{"title":"2007-2009年东海浙江沿岸上升流的卫星观测","authors":"X. Lou, A. Shi, Q. Xiao, Huaguo Zhang","doi":"10.1117/12.898140","DOIUrl":null,"url":null,"abstract":"In this article, EOS MODIS sea surface temperature (SST) data are used to observe the Zhejiang Coastal Upwelling in the East China Sea. MODIS SST data in summer from 2007 to 2009 are selected and processed. Based on the upwelling's temperature features in SST imagery, a temperature threshold approach is established to measure the physical parameters of the upwelling. And then the temporal and spatial characteristics of the upwelling are analyzed. Results show that the upwelling distributes along the Zhejiang Coast running from south to northeast, and covers an average area of 11,000 square kilometers. The mean temperature of the upwelling is about 25~28°C, and its temperature difference from surrounding non-upwelling waters is in the ranges of 2~4°C. The upwelling appears in June and develops to its strongest period in July and August, and then it weakens and vanishes in late September. Three years of observational results reveal that the upwelling has short-time, seasonal and interannual variances. The upwelling is also closely related to the coastal topography.","PeriodicalId":48993,"journal":{"name":"Remote Sensing","volume":"33 1","pages":""},"PeriodicalIF":4.1000,"publicationDate":"2011-10-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"15","resultStr":"{\"title\":\"Satellite observation of the Zhejiang Coastal upwelling in the East China Sea during 2007-2009\",\"authors\":\"X. Lou, A. Shi, Q. Xiao, Huaguo Zhang\",\"doi\":\"10.1117/12.898140\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In this article, EOS MODIS sea surface temperature (SST) data are used to observe the Zhejiang Coastal Upwelling in the East China Sea. MODIS SST data in summer from 2007 to 2009 are selected and processed. Based on the upwelling's temperature features in SST imagery, a temperature threshold approach is established to measure the physical parameters of the upwelling. And then the temporal and spatial characteristics of the upwelling are analyzed. Results show that the upwelling distributes along the Zhejiang Coast running from south to northeast, and covers an average area of 11,000 square kilometers. The mean temperature of the upwelling is about 25~28°C, and its temperature difference from surrounding non-upwelling waters is in the ranges of 2~4°C. The upwelling appears in June and develops to its strongest period in July and August, and then it weakens and vanishes in late September. Three years of observational results reveal that the upwelling has short-time, seasonal and interannual variances. The upwelling is also closely related to the coastal topography.\",\"PeriodicalId\":48993,\"journal\":{\"name\":\"Remote Sensing\",\"volume\":\"33 1\",\"pages\":\"\"},\"PeriodicalIF\":4.1000,\"publicationDate\":\"2011-10-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"15\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Remote Sensing\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://doi.org/10.1117/12.898140\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Remote Sensing","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1117/12.898140","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Satellite observation of the Zhejiang Coastal upwelling in the East China Sea during 2007-2009
In this article, EOS MODIS sea surface temperature (SST) data are used to observe the Zhejiang Coastal Upwelling in the East China Sea. MODIS SST data in summer from 2007 to 2009 are selected and processed. Based on the upwelling's temperature features in SST imagery, a temperature threshold approach is established to measure the physical parameters of the upwelling. And then the temporal and spatial characteristics of the upwelling are analyzed. Results show that the upwelling distributes along the Zhejiang Coast running from south to northeast, and covers an average area of 11,000 square kilometers. The mean temperature of the upwelling is about 25~28°C, and its temperature difference from surrounding non-upwelling waters is in the ranges of 2~4°C. The upwelling appears in June and develops to its strongest period in July and August, and then it weakens and vanishes in late September. Three years of observational results reveal that the upwelling has short-time, seasonal and interannual variances. The upwelling is also closely related to the coastal topography.
期刊介绍:
Remote Sensing (ISSN 2072-4292) publishes regular research papers, reviews, letters and communications covering all aspects of the remote sensing process, from instrument design and signal processing to the retrieval of geophysical parameters and their application in geosciences. Our aim is to encourage scientists to publish experimental, theoretical and computational results in as much detail as possible so that results can be easily reproduced. There is no restriction on the length of the papers. The full experimental details must be provided so that the results can be reproduced.