Effects of ocean eddies on the tropical storm Roanu intensity in the Bay of Bengal
A tropical storm (TS) Roanu occurred in northern Sri Lanka in 2016, which transported northwards along the west coast of the Bay of Bengal (BoB). During the development of the TS, ocean eddies on its track had an important effect on the intensity of Roanu. The dynamic mechanism was investigated with...
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| description | A tropical storm (TS) Roanu occurred in northern Sri Lanka in 2016, which transported northwards along the west coast of the Bay of Bengal (BoB). During the development of the TS, ocean eddies on its track had an important effect on the intensity of Roanu. The dynamic mechanism was investigated with multisource reanalysis and Argo float data in this study. The results show that ocean eddies were the main reason why Roanu first enhanced, weakened, and then enhanced again. Warm eddy W1 supports the initial development of the TS, cold eddy C1 weakens Roanu, and warm eddy W2 continues to support Roanu. On May 19, 2016, the maximum average latent heat flux over W1 was 260.85 w/m2, while that of C1 was only 200.71 w/m2. After the passage of Roanu, the tropical cyclone heat potential (TCHP) of eddies significantly decreased. The TCHP of W1, W2, C1 and C2 decreased by 20.95 kJ/cm2, 11.07 kJ/cm2, 29.82 kJ/cm2, 9.31 kJ/cm2, respectively. The mixed layer of warm eddies deepened much more than that of cold eddies, supporting Roanu development. In addition, changes in potential vorticity (PV) values caused by the disturbance of eddies may also reflect changes in the TS intensity. This study offers new insights on the influence of ocean eddies in regulating the development of tropical cyclone (TC) in the BoB. |
| doi_str_mv | 10.1371/journal.pone.0247521 |
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During the development of the TS, ocean eddies on its track had an important effect on the intensity of Roanu. The dynamic mechanism was investigated with multisource reanalysis and Argo float data in this study. The results show that ocean eddies were the main reason why Roanu first enhanced, weakened, and then enhanced again. Warm eddy W1 supports the initial development of the TS, cold eddy C1 weakens Roanu, and warm eddy W2 continues to support Roanu. On May 19, 2016, the maximum average latent heat flux over W1 was 260.85 w/m2, while that of C1 was only 200.71 w/m2. After the passage of Roanu, the tropical cyclone heat potential (TCHP) of eddies significantly decreased. The TCHP of W1, W2, C1 and C2 decreased by 20.95 kJ/cm2, 11.07 kJ/cm2, 29.82 kJ/cm2, 9.31 kJ/cm2, respectively. The mixed layer of warm eddies deepened much more than that of cold eddies, supporting Roanu development. In addition, changes in potential vorticity (PV) values caused by the disturbance of eddies may also reflect changes in the TS intensity. This study offers new insights on the influence of ocean eddies in regulating the development of tropical cyclone (TC) in the BoB.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0247521</identifier><identifier>PMID: 33667249</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Analysis ; Atmospheric data ; Biotechnology ; Coriolis force ; Cyclones ; Cyclonic vortexes ; Earth Sciences ; Ecology and Environmental Sciences ; Eddies ; Editing ; Environments ; Funding ; Geopotential ; Geopotential height ; Heat ; Laboratories ; Lower troposphere ; Marine resources ; Marine technology ; Methodology ; Middle troposphere ; Ocean ; Ocean circulation ; Oceans ; Physical Sciences ; Remote sensing systems ; Reviews ; Sea level ; Seawater ; Tropical cyclones ; Tropical storms ; Troposphere ; Vertical forces ; Vertical wind shear ; Vortices ; Weather ; Weather forecasting ; Wind ; Wind shear</subject><ispartof>PloS one, 2021-03, Vol.16 (3), p.e0247521-e0247521</ispartof><rights>COPYRIGHT 2021 Public Library of Science</rights><rights>2021 Liu et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2021 Liu et al 2021 Liu et al</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c692t-1249e0230213a5e5fbf0f258ba0516a26f945ac2a70c0541160336b2f7e5c7d33</citedby><cites>FETCH-LOGICAL-c692t-1249e0230213a5e5fbf0f258ba0516a26f945ac2a70c0541160336b2f7e5c7d33</cites><orcidid>0000-0002-0951-1363</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC7935279/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC7935279/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,724,777,781,861,882,2096,2915,23847,27905,27906,53772,53774,79349,79350</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/33667249$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><contributor>Dias, João Miguel</contributor><creatorcontrib>Liu, Yujun</creatorcontrib><creatorcontrib>LÜ, Haibin</creatorcontrib><creatorcontrib>Zhang, Honghua</creatorcontrib><creatorcontrib>Cui, Yusheng</creatorcontrib><creatorcontrib>Xing, Xueting</creatorcontrib><title>Effects of ocean eddies on the tropical storm Roanu intensity in the Bay of Bengal</title><title>PloS one</title><addtitle>PLoS One</addtitle><description>A tropical storm (TS) Roanu occurred in northern Sri Lanka in 2016, which transported northwards along the west coast of the Bay of Bengal (BoB). During the development of the TS, ocean eddies on its track had an important effect on the intensity of Roanu. The dynamic mechanism was investigated with multisource reanalysis and Argo float data in this study. The results show that ocean eddies were the main reason why Roanu first enhanced, weakened, and then enhanced again. Warm eddy W1 supports the initial development of the TS, cold eddy C1 weakens Roanu, and warm eddy W2 continues to support Roanu. On May 19, 2016, the maximum average latent heat flux over W1 was 260.85 w/m2, while that of C1 was only 200.71 w/m2. After the passage of Roanu, the tropical cyclone heat potential (TCHP) of eddies significantly decreased. The TCHP of W1, W2, C1 and C2 decreased by 20.95 kJ/cm2, 11.07 kJ/cm2, 29.82 kJ/cm2, 9.31 kJ/cm2, respectively. The mixed layer of warm eddies deepened much more than that of cold eddies, supporting Roanu development. In addition, changes in potential vorticity (PV) values caused by the disturbance of eddies may also reflect changes in the TS intensity. This study offers new insights on the influence of ocean eddies in regulating the development of tropical cyclone (TC) in the BoB.</description><subject>Analysis</subject><subject>Atmospheric data</subject><subject>Biotechnology</subject><subject>Coriolis force</subject><subject>Cyclones</subject><subject>Cyclonic vortexes</subject><subject>Earth Sciences</subject><subject>Ecology and Environmental Sciences</subject><subject>Eddies</subject><subject>Editing</subject><subject>Environments</subject><subject>Funding</subject><subject>Geopotential</subject><subject>Geopotential height</subject><subject>Heat</subject><subject>Laboratories</subject><subject>Lower troposphere</subject><subject>Marine resources</subject><subject>Marine technology</subject><subject>Methodology</subject><subject>Middle troposphere</subject><subject>Ocean</subject><subject>Ocean circulation</subject><subject>Oceans</subject><subject>Physical Sciences</subject><subject>Remote sensing 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One</addtitle><date>2021-03-05</date><risdate>2021</risdate><volume>16</volume><issue>3</issue><spage>e0247521</spage><epage>e0247521</epage><pages>e0247521-e0247521</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>A tropical storm (TS) Roanu occurred in northern Sri Lanka in 2016, which transported northwards along the west coast of the Bay of Bengal (BoB). During the development of the TS, ocean eddies on its track had an important effect on the intensity of Roanu. The dynamic mechanism was investigated with multisource reanalysis and Argo float data in this study. The results show that ocean eddies were the main reason why Roanu first enhanced, weakened, and then enhanced again. Warm eddy W1 supports the initial development of the TS, cold eddy C1 weakens Roanu, and warm eddy W2 continues to support Roanu. On May 19, 2016, the maximum average latent heat flux over W1 was 260.85 w/m2, while that of C1 was only 200.71 w/m2. After the passage of Roanu, the tropical cyclone heat potential (TCHP) of eddies significantly decreased. The TCHP of W1, W2, C1 and C2 decreased by 20.95 kJ/cm2, 11.07 kJ/cm2, 29.82 kJ/cm2, 9.31 kJ/cm2, respectively. The mixed layer of warm eddies deepened much more than that of cold eddies, supporting Roanu development. In addition, changes in potential vorticity (PV) values caused by the disturbance of eddies may also reflect changes in the TS intensity. This study offers new insights on the influence of ocean eddies in regulating the development of tropical cyclone (TC) in the BoB.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>33667249</pmid><doi>10.1371/journal.pone.0247521</doi><tpages>e0247521</tpages><orcidid>https://orcid.org/0000-0002-0951-1363</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | Analysis Atmospheric data Biotechnology Coriolis force Cyclones Cyclonic vortexes Earth Sciences Ecology and Environmental Sciences Eddies Editing Environments Funding Geopotential Geopotential height Heat Laboratories Lower troposphere Marine resources Marine technology Methodology Middle troposphere Ocean Ocean circulation Oceans Physical Sciences Remote sensing systems Reviews Sea level Seawater Tropical cyclones Tropical storms Troposphere Vertical forces Vertical wind shear Vortices Weather Weather forecasting Wind Wind shear |
| title | Effects of ocean eddies on the tropical storm Roanu intensity in the Bay of Bengal |
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