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DOI10.1007/s00382-018-4152-0
Influence of air–sea coupling on Indian Ocean tropical cyclones
Lengaigne M.; Neetu S.; Samson G.; Vialard J.; Krishnamohan K.S.; Masson S.; Jullien S.; Suresh I.; Menkes C.E.
发表日期2019
ISSN0930-7575
起始页码577
结束页码598
卷号52期号:2020-01-02
英文摘要This paper assesses the impact of air–sea coupling on Indian Ocean tropical cyclones (TCs) by comparing a 20-year long simulation of a ¼° regional coupled ocean–atmosphere model with a twin experiment, where the atmospheric component is forced by sea surface temperature from the coupled simulation. The coupled simulation reproduces the observed spatio-temporal TCs distribution and TC-induced surface cooling reasonably well, but overestimates the number of TCs. Air–sea coupling does not affect the cyclogenesis spatial distribution but reduces the number of TCs by ~ 20% and yields a better-resolved bimodal seasonal distribution in the northern hemisphere. Coupling also affects intensity distribution, inducing a four-fold decrease in the proportion of intense TCs (Cat-2 and stronger). Air–sea coupling damps TCs growth through a reduction of inner-core upward enthalpy fluxes due to the TC-induced cooling. This reduction is particularly large for the most intense TCs of the northern Indian Ocean (up to 250 W m −2 ), due to higher ambient surface temperatures and larger TC-induced cooling there. The negative feedback of air–sea coupling on strongest TCs is mainly associated with slow-moving storms, which spend more time over the cold wake they induce. Sensitivity experiments using a different convective parameterization yield qualitatively similar results, with a larger (~ 65%) reduction in the number of TCs. Because of their relatively coarse resolution (¼°), both set of experiments however fail to reproduce the most intense observed TCs. Further studies with finer resolution models in the Bay of Bengal will be needed to assess the expectedly large impact of air–sea coupling on those intense and deadly TCs. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature.
英文关键词Air–sea coupling; Cold wake; Indian Ocean; Regional coupled ocean–atmosphere model; Tropical cyclones
语种英语
scopus关键词atmosphere-ocean coupling; atmospheric modeling; cyclogenesis; Northern Hemisphere; parameterization; sea surface temperature; tropical cyclone; wake; Indian Ocean; Indian Ocean (North)
来源期刊Climate Dynamics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/146629
作者单位Sorbonne Universités (UPMC, Univ Paris 06)-CNRS-IRD-MNHN, LOCEAN Laboratory, IPSL, Paris, France; Indo-French Cell for Water Sciences, IISc-NIO-IITM-IRD Joint International Laboratory, National Institute of Oceanography, Dona Paula, Goa, India; CSIR-National Institute of Oceanography, Dona Paula, Goa, India; Mercator Océan, Ramonville-Saint-Agne, France; Laboratoire d’Océanographie Physique et Spatiale (LOPS), Univ. Brest, CNRS, IRD, Ifremer, IUEM, Plouzané, France; Centre IRD, Nouméa, New Caledonia
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GB/T 7714
Lengaigne M.,Neetu S.,Samson G.,等. Influence of air–sea coupling on Indian Ocean tropical cyclones[J],2019,52(2020-01-02).
APA Lengaigne M..,Neetu S..,Samson G..,Vialard J..,Krishnamohan K.S..,...&Menkes C.E..(2019).Influence of air–sea coupling on Indian Ocean tropical cyclones.Climate Dynamics,52(2020-01-02).
MLA Lengaigne M.,et al."Influence of air–sea coupling on Indian Ocean tropical cyclones".Climate Dynamics 52.2020-01-02(2019).
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