{"title":"延伸性河口对冬季风暴的响应","authors":"A. Elliott","doi":"10.2307/1351200","DOIUrl":null,"url":null,"abstract":"Current and tidal records from the Patuxent estuary are analyzed to investigate the response of the river after a two-day period of strong northwesterly winds. The storm depressed mean water levels throughout the Chesapeake area, and the Patuxent, required about two days to recover to its former mean water level. Surface slopes provided evidence for the existence of a long period seiche.","PeriodicalId":106819,"journal":{"name":"Chesapeake Science","volume":"9 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1976-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"Response of the patuxent estuary to a winter storm\",\"authors\":\"A. Elliott\",\"doi\":\"10.2307/1351200\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Current and tidal records from the Patuxent estuary are analyzed to investigate the response of the river after a two-day period of strong northwesterly winds. The storm depressed mean water levels throughout the Chesapeake area, and the Patuxent, required about two days to recover to its former mean water level. Surface slopes provided evidence for the existence of a long period seiche.\",\"PeriodicalId\":106819,\"journal\":{\"name\":\"Chesapeake Science\",\"volume\":\"9 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1976-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chesapeake Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2307/1351200\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chesapeake Science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2307/1351200","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Response of the patuxent estuary to a winter storm
Current and tidal records from the Patuxent estuary are analyzed to investigate the response of the river after a two-day period of strong northwesterly winds. The storm depressed mean water levels throughout the Chesapeake area, and the Patuxent, required about two days to recover to its former mean water level. Surface slopes provided evidence for the existence of a long period seiche.