{"title":"1958年3月加利福尼亚海流的测量","authors":"Feenan D. Jennings , Richard A. Schwartzlose","doi":"10.1016/0146-6313(60)90006-X","DOIUrl":null,"url":null,"abstract":"<div><p>Two sets of drogues were placed approximately normal to the usual flow and followed for one and three days respectively. The first set, which extended thirty miles offshore, drifted south-eastward. The second set, which extended from thirty to seventy miles offshore, also moved south-eastward but with considerable variation in speed and direction along the line. In the latter set two rapidly moving streams appeared with a body of slower water between.</p></div>","PeriodicalId":100361,"journal":{"name":"Deep Sea Research (1953)","volume":"7 1","pages":"Pages 42-47"},"PeriodicalIF":0.0000,"publicationDate":"1960-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0146-6313(60)90006-X","citationCount":"7","resultStr":"{\"title\":\"Measurements of the California current in March 1958\",\"authors\":\"Feenan D. Jennings , Richard A. Schwartzlose\",\"doi\":\"10.1016/0146-6313(60)90006-X\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Two sets of drogues were placed approximately normal to the usual flow and followed for one and three days respectively. The first set, which extended thirty miles offshore, drifted south-eastward. The second set, which extended from thirty to seventy miles offshore, also moved south-eastward but with considerable variation in speed and direction along the line. In the latter set two rapidly moving streams appeared with a body of slower water between.</p></div>\",\"PeriodicalId\":100361,\"journal\":{\"name\":\"Deep Sea Research (1953)\",\"volume\":\"7 1\",\"pages\":\"Pages 42-47\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1960-08-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0146-6313(60)90006-X\",\"citationCount\":\"7\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep Sea Research (1953)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/014663136090006X\",\"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/014663136090006X","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Measurements of the California current in March 1958
Two sets of drogues were placed approximately normal to the usual flow and followed for one and three days respectively. The first set, which extended thirty miles offshore, drifted south-eastward. The second set, which extended from thirty to seventy miles offshore, also moved south-eastward but with considerable variation in speed and direction along the line. In the latter set two rapidly moving streams appeared with a body of slower water between.
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
