Jason W Barnes, Christophe Sotin, Jason M Soderblom, Robert H Brown, Alexander G Hayes, Mark Donelan, Sebastien Rodriguez, Stéphane Le Mouélic, Kevin H Baines, Thomas B McCord
{"title":"卡西尼/VIMS观察到土卫六Punga Mare粗糙表面的镜面反射。","authors":"Jason W Barnes, Christophe Sotin, Jason M Soderblom, Robert H Brown, Alexander G Hayes, Mark Donelan, Sebastien Rodriguez, Stéphane Le Mouélic, Kevin H Baines, Thomas B McCord","doi":"10.1186/s13535-014-0003-4","DOIUrl":null,"url":null,"abstract":"<p><p><i>Cassini</i>/VIMS high-phase specular observations of Titan's north pole during the T85 flyby show evidence for isolated patches of rough liquid surface within the boundaries of the sea Punga Mare. The roughness shows typical slopes of 6°±1°. These rough areas could be either wet mudflats or a wavy sea. Because of their large areal extent, patchy geographic distribution, and uniform appearance at low phase, we prefer a waves interpretation. Applying theoretical wave calculations based on Titan conditions our slope determination allows us to infer winds of 0.76±0.09 m/s and significant wave heights of [Formula: see text] cm at the time and locations of the observation. If correct, these would represent the first waves seen on Titan's seas, and also the first extraterrestrial sea-surface waves in general.</p>","PeriodicalId":91593,"journal":{"name":"Planetary science","volume":"3 ","pages":"3"},"PeriodicalIF":0.0000,"publicationDate":"2014-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1186/s13535-014-0003-4","citationCount":"34","resultStr":"{\"title\":\"<i>Cassini</i>/VIMS observes rough surfaces on Titan's Punga Mare in specular reflection.\",\"authors\":\"Jason W Barnes, Christophe Sotin, Jason M Soderblom, Robert H Brown, Alexander G Hayes, Mark Donelan, Sebastien Rodriguez, Stéphane Le Mouélic, Kevin H Baines, Thomas B McCord\",\"doi\":\"10.1186/s13535-014-0003-4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p><i>Cassini</i>/VIMS high-phase specular observations of Titan's north pole during the T85 flyby show evidence for isolated patches of rough liquid surface within the boundaries of the sea Punga Mare. The roughness shows typical slopes of 6°±1°. These rough areas could be either wet mudflats or a wavy sea. Because of their large areal extent, patchy geographic distribution, and uniform appearance at low phase, we prefer a waves interpretation. Applying theoretical wave calculations based on Titan conditions our slope determination allows us to infer winds of 0.76±0.09 m/s and significant wave heights of [Formula: see text] cm at the time and locations of the observation. If correct, these would represent the first waves seen on Titan's seas, and also the first extraterrestrial sea-surface waves in general.</p>\",\"PeriodicalId\":91593,\"journal\":{\"name\":\"Planetary science\",\"volume\":\"3 \",\"pages\":\"3\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2014-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1186/s13535-014-0003-4\",\"citationCount\":\"34\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Planetary science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1186/s13535-014-0003-4\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"2014/8/21 0:00:00\",\"PubModel\":\"Epub\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Planetary science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1186/s13535-014-0003-4","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2014/8/21 0:00:00","PubModel":"Epub","JCR":"","JCRName":"","Score":null,"Total":0}
Cassini/VIMS observes rough surfaces on Titan's Punga Mare in specular reflection.
Cassini/VIMS high-phase specular observations of Titan's north pole during the T85 flyby show evidence for isolated patches of rough liquid surface within the boundaries of the sea Punga Mare. The roughness shows typical slopes of 6°±1°. These rough areas could be either wet mudflats or a wavy sea. Because of their large areal extent, patchy geographic distribution, and uniform appearance at low phase, we prefer a waves interpretation. Applying theoretical wave calculations based on Titan conditions our slope determination allows us to infer winds of 0.76±0.09 m/s and significant wave heights of [Formula: see text] cm at the time and locations of the observation. If correct, these would represent the first waves seen on Titan's seas, and also the first extraterrestrial sea-surface waves in general.
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