{"title":"赤道地区的一般热环流","authors":"Allan R. Robinson","doi":"10.1016/0146-6313(59)90090-5","DOIUrl":null,"url":null,"abstract":"<div><p>An approximation valid near the equator is developed for a model of the general thermal circulation. The existence of equatorial effects is related to the vanishing of the Coriolis parameter, and the equatorial approximation is related to the mid-latitude circulation. Qualitative features of the solutions are discussed.</p></div>","PeriodicalId":100361,"journal":{"name":"Deep Sea Research (1953)","volume":"6 ","pages":"Pages 311-317"},"PeriodicalIF":0.0000,"publicationDate":"1959-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0146-6313(59)90090-5","citationCount":"19","resultStr":"{\"title\":\"The general thermal circulation in equatorial regions\",\"authors\":\"Allan R. Robinson\",\"doi\":\"10.1016/0146-6313(59)90090-5\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>An approximation valid near the equator is developed for a model of the general thermal circulation. The existence of equatorial effects is related to the vanishing of the Coriolis parameter, and the equatorial approximation is related to the mid-latitude circulation. Qualitative features of the solutions are discussed.</p></div>\",\"PeriodicalId\":100361,\"journal\":{\"name\":\"Deep Sea Research (1953)\",\"volume\":\"6 \",\"pages\":\"Pages 311-317\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1959-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0146-6313(59)90090-5\",\"citationCount\":\"19\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Deep Sea Research (1953)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0146631359900905\",\"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/0146631359900905","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The general thermal circulation in equatorial regions
An approximation valid near the equator is developed for a model of the general thermal circulation. The existence of equatorial effects is related to the vanishing of the Coriolis parameter, and the equatorial approximation is related to the mid-latitude circulation. Qualitative features of the solutions are discussed.
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