Response of the upper ocean to tropical cyclone in the Northwest Pacific observed by gliders during fall 2018
The evolution of thermohaline structure at the upper ocean during three tropical cyclones (TCs) in the Northwest Pacific was studied in this study based on successive observation by two new-style underwater gliders during fall 2018. These remote-controllable gliders with CTD sensor enabled us to exp...
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| Veröffentlicht in: | Acta oceanologica Sinica 2021, Vol.40 (1), p.103-112 |
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| creator | Ni, Zekai Yu, Jiancheng Shang, Xuekun Jin, Wenming Luo, Yeteng Vetter, Philip A. Jiang, Huichang Yu, Liu Liu, Sumin Xu, Hongzhou |
| description | The evolution of thermohaline structure at the upper ocean during three tropical cyclones (TCs) in the Northwest Pacific was studied in this study based on successive observation by two new-style underwater gliders during fall 2018. These remote-controllable gliders with CTD sensor enabled us to explore high frequency responses of temperature, salinity, mixed and barrier layers in the upper ocean to severe TCs in this area. Results showed that three significant cooling-to-warming and stratification destructing-to-reconstructing processes at the mixed layer occurred during the lives of three TCs. The maximal cooling of SST all reached ⩾=0.5°C although TCs with different intensities had different minimal distances to the observed area. Under potential impacts of solar radiation, tide and inertial motions, the mixed layer depth possessed significant high-frequency fluctuations during TC periods. In addition, barrier layers appeared and vanished quickly during TCs, accompanied with varied temperature inversion processes. |
| doi_str_mv | 10.1007/s13131-020-1672-3 |
| format | Article |
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These remote-controllable gliders with CTD sensor enabled us to explore high frequency responses of temperature, salinity, mixed and barrier layers in the upper ocean to severe TCs in this area. Results showed that three significant cooling-to-warming and stratification destructing-to-reconstructing processes at the mixed layer occurred during the lives of three TCs. The maximal cooling of SST all reached ⩾=0.5°C although TCs with different intensities had different minimal distances to the observed area. Under potential impacts of solar radiation, tide and inertial motions, the mixed layer depth possessed significant high-frequency fluctuations during TC periods. In addition, barrier layers appeared and vanished quickly during TCs, accompanied with varied temperature inversion processes.</description><identifier>ISSN: 0253-505X</identifier><identifier>EISSN: 1869-1099</identifier><identifier>DOI: 10.1007/s13131-020-1672-3</identifier><language>eng</language><publisher>Beijing: The Chinese Society of Oceanography</publisher><subject>Barrier layers ; Climatology ; Controllability ; Cooling ; Cyclones ; Datasets ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Engineering Fluid Dynamics ; Environmental Chemistry ; Gliders ; Heat ; High frequency ; Hurricanes ; Inertia ; Marine & Freshwater Sciences ; Mixed layer ; Mixed layer depth ; Ocean circulation ; Oceanography ; Oceans ; Precipitation ; Remote observing ; Remote sensors ; Sea surface ; Sea surface temperature ; Solar radiation ; Stratification ; Temperature inversion ; Temperature inversions ; Thermohaline structure ; Tropical climate ; Tropical cyclones ; Underwater gliders ; Underwater vehicles ; Upper ocean ; Weather ; Wind</subject><ispartof>Acta oceanologica Sinica, 2021, Vol.40 (1), p.103-112</ispartof><rights>Chinese Society for Oceanography and Springer-Verlag GmbH Germany, part of Springer Nature 2021</rights><rights>Chinese Society for Oceanography and Springer-Verlag GmbH Germany, part of Springer Nature 2021.</rights><rights>Copyright © Wanfang Data Co. 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All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c376t-63ca994d9d13d512baa6e99e47d5c28129bb00c348fd290ba61a1525340457f33</citedby><cites>FETCH-LOGICAL-c376t-63ca994d9d13d512baa6e99e47d5c28129bb00c348fd290ba61a1525340457f33</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/hyxb-e/hyxb-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13131-020-1672-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2919691778?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,780,784,4024,21388,27923,27924,27925,33744,41488,42557,43805,51319,64385,64389,72469</link.rule.ids></links><search><creatorcontrib>Ni, Zekai</creatorcontrib><creatorcontrib>Yu, Jiancheng</creatorcontrib><creatorcontrib>Shang, Xuekun</creatorcontrib><creatorcontrib>Jin, Wenming</creatorcontrib><creatorcontrib>Luo, Yeteng</creatorcontrib><creatorcontrib>Vetter, Philip A.</creatorcontrib><creatorcontrib>Jiang, Huichang</creatorcontrib><creatorcontrib>Yu, Liu</creatorcontrib><creatorcontrib>Liu, Sumin</creatorcontrib><creatorcontrib>Xu, Hongzhou</creatorcontrib><title>Response of the upper ocean to tropical cyclone in the Northwest Pacific observed by gliders during fall 2018</title><title>Acta oceanologica Sinica</title><addtitle>Acta Oceanol. Sin</addtitle><description>The evolution of thermohaline structure at the upper ocean during three tropical cyclones (TCs) in the Northwest Pacific was studied in this study based on successive observation by two new-style underwater gliders during fall 2018. These remote-controllable gliders with CTD sensor enabled us to explore high frequency responses of temperature, salinity, mixed and barrier layers in the upper ocean to severe TCs in this area. Results showed that three significant cooling-to-warming and stratification destructing-to-reconstructing processes at the mixed layer occurred during the lives of three TCs. The maximal cooling of SST all reached ⩾=0.5°C although TCs with different intensities had different minimal distances to the observed area. Under potential impacts of solar radiation, tide and inertial motions, the mixed layer depth possessed significant high-frequency fluctuations during TC periods. In addition, barrier layers appeared and vanished quickly during TCs, accompanied with varied temperature inversion processes.</description><subject>Barrier layers</subject><subject>Climatology</subject><subject>Controllability</subject><subject>Cooling</subject><subject>Cyclones</subject><subject>Datasets</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Engineering Fluid Dynamics</subject><subject>Environmental Chemistry</subject><subject>Gliders</subject><subject>Heat</subject><subject>High frequency</subject><subject>Hurricanes</subject><subject>Inertia</subject><subject>Marine & Freshwater Sciences</subject><subject>Mixed layer</subject><subject>Mixed layer depth</subject><subject>Ocean circulation</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Precipitation</subject><subject>Remote observing</subject><subject>Remote sensors</subject><subject>Sea surface</subject><subject>Sea surface temperature</subject><subject>Solar radiation</subject><subject>Stratification</subject><subject>Temperature inversion</subject><subject>Temperature inversions</subject><subject>Thermohaline structure</subject><subject>Tropical climate</subject><subject>Tropical cyclones</subject><subject>Underwater gliders</subject><subject>Underwater vehicles</subject><subject>Upper 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Northwest Pacific observed by gliders during fall 2018</title><author>Ni, Zekai ; Yu, Jiancheng ; Shang, Xuekun ; Jin, Wenming ; Luo, Yeteng ; Vetter, Philip A. ; Jiang, Huichang ; Yu, Liu ; Liu, Sumin ; Xu, Hongzhou</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c376t-63ca994d9d13d512baa6e99e47d5c28129bb00c348fd290ba61a1525340457f33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Barrier layers</topic><topic>Climatology</topic><topic>Controllability</topic><topic>Cooling</topic><topic>Cyclones</topic><topic>Datasets</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Engineering Fluid Dynamics</topic><topic>Environmental Chemistry</topic><topic>Gliders</topic><topic>Heat</topic><topic>High frequency</topic><topic>Hurricanes</topic><topic>Inertia</topic><topic>Marine & Freshwater Sciences</topic><topic>Mixed 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(COJ)</collection><jtitle>Acta oceanologica Sinica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ni, Zekai</au><au>Yu, Jiancheng</au><au>Shang, Xuekun</au><au>Jin, Wenming</au><au>Luo, Yeteng</au><au>Vetter, Philip A.</au><au>Jiang, Huichang</au><au>Yu, Liu</au><au>Liu, Sumin</au><au>Xu, Hongzhou</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Response of the upper ocean to tropical cyclone in the Northwest Pacific observed by gliders during fall 2018</atitle><jtitle>Acta oceanologica Sinica</jtitle><stitle>Acta Oceanol. Sin</stitle><date>2021</date><risdate>2021</risdate><volume>40</volume><issue>1</issue><spage>103</spage><epage>112</epage><pages>103-112</pages><issn>0253-505X</issn><eissn>1869-1099</eissn><abstract>The evolution of thermohaline structure at the upper ocean during three tropical cyclones (TCs) in the Northwest Pacific was studied in this study based on successive observation by two new-style underwater gliders during fall 2018. These remote-controllable gliders with CTD sensor enabled us to explore high frequency responses of temperature, salinity, mixed and barrier layers in the upper ocean to severe TCs in this area. Results showed that three significant cooling-to-warming and stratification destructing-to-reconstructing processes at the mixed layer occurred during the lives of three TCs. The maximal cooling of SST all reached ⩾=0.5°C although TCs with different intensities had different minimal distances to the observed area. Under potential impacts of solar radiation, tide and inertial motions, the mixed layer depth possessed significant high-frequency fluctuations during TC periods. In addition, barrier layers appeared and vanished quickly during TCs, accompanied with varied temperature inversion processes.</abstract><cop>Beijing</cop><pub>The Chinese Society of Oceanography</pub><doi>10.1007/s13131-020-1672-3</doi><tpages>10</tpages></addata></record> |
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| subjects | Barrier layers Climatology Controllability Cooling Cyclones Datasets Earth and Environmental Science Earth Sciences Ecology Engineering Fluid Dynamics Environmental Chemistry Gliders Heat High frequency Hurricanes Inertia Marine & Freshwater Sciences Mixed layer Mixed layer depth Ocean circulation Oceanography Oceans Precipitation Remote observing Remote sensors Sea surface Sea surface temperature Solar radiation Stratification Temperature inversion Temperature inversions Thermohaline structure Tropical climate Tropical cyclones Underwater gliders Underwater vehicles Upper ocean Weather Wind |
| title | Response of the upper ocean to tropical cyclone in the Northwest Pacific observed by gliders during fall 2018 |
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