{"title":"Some effects of lateral shifts of the Gulf Stream on the circulation northeast of Cape Hatteras","authors":"Charles E. Parker","doi":"10.1016/0011-7471(76)90847-0","DOIUrl":null,"url":null,"abstract":"<div><p>Data obtained from the U.S. Coast Guard Environmental Buoy EBO-1 for the period of January 1971 to June 1972 are analyzed. The buoy, off the Virginia capes at approximately 36°30′N and 73°30′W, radioed hourly meteorological and oceanographic data to a shore station. Identification of water types at the buoy has been made by comparing the transmitted data with temperature-salinity diagrams. Concurrent observations of lateral shifts in the position of the Gulf Stream show a close correlation with changes in the amount, direction, and temperature-salinity characteristics of the flow at the buoy.</p></div>","PeriodicalId":11253,"journal":{"name":"Deep Sea Research and Oceanographic Abstracts","volume":"23 9","pages":"Pages 795-803"},"PeriodicalIF":0.0000,"publicationDate":"1976-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0011-7471(76)90847-0","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Deep Sea Research and Oceanographic Abstracts","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0011747176908470","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
Data obtained from the U.S. Coast Guard Environmental Buoy EBO-1 for the period of January 1971 to June 1972 are analyzed. The buoy, off the Virginia capes at approximately 36°30′N and 73°30′W, radioed hourly meteorological and oceanographic data to a shore station. Identification of water types at the buoy has been made by comparing the transmitted data with temperature-salinity diagrams. Concurrent observations of lateral shifts in the position of the Gulf Stream show a close correlation with changes in the amount, direction, and temperature-salinity characteristics of the flow at the buoy.