{"title":"利用卫星图像监测海洋表面温度的亚北极锋","authors":"V. V. Devitsyn, A. Kovalev, G. Vanyushin","doi":"10.1080/07493878.2001.10642160","DOIUrl":null,"url":null,"abstract":"Surface temperature gradients, used in identifying the principal hydrological fronts of the southwestern Atlantic Ocean, were computed from charts of ocean surface temperature plotted with the use of satellite information for the period 1988–1997. An analysis is made of the seasonal variability of ocean temperature gradients in the frontal zone, as well as changes in its geographical position. The year-to-year variability of the position of the Subantarctic Front is examined.","PeriodicalId":405012,"journal":{"name":"Mapping Sciences and Remote Sensing","volume":"15 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2001-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"MONITORING THE SUBARCTIC FRONT IN OCEAN SURFACE TEMPERATURE USING SATELLITE IMAGERY\",\"authors\":\"V. V. Devitsyn, A. Kovalev, G. Vanyushin\",\"doi\":\"10.1080/07493878.2001.10642160\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Surface temperature gradients, used in identifying the principal hydrological fronts of the southwestern Atlantic Ocean, were computed from charts of ocean surface temperature plotted with the use of satellite information for the period 1988–1997. An analysis is made of the seasonal variability of ocean temperature gradients in the frontal zone, as well as changes in its geographical position. The year-to-year variability of the position of the Subantarctic Front is examined.\",\"PeriodicalId\":405012,\"journal\":{\"name\":\"Mapping Sciences and Remote Sensing\",\"volume\":\"15 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mapping Sciences and Remote Sensing\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/07493878.2001.10642160\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mapping Sciences and Remote Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/07493878.2001.10642160","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
MONITORING THE SUBARCTIC FRONT IN OCEAN SURFACE TEMPERATURE USING SATELLITE IMAGERY
Surface temperature gradients, used in identifying the principal hydrological fronts of the southwestern Atlantic Ocean, were computed from charts of ocean surface temperature plotted with the use of satellite information for the period 1988–1997. An analysis is made of the seasonal variability of ocean temperature gradients in the frontal zone, as well as changes in its geographical position. The year-to-year variability of the position of the Subantarctic Front is examined.
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