{"title":"从卫星图像上看，本格拉的横向细丝上涌","authors":"A. G. Kostyanoy, G. Bubnov","doi":"10.1080/07493878.1995.10642003","DOIUrl":null,"url":null,"abstract":"The existence of a system of cold and warm transverse upwelling filaments was established on the basis of an analysis of daily infrared satellite images of the Benguela upwelling (15-32° S) recorded during two sea expeditions during January-February 1986 and April-June 1988 and its principal characteristics were determined. The geographic location of the filaments and their relationship to bottom topography is analyzed. A correlation is established between the spatial temporal variability of the system of cold filaments and the seasonal intensification of the upwelling.","PeriodicalId":175956,"journal":{"name":"Mapping Sciences & Remote Sensing","volume":"18 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1995-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"TRANSVERSE FILAMENTS OF THE BENGUELA UPWELLING FROM SATELLITE IMAGERY\",\"authors\":\"A. G. Kostyanoy, G. Bubnov\",\"doi\":\"10.1080/07493878.1995.10642003\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The existence of a system of cold and warm transverse upwelling filaments was established on the basis of an analysis of daily infrared satellite images of the Benguela upwelling (15-32° S) recorded during two sea expeditions during January-February 1986 and April-June 1988 and its principal characteristics were determined. The geographic location of the filaments and their relationship to bottom topography is analyzed. A correlation is established between the spatial temporal variability of the system of cold filaments and the seasonal intensification of the upwelling.\",\"PeriodicalId\":175956,\"journal\":{\"name\":\"Mapping Sciences & Remote Sensing\",\"volume\":\"18 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1995-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mapping Sciences & Remote Sensing\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/07493878.1995.10642003\",\"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 & Remote Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/07493878.1995.10642003","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
TRANSVERSE FILAMENTS OF THE BENGUELA UPWELLING FROM SATELLITE IMAGERY
The existence of a system of cold and warm transverse upwelling filaments was established on the basis of an analysis of daily infrared satellite images of the Benguela upwelling (15-32° S) recorded during two sea expeditions during January-February 1986 and April-June 1988 and its principal characteristics were determined. The geographic location of the filaments and their relationship to bottom topography is analyzed. A correlation is established between the spatial temporal variability of the system of cold filaments and the seasonal intensification of the upwelling.
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