DC ElementWertSprache
dc.contributor.authorPail, R.-
dc.contributor.authorBamber, J.-
dc.contributor.authorBiancale, R.-
dc.contributor.authorBingham, R.-
dc.contributor.authorBraitenberg, C.-
dc.contributor.authorEicker, Annette-
dc.contributor.authorFlechtner, F.-
dc.contributor.authorGruber, T.-
dc.contributor.authorGüntner, A.-
dc.contributor.authorHeinzel, G.-
dc.contributor.authorHorwath, M.-
dc.contributor.authorLonguevergne, L.-
dc.contributor.authorMüller, J.-
dc.contributor.authorPanet, I.-
dc.contributor.authorSavenije, H.-
dc.contributor.authorSeneviratne, S.-
dc.contributor.authorSneeuw, N.-
dc.contributor.authorvan Dam, T.-
dc.contributor.authorWouters, B.-
dc.date.accessioned2023-11-17T10:11:29Z-
dc.date.available2023-11-17T10:11:29Z-
dc.date.issued2019-
dc.identifier.issn2081-9943en_US
dc.identifier.urihttps://repos.hcu-hamburg.de/handle/hcu/930-
dc.description.abstractAs changes in gravity are directly related to mass variability, satellite missions observing the Earth's time varying gravity field are a unique tool for observing mass transport processes in the Earth system, such as the water cycle, rapid changes in the cryosphere, oceans, and solid Earth processes, on a global scale. The observation of Earth's gravity field was successfully performed by the GRACE and GOCE satellite missions, and will be continued by the GRACE Follow-On mission. A comprehensive team of European scientists proposed the next-generation gravity field mission MOBILE in response to the European Space Agency (ESA) call for a Core Mission in the frame of Earth Explorer 10 (EE10). MOBILE is based on the innovative observational concept of a high-low tracking formation with micrometer ranging accuracy, complemented by new instrument concepts. Since a high-low tracking mission primarily observes the radial component of gravity-induced orbit perturbations, the error structure is close to isotropic. This geometry significantly reduces artefacts of previous along-track ranging low-low formations (GRACE, GRACE-Follow-On) such as the typical striping patterns. The minimum configuration consists of at least two medium-Earth orbiters (MEOs) at 10000 km altitude or higher, and one low-Earth orbiter (LEO) at 350-400 km. The main instrument is a laser-based distance or distance change measurement system, which is placed at the LEO. The MEOs are equipped either with passive reflectors or transponders. In a numerical closed-loop simulation, it was demonstrated that this minimum configuration is in agreement with the threshold science requirements of 5 mm equivalent water height (EWH) accuracy at 400 km wavelength, and 10 cm EWH at 200 km. MOBILE provides promising potential future perspectives by linking the concept to existing space infrastructure such as Galileo next-generation, as future element of the Copernicus/Sentinel programme, and holds the potential of miniaturization even up to swarm configurations. As such MOBILE can be considered as a precursor and role model for a sustained mass transport observing system from space.en
dc.language.isoenen_US
dc.publisherDe Gruyteren_US
dc.relation.ispartofJournal of Geodetic Scienceen_US
dc.subjectmass transporten
dc.subjectnext-generation gravity missionen
dc.subjectgravity fielden
dc.subjecthigh-low trackingen
dc.subjectspherical harmonicsen
dc.subject.ddc550: Geowissenschaftenen_US
dc.titleMass variation observing system by high low inter-satellite links (MOBILE) – a new concept for sustained observation of mass transport from spacede
dc.typeArticleen_US
dc.type.diniarticle-
dc.type.driverarticle-
dc.rights.cchttps://creativecommons.org/licenses/by/4.0/en_US
dc.type.casraiJournal Article-
dcterms.DCMITypeText-
tuhh.identifier.urnurn:nbn:de:gbv:1373-repos-11995-
tuhh.oai.showtrueen_US
tuhh.publisher.doi10.1515/jogs-2019-0006-
tuhh.publication.instituteGeodäsie und Ausgleichungsrechnungen_US
tuhh.type.opus(wissenschaftlicher) Artikel-
tuhh.container.issue1en_US
tuhh.container.volume9en_US
tuhh.container.startpage48en_US
tuhh.container.endpage58en_US
openaire.rightsinfo:eu-repo/semantics/openAccessen_US
item.languageiso639-1en-
item.fulltextWith Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.creatorGNDPail, R.-
item.creatorGNDBamber, J.-
item.creatorGNDBiancale, R.-
item.creatorGNDBingham, R.-
item.creatorGNDBraitenberg, C.-
item.creatorGNDEicker, Annette-
item.creatorGNDFlechtner, F.-
item.creatorGNDGruber, T.-
item.creatorGNDGüntner, A.-
item.creatorGNDHeinzel, G.-
item.creatorGNDHorwath, M.-
item.creatorGNDLonguevergne, L.-
item.creatorGNDMüller, J.-
item.creatorGNDPanet, I.-
item.creatorGNDSavenije, H.-
item.creatorGNDSeneviratne, S.-
item.creatorGNDSneeuw, N.-
item.creatorGNDvan Dam, T.-
item.creatorGNDWouters, B.-
item.grantfulltextopen-
item.openairetypeArticle-
item.creatorOrcidPail, R.-
item.creatorOrcidBamber, J.-
item.creatorOrcidBiancale, R.-
item.creatorOrcidBingham, R.-
item.creatorOrcidBraitenberg, C.-
item.creatorOrcidEicker, Annette-
item.creatorOrcidFlechtner, F.-
item.creatorOrcidGruber, T.-
item.creatorOrcidGüntner, A.-
item.creatorOrcidHeinzel, G.-
item.creatorOrcidHorwath, M.-
item.creatorOrcidLonguevergne, L.-
item.creatorOrcidMüller, J.-
item.creatorOrcidPanet, I.-
item.creatorOrcidSavenije, H.-
item.creatorOrcidSeneviratne, S.-
item.creatorOrcidSneeuw, N.-
item.creatorOrcidvan Dam, T.-
item.creatorOrcidWouters, B.-
item.cerifentitytypePublications-
crisitem.author.deptGeodäsie und Ausgleichungsrechnung-
crisitem.author.orcid0000-0002-9087-1445-
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