mycoreobjectrosdok_disshab_0000000864rosdok_disshab_0000000864rosdokdisshabrosdok_derivate_00000049182023-08-08T10:03:31.927Z2012-10-24T10:58:52.045Zadministratorpublished1rosdok_derivate_0000004918truetruederivate_types:fulltextVolltextfulltextwf_edit_epub wf_register_epubstate:publishedstate:publishedveröffentlichtpublishedrosdok/id00001043728562693MODS updated during RosDok migration in June 2021DissertationHochschulschrift1027036279SebastianBrune1974-VerfasserInautAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseenProf. Dr.ErichBeckerAkademischeR BetreuerIndgsProf. Dr.VolkmarWirthAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg10.18453/rosdok_id00001043http://purl.uni-rostock.de/rosdok/id00001043urn:nbn:de:gbv:28-diss2012-0082-2550 Geowissenschaften530 PhysikMathematisch-Naturwissenschaftliche Fakultätfrei zugänglich (Open Access)Lizenz Metadaten: CC0Nutzungsrechte erteiltalle Rechte vorbehaltenUniversität RostockRostock2012monographic20122012Universitätsbibliothek RostockRostock20122012This thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy spectrum can be explained by stratified turbulence. Secondly, the mesoscale energy deposition in the upper mesosphere can be explained by the vertical pressure flux carried by mesoscale gravity waves from the troposphere, which is converted into kinetic energy of these waves and then dissipated.tropospheremesosphereturbulencegeneral circulation modelgravity waveUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id00001043doctype:epubdoctype:epubDokumenttypDocument typedoctype:epub.dissertationdoctype:epub.dissertationDissertationdoctoral thesisdiniPublType:doctoralThesis diniPublType2022:PhDThesis XMetaDissPlusThesisLevel:thesis.doctoralinfo:eu-repo/semantics/doctoralThesisdocumentnatureOfContent:ppn_105825778natureOfContent:ppn_105825778HochschulschriftdiniPublType2022:DoctoralThesisdiniPublType2022:DoctoralThesisDissertation oder HabilitationDoctoral thesisDRIVERdiniPublType2022:PhDThesisdiniPublType2022:PhDThesisDissertationPhD thesisKDSF (Pu34)XMetaDissPlusThesisLevel:thesis.doctoralXMetaDissPlusThesisLevel:thesis.doctoralDoktorarbeitdoctoral thesisrfc5646:enrfc5646:enEnglischEnglishengengSDNB:550SDNB:550550 Geowissenschaften550 Earth sciencesSDNB:530SDNB:530530 Physik530 Physicsinstitution:unirostockinstitution:unirostockUniversität RostockUniversity of RostockUniversität RostockUniversität RostockUni.Rostockhttp://d-nb.info/gnd/38329-6institution:unirostock.mnfinstitution:unirostock.mnfMathematisch-Naturwissenschaftliche FakultätFaculty of Mathematics and Natural SciencesUniversität Rostock. Mathematisch-Naturwissenschaftliche FakultätMathematisch-Natur-<br />wissenschaftliche FakultätUni.Rostock.Fakultaet.MNFhttp://d-nb.info/gnd/2147083-2accesscondition:openaccessaccesscondition:openaccessfrei zugänglich (Open Access)open accesshttp://purl.org/coar/access_right/c_abf2OAfreeinfo:eu-repo/semantics/openAccess[DE-28]Open Access$gControlled Vocabulary for Access Rights$uhttp://purl.org/coar/access_right/c_abf2licenseinfo:metadatalicenseinfo:metadataLizenzen für Metadatenlicenseinfo:metadata.cc0licenseinfo:metadata.cc0Lizenz Metadaten: CC0license metadata: CC0/creativecommons/p/zero/1.0/88x31.pnghttps://creativecommons.org/publicdomain/zero/1.0/licenseinfo:depositlicenseinfo:depositVeröffentlichungsgenehmigungpermission to storelicenseinfo:deposit.rightsgrantedlicenseinfo:deposit.rightsgrantedNutzungsrechte erteiltrights grantedlicenseinfo:worklicenseinfo:workWerkworklicenseinfo:work.rightsreservedlicenseinfo:work.rightsreservedalle Rechte vorbehaltenall rights reserved/creativecommons/r/reserved/0.9/88x31.png[DE-28]Urheberrechtsschutz 1.0$gRights Statements$uhttp://rightsstatements.org/vocab/InC/1.0/http://rightsstatements.org/vocab/InC/1.0/http://rightsstatements.org/vocab/InC/1.0/Analysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the Mesopausegnd:1027036279gnd:2147083-2gnd:1027036279gnd:2147083-2rosdok_disshab_0000000864-d919612e39gnd:1027036279Sebastian BruneSebastian Brunerosdok_disshab_0000000864-d919612e60Prof. Dr. Erich BeckerProf. Dr. Erich Beckerrosdok_disshab_0000000864-d919612e72Prof. Dr. Volkmar WirthProf. Dr. Volkmar Wirthrosdok_disshab_0000000864-d919612e84gnd:2147083-2Universität Rostock Mathematisch-Naturwissenschaftliche FakultätUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneProf. Dr. Erich BeckerProf. Dr. Volkmar WirthUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneProf. Dr. Erich BeckerProf. Dr. Volkmar WirthUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneRostockUniversität Rostockepub.dissertation10.18453/rosdok_id00001043http://purl.uni-rostock.de/rosdok/id00001043urn:nbn:de:gbv:28-diss2012-0082-2tropospheremesosphereturbulencegeneral circulation modelgravity waveThis thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy spectrum can be explained by stratified turbulence. Secondly, the mesoscale energy deposition in the upper mesosphere can be explained by the vertical pressure flux carried by mesoscale gravity waves from the troposphere, which is converted into kinetic energy of these waves and then dissipated.20122012epub.dissertation1 Dissertation_Brune_2012.pdf 21376461 96f3cf280dfe773b155a4356a505895c rosdok/id00001043728562693MODS updated during RosDok migration in June 2021DissertationHochschulschrift1027036279SebastianBrune1974-VerfasserInautAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseenProf. Dr.ErichBeckerAkademischeR BetreuerIndgsProf. Dr.VolkmarWirthAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg10.18453/rosdok_id00001043http://purl.uni-rostock.de/rosdok/id00001043urn:nbn:de:gbv:28-diss2012-0082-2550 Geowissenschaften530 PhysikMathematisch-Naturwissenschaftliche Fakultätfrei zugänglich (Open Access)Lizenz Metadaten: CC0Nutzungsrechte erteiltalle Rechte vorbehaltenUniversität RostockRostock2012monographic20122012Universitätsbibliothek RostockRostock20122012This thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy spectrum can be explained by stratified turbulence. Secondly, the mesoscale energy deposition in the upper mesosphere can be explained by the vertical pressure flux carried by mesoscale gravity waves from the troposphere, which is converted into kinetic energy of these waves and then dissipated.tropospheremesosphereturbulencegeneral circulation modelgravity waveUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id00001043 2012-10-24T10:58:52.045Z 2023-08-08T10:03:31.927Z 2023-08-18T10:03:31.932Z {"identifier":"rosdok/id00001043","type":"local_id","additional":"","service":"MCRLocalID","created":"2018-06-30T12:58:35.632Z"} {"identifier":"http://purl.uni-rostock.de/rosdok/id00001043","type":"purl","additional":"","service":"RosDokPURL","created":"2018-06-30T12:58:35.828Z","registered":"2018-06-30T12:58:35.828Z"} {"identifier":"10.18453/rosdok_id00001043","type":"doi","additional":"","service":"RosDokDOI","created":"2018-06-30T12:58:37.090Z","registered":"2018-06-30T12:58:37.090Z"} {"identifier":"urn:nbn:de:gbv:28-diss2012-0082-2","type":"dnbUrn","additional":"","service":"RosDokURN","created":"2018-06-30T12:58:35.637Z","registered":"2012-10-26T02:30:14.983Z"} administratorfulltextfile/rosdok_disshab_0000000864/rosdok_derivate_0000004918/Dissertation_Brune_2012.pdfAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the Mesopausegnd:1027036279gnd:2147083-2gnd:1027036279gnd:2147083-2rosdok_disshab_0000000864-d919612e39gnd:1027036279Sebastian BruneSebastian Brunerosdok_disshab_0000000864-d919612e60Prof. Dr. Erich BeckerProf. Dr. Erich Beckerrosdok_disshab_0000000864-d919612e72Prof. Dr. Volkmar WirthProf. Dr. Volkmar Wirthrosdok_disshab_0000000864-d919612e84gnd:2147083-2Universität Rostock Mathematisch-Naturwissenschaftliche FakultätUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneProf. Dr. Erich BeckerProf. Dr. Volkmar WirthUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneProf. Dr. Erich BeckerProf. Dr. Volkmar WirthUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätSebastian BruneRostockUniversität Rostockepub.dissertation10.18453/rosdok_id00001043http://purl.uni-rostock.de/rosdok/id00001043urn:nbn:de:gbv:28-diss2012-0082-2tropospheremesosphereturbulencegeneral circulation modelgravity waveThis thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy spectrum can be explained by stratified turbulence. Secondly, the mesoscale energy deposition in the upper mesosphere can be explained by the vertical pressure flux carried by mesoscale gravity waves from the troposphere, which is converted into kinetic energy of these waves and then dissipated.20122012[xslt]Saxonrosdok/id00001043https://purl.uni-rostock.de/rosdok/id0000104372856269310.18453/rosdok_id00001043urn:nbn:de:gbv:28-diss2012-0082-2Sebastian BruneBrune SebastianAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseDissertationdoctoral thesisUniversität Rostock, 2012This thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy…Sebastian BruneAnalysis of the Global Spectrum of the Atmospheric Horizontal Kinetic Energy from the Boundary Layer to the MesopauseUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id000010431027036279SebastianBrune1974-VerfasserInautProf. Dr.ErichBeckerAkademischeR BetreuerIndgsProf. Dr.VolkmarWirthAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg[doi]10.18453/rosdok_id00001043[purl]http://purl.uni-rostock.de/rosdok/id00001043[urn]urn:nbn:de:gbv:28-diss2012-0082-2open_access20122012epoch:21th_centuryrfc5646:endoctype:epub.dissertationaccesscondition:openaccessSDNB:550SDNB:530institution:unirostock.mnfstate:published