dc.contributor.author
Dahle, Christoph
dc.contributor.author
Sulzbach, Roman
dc.contributor.author
Murböck, Michael
dc.contributor.author
Flechtner, Frank
dc.contributor.author
Dobslaw, Henryk
dc.contributor.author
Michalak, Grzegorz
dc.contributor.author
Neumayer, Karl Hans
dc.contributor.author
Abrykosov, Oleh
dc.contributor.author
Reinhold, Anton
dc.contributor.author
König, Rolf
dc.contributor.author
Förste, Christoph
dc.date.accessioned
2019-10-25T08:26:03Z
dc.date.available
2019-10-25T08:26:03Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/25801
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-25562
dc.description.abstract
Time-variable gravity field models derived from observations of the Gravity Recovery and Climate Experiment (GRACE) mission, whose science operations phase ended in June 2017 after more than 15 years, enabled a multitude of studies of Earth’s surface mass transport processes and climate change. The German Research Centre for Geosciences (GFZ), routinely processing such monthly gravity fields as part of the GRACE Science Data System, has reprocessed the complete GRACE mission and released an improved GFZ GRACE RL06 monthly gravity field time series. This study provides an insight into the processing strategy of GFZ RL06 which has been considerably changed with respect to previous GFZ GRACE releases, and modifications relative to the precursor GFZ RL05a are described. The quality of the RL06 gravity field models is analyzed and discussed both in the spectral and spatial domain in comparison to the RL05a time series. All results indicate significant improvements of about 40% in terms of reduced noise. It is also shown that the GFZ RL06 time series is a step forward in terms of consistency, and that errors of the gravity field coefficients are more realistic. These findings are confirmed as well by independent validation of the monthly GRACE models, as done in this work by means of ocean bottom pressure in situ observations and orbit tests with the GOCE satellite. Thus, the GFZ GRACE RL06 time series allows for a better quantification of mass changes in the Earth system.
en
dc.format.extent
22 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
satellite gravimetry
en
dc.subject
Level-2 processing
en
dc.subject
time-variable gravity field
en
dc.subject
mass change monitoring
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::551 Geologie, Hydrologie, Meteorologie
dc.title
The GFZ GRACE RL06 monthly gravity field time series: Processing details and quality assessment
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.doi
10.3390/rs11182116
dcterms.bibliographicCitation.journaltitle
Remote sensing
dcterms.bibliographicCitation.number
18
dcterms.bibliographicCitation.volume
11
dcterms.bibliographicCitation.url
https://doi.org/10.3390/rs11182116
refubium.affiliation
Geowissenschaften
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.issn
2072-4292
dcterms.isPartOf.issn
2072-4292
refubium.resourceType.provider
WoS-Alert