{"title":"海上人工上升流的流量估算","authors":"John Thorson","doi":"10.1016/0146-6313(61)90050-8","DOIUrl":null,"url":null,"abstract":"<div><p>An order-of-magnitude calculation of the limiting efficiency of an artificial heat source in producing a vertical oceanic current is suggested. An estimate by Groves then permits interpretation of upward flow rate of deep nutrient-rich water in terms of edible fish production rate near the surface. The latter quantity is found to be small for very large artificial heat sources.</p></div>","PeriodicalId":100361,"journal":{"name":"Deep Sea Research (1953)","volume":"7 4","pages":"Pages 296-297"},"PeriodicalIF":0.0000,"publicationDate":"1961-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0146-6313(61)90050-8","citationCount":"2","resultStr":"{\"title\":\"Flow estimate for an artificial upwelling in the sea\",\"authors\":\"John Thorson\",\"doi\":\"10.1016/0146-6313(61)90050-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>An order-of-magnitude calculation of the limiting efficiency of an artificial heat source in producing a vertical oceanic current is suggested. An estimate by Groves then permits interpretation of upward flow rate of deep nutrient-rich water in terms of edible fish production rate near the surface. The latter quantity is found to be small for very large artificial heat sources.</p></div>\",\"PeriodicalId\":100361,\"journal\":{\"name\":\"Deep Sea Research (1953)\",\"volume\":\"7 4\",\"pages\":\"Pages 296-297\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1961-03-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0146-6313(61)90050-8\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep Sea Research (1953)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0146631361900508\",\"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/0146631361900508","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Flow estimate for an artificial upwelling in the sea
An order-of-magnitude calculation of the limiting efficiency of an artificial heat source in producing a vertical oceanic current is suggested. An estimate by Groves then permits interpretation of upward flow rate of deep nutrient-rich water in terms of edible fish production rate near the surface. The latter quantity is found to be small for very large artificial heat sources.
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