{"title":"Results of a marine radar sea clutter experiment for non-equilibrium seas","authors":"D.B. Trizna","doi":"10.1109/NRC.1989.47640","DOIUrl":null,"url":null,"abstract":"Results are presented for an upwind-illumination, low-grazing-angle marine radar sea scatter experiment conducted in the Pacific Ocean. A wide range of wind speeds and directions resulted in nonequilibrium sea conditions, in contrast to a previous Atlantic Ocean experiment in which ocean waves were fully developed. Statistical properties of the radar echoes are parameterized by a dual-Weibull model versus wind speed and are compared with the North Atlantic data. It is concluded that the Pacific results can be regarded as a lower limit case, appropriate to random seas, whereas the North Atlantic results can be regarded as an upper limit for well-developed seas.<<ETX>>","PeriodicalId":167059,"journal":{"name":"Proceedings of the IEEE National Radar Conference","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"1989-03-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the IEEE National Radar Conference","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/NRC.1989.47640","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3
Abstract
Results are presented for an upwind-illumination, low-grazing-angle marine radar sea scatter experiment conducted in the Pacific Ocean. A wide range of wind speeds and directions resulted in nonequilibrium sea conditions, in contrast to a previous Atlantic Ocean experiment in which ocean waves were fully developed. Statistical properties of the radar echoes are parameterized by a dual-Weibull model versus wind speed and are compared with the North Atlantic data. It is concluded that the Pacific results can be regarded as a lower limit case, appropriate to random seas, whereas the North Atlantic results can be regarded as an upper limit for well-developed seas.<>