Observations of Ultrafast Kelvin Wave Breaking in the Mars Thermosphere
Ultrafast Kelvin Waves (UFKWs) have been recently discovered at Mars using measurements by the Mars Atmosphere and Evolution (MAVEN) Accelerometer (ACC) instrument and the Mars Reconnaissance Orbiter (MRO) Mars Climate Sound (MCS) instrument [1]. UFKWs are eastward propagating, have a 2-3 sol period...
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description | Ultrafast Kelvin Waves (UFKWs) have been recently discovered at Mars using measurements by the Mars Atmosphere and Evolution (MAVEN) Accelerometer (ACC) instrument and the Mars Reconnaissance Orbiter (MRO) Mars Climate Sound (MCS) instrument [1]. UFKWs are eastward propagating, have a 2-3 sol period with sufficiently long vertical wavelengths to propagate into the thermosphere, and are predicted by classical wave theory to be equatorially trapped. These prior measurements characterized UFKWs at two relatively narrow altitude bands, with one measurement altitude near 80 km and a second near 150 km. Thermospheric density profiles from solar occultation (SO) measurements made by the Extreme Ultraviolet Monitor (EUVM) onboard MAVEN [2] provide a means to characterize multi-sol period waves, including UFKWs, as a function of altitude. In this study, we present first-ever observations of UFKWs as a function of altitude, including observations of rapid wave energy dissipation near 170 km indicative of wave breaking. |
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UFKWs are eastward propagating, have a 2-3 sol period with sufficiently long vertical wavelengths to propagate into the thermosphere, and are predicted by classical wave theory to be equatorially trapped. These prior measurements characterized UFKWs at two relatively narrow altitude bands, with one measurement altitude near 80 km and a second near 150 km. Thermospheric density profiles from solar occultation (SO) measurements made by the Extreme Ultraviolet Monitor (EUVM) onboard MAVEN [2] provide a means to characterize multi-sol period waves, including UFKWs, as a function of altitude. In this study, we present first-ever observations of UFKWs as a function of altitude, including observations of rapid wave energy dissipation near 170 km indicative of wave breaking.</description><identifier>EISSN: 2331-8422</identifier><language>eng</language><publisher>Ithaca: Cornell University Library, arXiv.org</publisher><subject>Accelerometers ; Altitude ; Energy dissipation ; Kelvin waves ; Mars ; Mars atmosphere ; Solar occultation ; Thermosphere ; Wave breaking ; Wave power ; Wave propagation</subject><ispartof>arXiv.org, 2019-05</ispartof><rights>2019. This work is published under http://arxiv.org/licenses/nonexclusive-distrib/1.0/ (the “License”). 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UFKWs are eastward propagating, have a 2-3 sol period with sufficiently long vertical wavelengths to propagate into the thermosphere, and are predicted by classical wave theory to be equatorially trapped. These prior measurements characterized UFKWs at two relatively narrow altitude bands, with one measurement altitude near 80 km and a second near 150 km. Thermospheric density profiles from solar occultation (SO) measurements made by the Extreme Ultraviolet Monitor (EUVM) onboard MAVEN [2] provide a means to characterize multi-sol period waves, including UFKWs, as a function of altitude. In this study, we present first-ever observations of UFKWs as a function of altitude, including observations of rapid wave energy dissipation near 170 km indicative of wave breaking.</description><subject>Accelerometers</subject><subject>Altitude</subject><subject>Energy dissipation</subject><subject>Kelvin waves</subject><subject>Mars</subject><subject>Mars atmosphere</subject><subject>Solar occultation</subject><subject>Thermosphere</subject><subject>Wave breaking</subject><subject>Wave power</subject><subject>Wave propagation</subject><issn>2331-8422</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNqNissKgkAUQIcgSMp_uNBasDs62bboARFtjJYywTU1m7G5o9-fiz6g1YFzzkQEKOUqyhLEmQiZmziOUa0xTWUgjtcHkxu0r61hsCXcWu90qdnDmdqhNnDXA8HWkX7V5gmj8BXBRTuGvCL3ttyNoIWYlrplCn-ci-Vhn-9OUefspyf2RWN7Z8ZUIKJSMkvkRv53fQH3qzuQ</recordid><startdate>20190515</startdate><enddate>20190515</enddate><creator>Thiemann, Edward M B</creator><creator>Entin, Nicholas D</creator><creator>Bougher, Stephen</creator><creator>Yigit, Erdal</creator><creator>Pawlowski, David</creator><creator>Eparvier, Francis</creator><general>Cornell University Library, arXiv.org</general><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>L6V</scope><scope>M7S</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope></search><sort><creationdate>20190515</creationdate><title>Observations of Ultrafast Kelvin Wave Breaking in the Mars Thermosphere</title><author>Thiemann, Edward M B ; Entin, Nicholas D ; Bougher, Stephen ; Yigit, Erdal ; Pawlowski, David ; Eparvier, Francis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-proquest_journals_22266384393</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Accelerometers</topic><topic>Altitude</topic><topic>Energy dissipation</topic><topic>Kelvin waves</topic><topic>Mars</topic><topic>Mars atmosphere</topic><topic>Solar occultation</topic><topic>Thermosphere</topic><topic>Wave breaking</topic><topic>Wave power</topic><topic>Wave propagation</topic><toplevel>online_resources</toplevel><creatorcontrib>Thiemann, Edward M B</creatorcontrib><creatorcontrib>Entin, Nicholas D</creatorcontrib><creatorcontrib>Bougher, Stephen</creatorcontrib><creatorcontrib>Yigit, Erdal</creatorcontrib><creatorcontrib>Pawlowski, David</creatorcontrib><creatorcontrib>Eparvier, Francis</creatorcontrib><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Engineering Collection</collection><collection>Engineering Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Thiemann, Edward M B</au><au>Entin, Nicholas D</au><au>Bougher, Stephen</au><au>Yigit, Erdal</au><au>Pawlowski, David</au><au>Eparvier, Francis</au><format>book</format><genre>document</genre><ristype>GEN</ristype><atitle>Observations of Ultrafast Kelvin Wave Breaking in the Mars Thermosphere</atitle><jtitle>arXiv.org</jtitle><date>2019-05-15</date><risdate>2019</risdate><eissn>2331-8422</eissn><abstract>Ultrafast Kelvin Waves (UFKWs) have been recently discovered at Mars using measurements by the Mars Atmosphere and Evolution (MAVEN) Accelerometer (ACC) instrument and the Mars Reconnaissance Orbiter (MRO) Mars Climate Sound (MCS) instrument [1]. 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subjects | Accelerometers Altitude Energy dissipation Kelvin waves Mars Mars atmosphere Solar occultation Thermosphere Wave breaking Wave power Wave propagation |
title | Observations of Ultrafast Kelvin Wave Breaking in the Mars Thermosphere |
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