mycoreobjectrosdok_disshab_0000001853rosdok_disshab_0000001853rosdokdisshabrosdok_derivate_00000384642023-08-08T10:08:38.249Z2018-03-21T15:22:19.114ZadministratoreditorDpublished1rosdok_derivate_0000038464truetruederivate_types:fulltextVolltextfulltextwf_edit_epub wf_register_epubstate:publishedstate:publishedveröffentlichtpublishedrosdok/id000020311016265794MODS updated during RosDok migration in June 2021DissertationHochschulschrift1154443795ChrisLappe1986-VerfasserInautBoundary mixing in non-tidal basinsobservations from the Baltic Seaen123500036Dr.LarsUmlaufUniversität Rostock, Leibniz-Institut für Ostseeforschung WarnemündeAkademischeR BetreuerIndgsProf. Dr.LarsArneborgUniversity of Gothenburg, Swedish Meteorological and Hydrological InstituteAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg10.18453/rosdok_id00002031http://purl.uni-rostock.de/rosdok/id00002031urn:nbn:de:gbv:28-diss2018-0025-6530 PhysikMathematisch-Naturwissenschaftliche Fakultätfrei zugänglich (Open Access)Lizenz Metadaten: CC0Nutzungsrechte erteiltalle Rechte vorbehaltenUniversität RostockRostock2018monographic20182018Universitätsbibliothek RostockRostock20182018The investigations are based on two data sets from the Bornholm Basin and include high-resolution CTD, shear microstructure, and velocity data. A highly turbulent and strongly stratified bottom boundary layer (BBL) of a few meters thickness develops, which exhibits high mixing rates and a bulk mixing efficiency that is comparable to the interior value of 0.2. The BBL turbulence was found to be suppressed within the halocline in summer, and does therefore not contribute to cross-halocline mixing in this region.diapycnal mixingmixing efficiencyBBLsloping boundaryhaloclineUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id00002031doctype: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: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/Boundary mixing in non-tidal basinsobservations from the Baltic SeaBoundary mixing in non-tidal basinsobservations from the Baltic Seagnd:1154443795gnd:123500036gnd:2147083-2gnd:1154443795gnd:123500036gnd:2147083-2rosdok_disshab_0000001853-d2075063e39gnd:1154443795Chris LappeChris Lapperosdok_disshab_0000001853-d2075063e61gnd:123500036Dr. Lars UmlaufDr. Lars Umlaufrosdok_disshab_0000001853-d2075063e76Prof. Dr. Lars ArneborgProf. Dr. Lars Arneborgrosdok_disshab_0000001853-d2075063e89gnd:2147083-2Universität Rostock Mathematisch-Naturwissenschaftliche FakultätUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeDr. Lars UmlaufProf. Dr. Lars ArneborgUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeDr. Lars UmlaufProf. Dr. Lars ArneborgUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeRostockUniversität Rostockepub.dissertation10.18453/rosdok_id00002031http://purl.uni-rostock.de/rosdok/id00002031urn:nbn:de:gbv:28-diss2018-0025-6diapycnal mixingmixing efficiencyBBLsloping boundaryhaloclineThe investigations are based on two data sets from the Bornholm Basin and include high-resolution CTD, shear microstructure, and velocity data. A highly turbulent and strongly stratified bottom boundary layer (BBL) of a few meters thickness develops, which exhibits high mixing rates and a bulk mixing efficiency that is comparable to the interior value of 0.2. The BBL turbulence was found to be suppressed within the halocline in summer, and does therefore not contribute to cross-halocline mixing in this region.20182018epub.dissertation1 Dissertation_Lappe_2018.pdf 26163860 24cb5a2c474cdfa38f596baafd6574f4 rosdok/id000020311016265794MODS updated during RosDok migration in June 2021DissertationHochschulschrift1154443795ChrisLappe1986-VerfasserInautBoundary mixing in non-tidal basinsobservations from the Baltic Seaen123500036Dr.LarsUmlaufUniversität Rostock, Leibniz-Institut für Ostseeforschung WarnemündeAkademischeR BetreuerIndgsProf. Dr.LarsArneborgUniversity of Gothenburg, Swedish Meteorological and Hydrological InstituteAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg10.18453/rosdok_id00002031http://purl.uni-rostock.de/rosdok/id00002031urn:nbn:de:gbv:28-diss2018-0025-6530 PhysikMathematisch-Naturwissenschaftliche Fakultätfrei zugänglich (Open Access)Lizenz Metadaten: CC0Nutzungsrechte erteiltalle Rechte vorbehaltenUniversität RostockRostock2018monographic20182018Universitätsbibliothek RostockRostock20182018The investigations are based on two data sets from the Bornholm Basin and include high-resolution CTD, shear microstructure, and velocity data. A highly turbulent and strongly stratified bottom boundary layer (BBL) of a few meters thickness develops, which exhibits high mixing rates and a bulk mixing efficiency that is comparable to the interior value of 0.2. The BBL turbulence was found to be suppressed within the halocline in summer, and does therefore not contribute to cross-halocline mixing in this region.diapycnal mixingmixing efficiencyBBLsloping boundaryhaloclineUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id00002031 2018-03-21T15:22:19.114Z 2023-08-08T10:08:38.249Z 2023-08-18T10:08:38.254Z editorD {"identifier":"rosdok/id00002031","type":"local_id","additional":"","service":"MCRLocalID","created":"2018-06-30T13:33:57.519Z"} {"identifier":"http://purl.uni-rostock.de/rosdok/id00002031","type":"purl","additional":"","service":"RosDokPURL","created":"2018-06-30T13:33:57.707Z","registered":"2018-06-30T13:33:57.707Z"} {"identifier":"10.18453/rosdok_id00002031","type":"doi","additional":"","service":"RosDokDOI","created":"2018-06-30T13:33:58.996Z","registered":"2018-06-30T13:33:58.996Z"} {"identifier":"urn:nbn:de:gbv:28-diss2018-0025-6","type":"dnbUrn","additional":"","service":"RosDokURN","created":"2018-06-30T13:33:57.525Z","registered":"2018-03-23T03:27:11.533Z"} administratorfulltextfile/rosdok_disshab_0000001853/rosdok_derivate_0000038464/Dissertation_Lappe_2018.pdfBoundary mixing in non-tidal basinsobservations from the Baltic SeaBoundary mixing in non-tidal basinsobservations from the Baltic Seagnd:1154443795gnd:123500036gnd:2147083-2gnd:1154443795gnd:123500036gnd:2147083-2rosdok_disshab_0000001853-d2075063e39gnd:1154443795Chris LappeChris Lapperosdok_disshab_0000001853-d2075063e61gnd:123500036Dr. Lars UmlaufDr. Lars Umlaufrosdok_disshab_0000001853-d2075063e76Prof. Dr. Lars ArneborgProf. Dr. Lars Arneborgrosdok_disshab_0000001853-d2075063e89gnd:2147083-2Universität Rostock Mathematisch-Naturwissenschaftliche FakultätUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeDr. Lars UmlaufProf. Dr. Lars ArneborgUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeDr. Lars UmlaufProf. Dr. Lars ArneborgUniversität Rostock Mathematisch-Naturwissenschaftliche FakultätChris LappeRostockUniversität Rostockepub.dissertation10.18453/rosdok_id00002031http://purl.uni-rostock.de/rosdok/id00002031urn:nbn:de:gbv:28-diss2018-0025-6diapycnal mixingmixing efficiencyBBLsloping boundaryhaloclineThe investigations are based on two data sets from the Bornholm Basin and include high-resolution CTD, shear microstructure, and velocity data. A highly turbulent and strongly stratified bottom boundary layer (BBL) of a few meters thickness develops, which exhibits high mixing rates and a bulk mixing efficiency that is comparable to the interior value of 0.2. The BBL turbulence was found to be suppressed within the halocline in summer, and does therefore not contribute to cross-halocline mixing in this region.20182018[xslt]Saxonrosdok/id00002031https://purl.uni-rostock.de/rosdok/id00002031101626579410.18453/rosdok_id00002031urn:nbn:de:gbv:28-diss2018-0025-6Chris LappeLappe ChrisBoundary mixing in non-tidal basins : observations from the Baltic SeaDissertationdoctoral thesisUniversität Rostock, 2018The investigations are based on two data sets from the Bornholm Basin and include high-resolution CTD, shear microstructure, and velocity data. A highly turbulent and strongly stratified bottom boundary layer (BBL) of a few meters thickness develops, which exhibits high mixing rates and a bulk…Chris LappeBoundary mixing in non-tidal basinsobservations from the Baltic SeaUniversitätsbibliothek Rostockhttp://purl.uni-rostock.de/rosdok/id000020311154443795ChrisLappe1986-VerfasserInaut123500036Dr.LarsUmlaufUniversität Rostock, Leibniz-Institut für Ostseeforschung WarnemündeAkademischeR BetreuerIndgsProf. Dr.LarsArneborgUniversity of Gothenburg, Swedish Meteorological and Hydrological InstituteAkademischeR BetreuerIndgs2147083-2Universität RostockMathematisch-Naturwissenschaftliche FakultätGrad-verleihende Institutiondgg[doi]10.18453/rosdok_id00002031[purl]http://purl.uni-rostock.de/rosdok/id00002031[urn]urn:nbn:de:gbv:28-diss2018-0025-6open_access20182018epoch:21th_centuryrfc5646:endoctype:epub.dissertationaccesscondition:openaccessSDNB:530institution:unirostock.mnfstate:published