kingdom; Université Grenoble Alpes, CNRS, IRD, Grenoble-INP, IGE, Grenoble, France; Geomar, Kiel, Germany; Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany; University of Southampton, Ocean and Earth Science, Southampton, United Kingdom; Atmosphere & Ocean Sciences Program, NOAA/GFDL + Princeton University, Princeton, NJ, United States; Atmosphere and Ocean Research Institute, The University of Tokyo, Tokyo, Japan; Met Office, Exeter, United Kingdom; Ocean Modeling and Data Assimilation Division, Centro Euro-Mediterraneo sui Cambiamenti Climatici, Italy; Research School of Earth Sciences, Australian National University + ARC Centre of Excellence for Climate Extremes, Canberra, ACT, Australia; Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada; Laboratoire d'océanographie Physique et Spatiale, CNRS, Brest, France; NCAR/UCAR, Boulder, CO, United States; Climate Change Research Centre, Univers... |
推荐引用方式 GB/T 7714 | Hirschi J.J.M.,Barnier B.,Böning C.,et al. The Atlantic Meridional Overturning Circulation in High-Resolution Models[J],2020,125(4). |
APA | Hirschi J.J.M..,Barnier B..,Böning C..,Biastoch A..,Blaker A.T..,...&Xu X..(2020).The Atlantic Meridional Overturning Circulation in High-Resolution Models.Journal of Geophysical Research: Oceans,125(4). |
MLA | Hirschi J.J.M.,et al."The Atlantic Meridional Overturning Circulation in High-Resolution Models".Journal of Geophysical Research: Oceans 125.4(2020). |
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