{"title":"迈阿密附近佛罗里达海流稳态横流分量的模式","authors":"Frank Chew","doi":"10.1016/0146-6313(61)90024-7","DOIUrl":null,"url":null,"abstract":"<div><p>The pattern of the steady state, transverse current component in the surface layer of the Florida Current off Miami is described on the basis of two independent sets of data. The first consists of over 500 GEK observations obtained over an 8 year period and the second of over 1100 observations selected from <span>Pillsbury's</span> measurements. There is a westward component along the western edge of the Current and an eastward one across the remainder. The maximum magnitude is about 10 cm/s. Discussions of the methods of data selection, reduction, and errors are included.</p></div>","PeriodicalId":100361,"journal":{"name":"Deep Sea Research (1953)","volume":"8 3","pages":"Pages 236-244"},"PeriodicalIF":0.0000,"publicationDate":"1961-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0146-6313(61)90024-7","citationCount":"1","resultStr":"{\"title\":\"The pattern of the steady state transverse current component in the Florida Current off Miami\",\"authors\":\"Frank Chew\",\"doi\":\"10.1016/0146-6313(61)90024-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The pattern of the steady state, transverse current component in the surface layer of the Florida Current off Miami is described on the basis of two independent sets of data. The first consists of over 500 GEK observations obtained over an 8 year period and the second of over 1100 observations selected from <span>Pillsbury's</span> measurements. There is a westward component along the western edge of the Current and an eastward one across the remainder. The maximum magnitude is about 10 cm/s. Discussions of the methods of data selection, reduction, and errors are included.</p></div>\",\"PeriodicalId\":100361,\"journal\":{\"name\":\"Deep Sea Research (1953)\",\"volume\":\"8 3\",\"pages\":\"Pages 236-244\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1961-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0146-6313(61)90024-7\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep Sea Research (1953)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0146631361900247\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep Sea Research (1953)","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0146631361900247","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The pattern of the steady state transverse current component in the Florida Current off Miami
The pattern of the steady state, transverse current component in the surface layer of the Florida Current off Miami is described on the basis of two independent sets of data. The first consists of over 500 GEK observations obtained over an 8 year period and the second of over 1100 observations selected from Pillsbury's measurements. There is a westward component along the western edge of the Current and an eastward one across the remainder. The maximum magnitude is about 10 cm/s. Discussions of the methods of data selection, reduction, and errors are included.
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
