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dc.identifier.uri http://dx.doi.org/10.15488/14075
dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/14189
dc.contributor.author Koch, Igor
dc.contributor.author Flury, Jakob
dc.contributor.author Naeimi, Majid
dc.contributor.author Shabanloui, Akbar
dc.contributor.editor Freymueller, Jeffrey T.
dc.contributor.editor Sánchez, Laura
dc.date.accessioned 2023-07-03T05:51:58Z
dc.date.available 2023-07-03T05:51:58Z
dc.date.issued 2020
dc.identifier.citation Koch, I.; Flury, J.; Naeimi, M.; Shabanloui, A.: LUH-GRACE2018. In: Freymueller, J.T.; Sánchez, L. (Eds.): Beyond 100 : the next century in geodesy. Berlin ; Heidelberg : Springer, 2023 (International Association of Geodesy symposia ; 152), S. 67-75. DOI: https://doi.org/10.1007/1345_2020_92
dc.description.abstract In this contribution, we present the LUH-GRACE2018 time series of monthly gravity field solutions covering the period January 2003–March 2016. The solutions are obtained from GRACE K-Band Range Rate (KBRR) measurements as main observations. The monthly solutions are computed using the in-house developed GRACE-SIGMA software. The processing is based on dynamic orbit and gravity field determination using variational equations and consists of two main steps. In the first step, 3-hourly orbital arcs of the two satellites and the state transition and sensitivity matrices are dynamically integrated using a modified Gauss-Jackson integrator. In this step, initial state vectors and 3D accelerometer bias parameters are adjusted using GRACE Level-1B reduced-dynamic positions as observations. In the second step, normal equations are accumulated and the normalized spherical harmonic coefficients up to degree and order 80 are estimated along with arc-wise initial states, accelerometer biases and empirical KBRR parameters. Here KBRR measurements are used as main observations and reduced-dynamic positions are introduced to solve for the low frequency coefficients. In terms of error degree standard deviations as well as Equivalent Water Heights (EWH), our gravity field solutions agree well with RL05 solutions of CSR, GFZ and JPL. eng
dc.language.iso eng
dc.publisher Berlin ; Heidelberg : Springer
dc.relation.ispartof Beyond 100 : the next century in geodesy ; proceedings of the IAG General Assembly, Montreal, Canada, July 8-18, 2019
dc.relation.ispartofseries International Association of Geodesy symposia ; 152 152 (2023)
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0
dc.subject GRACE eng
dc.subject GRACE Follow-On eng
dc.subject Gravity field recovery eng
dc.subject Time-variable gravity field eng
dc.subject.classification Konferenzschrift ger]
dc.subject.ddc 550 | Geowissenschaften
dc.title LUH-GRACE2018 eng
dc.type BookPart
dc.type Text
dc.relation.essn 2197-9359
dc.relation.isbn 978-3-031-09856-7
dc.relation.isbn 3-031-09856-0
dc.relation.isbn 978-3-031-09857-4
dc.relation.isbn 978-3-031-09859-8
dc.relation.issn 0939-9585
dc.relation.doi https://doi.org/10.1007/1345_2020_92
dc.bibliographicCitation.volume 152
dc.bibliographicCitation.date 2023
dc.bibliographicCitation.firstPage 67
dc.bibliographicCitation.lastPage 75
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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