{"title":"海浪破碎时产生的低频声音","authors":"S. L. Means","doi":"10.1121/1.1636502","DOIUrl":null,"url":null,"abstract":"An existing collective oscillation model for low-frequency sound generation from an open-ocean wave is extended to the surf zone. The hemispherical geometry of the open-ocean breaking wave entrained bubble cloud is replaced by a prolate hemispheroidal cloud. A Green’s function is obtained for a point source within this cloud. The far-field acoustic intensity is then computed for a distribution of point sources within a cloud. It is hypothesized that cloud resonances, assuming a “long” orientation is applicable, are determined by the minor-axis length for cloud sizes observed in the surf zone at frequencies of interest here.","PeriodicalId":87384,"journal":{"name":"Acoustics research letters online : ARLO","volume":"49 1","pages":"13-18"},"PeriodicalIF":0.0000,"publicationDate":"2004-02-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":"{\"title\":\"Low-frequency sound generation from breaking surf\",\"authors\":\"S. L. Means\",\"doi\":\"10.1121/1.1636502\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"An existing collective oscillation model for low-frequency sound generation from an open-ocean wave is extended to the surf zone. The hemispherical geometry of the open-ocean breaking wave entrained bubble cloud is replaced by a prolate hemispheroidal cloud. A Green’s function is obtained for a point source within this cloud. The far-field acoustic intensity is then computed for a distribution of point sources within a cloud. It is hypothesized that cloud resonances, assuming a “long” orientation is applicable, are determined by the minor-axis length for cloud sizes observed in the surf zone at frequencies of interest here.\",\"PeriodicalId\":87384,\"journal\":{\"name\":\"Acoustics research letters online : ARLO\",\"volume\":\"49 1\",\"pages\":\"13-18\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2004-02-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"7\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acoustics research letters online : ARLO\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1121/1.1636502\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acoustics research letters online : ARLO","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1121/1.1636502","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
An existing collective oscillation model for low-frequency sound generation from an open-ocean wave is extended to the surf zone. The hemispherical geometry of the open-ocean breaking wave entrained bubble cloud is replaced by a prolate hemispheroidal cloud. A Green’s function is obtained for a point source within this cloud. The far-field acoustic intensity is then computed for a distribution of point sources within a cloud. It is hypothesized that cloud resonances, assuming a “long” orientation is applicable, are determined by the minor-axis length for cloud sizes observed in the surf zone at frequencies of interest here.