Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions

Autores
Nastula, J.; Sliwiska-Bronowicz, J.; Wi«ska, M.
Año de publicación
2025
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
Hydrological angular momentum (HAM) is used to quantify the effect of mass changes in the continental hydrosphere on variations in polar motion (PM). It plays a key role in understanding the links between Earth system processes and changes in the planet’s rotation. In this study, we analyze HAM time series computed from various Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) solutions, satellite laser ranging (SLR) data, as well as hybrid datasets combining SLR. and GRACE/GRACE-FO solutions. Our results show that most HAM series derived from hybrid solutions closely match the hydrological signal observed in geodetic PM excitation (GAO). HAM derived from hybrid solutions generally performs similarly to, or better than the series based on single GRACE/GRACE-FO or SLR. solutions. For seasonal oscillations, the agreement between HAM and GAO is similar for both combined and single-technique solutions, while hybrid datasets show greater consistency in the non-seasonal spectral band. We find strong correlations between GAO and HAM from combined solutions for non-seasonal short-term variations (around 0.6) and non-seasonal long-term variations (around 0.9). These results highlight the significant potential of hybrid data for analyzing PM excitation, especially in the non-seasonal spectral band. The undeniable advantage of hybrid solutions compared to GRACE/GRACE-FO data is their significantly longer observation time series and the fact that their quality does not experience periodic declines as significant as those observed for GRACE/GRACE-FO.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Ciencias Astronómicas
Hydrological Angular Momentum (HAM)
Polar Motion Excitation
GRACE/GRACE-FO
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-nd/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/192027

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spelling Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutionsNastula, J.Sliwiska-Bronowicz, J.Wi«ska, M.Ciencias AstronómicasHydrological Angular Momentum (HAM)Polar Motion ExcitationGRACE/GRACE-FOHydrological angular momentum (HAM) is used to quantify the effect of mass changes in the continental hydrosphere on variations in polar motion (PM). It plays a key role in understanding the links between Earth system processes and changes in the planet’s rotation. In this study, we analyze HAM time series computed from various Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) solutions, satellite laser ranging (SLR) data, as well as hybrid datasets combining SLR. and GRACE/GRACE-FO solutions. Our results show that most HAM series derived from hybrid solutions closely match the hydrological signal observed in geodetic PM excitation (GAO). HAM derived from hybrid solutions generally performs similarly to, or better than the series based on single GRACE/GRACE-FO or SLR. solutions. For seasonal oscillations, the agreement between HAM and GAO is similar for both combined and single-technique solutions, while hybrid datasets show greater consistency in the non-seasonal spectral band. We find strong correlations between GAO and HAM from combined solutions for non-seasonal short-term variations (around 0.6) and non-seasonal long-term variations (around 0.9). These results highlight the significant potential of hybrid data for analyzing PM excitation, especially in the non-seasonal spectral band. The undeniable advantage of hybrid solutions compared to GRACE/GRACE-FO data is their significantly longer observation time series and the fact that their quality does not experience periodic declines as significant as those observed for GRACE/GRACE-FO.Facultad de Ciencias Astronómicas y Geofísicas2025-08info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionResumenhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/192027enginfo:eu-repo/semantics/reference/url/https://sedici.unlp.edu.ar/handle/10915/190232info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-nd/4.0/Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-03-26T09:21:46Zoai:sedici.unlp.edu.ar:10915/192027Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-03-26 09:21:46.988SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
title Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
spellingShingle Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
Nastula, J.
Ciencias Astronómicas
Hydrological Angular Momentum (HAM)
Polar Motion Excitation
GRACE/GRACE-FO
title_short Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
title_full Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
title_fullStr Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
title_full_unstemmed Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
title_sort Analysis of polar motion excitation using C21 and S21 coefficients from GRACE, SLR and hybrid solutions
dc.creator.none.fl_str_mv Nastula, J.
Sliwiska-Bronowicz, J.
Wi«ska, M.
author Nastula, J.
author_facet Nastula, J.
Sliwiska-Bronowicz, J.
Wi«ska, M.
author_role author
author2 Sliwiska-Bronowicz, J.
Wi«ska, M.
author2_role author
author
dc.subject.none.fl_str_mv Ciencias Astronómicas
Hydrological Angular Momentum (HAM)
Polar Motion Excitation
GRACE/GRACE-FO
topic Ciencias Astronómicas
Hydrological Angular Momentum (HAM)
Polar Motion Excitation
GRACE/GRACE-FO
dc.description.none.fl_txt_mv Hydrological angular momentum (HAM) is used to quantify the effect of mass changes in the continental hydrosphere on variations in polar motion (PM). It plays a key role in understanding the links between Earth system processes and changes in the planet’s rotation. In this study, we analyze HAM time series computed from various Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) solutions, satellite laser ranging (SLR) data, as well as hybrid datasets combining SLR. and GRACE/GRACE-FO solutions. Our results show that most HAM series derived from hybrid solutions closely match the hydrological signal observed in geodetic PM excitation (GAO). HAM derived from hybrid solutions generally performs similarly to, or better than the series based on single GRACE/GRACE-FO or SLR. solutions. For seasonal oscillations, the agreement between HAM and GAO is similar for both combined and single-technique solutions, while hybrid datasets show greater consistency in the non-seasonal spectral band. We find strong correlations between GAO and HAM from combined solutions for non-seasonal short-term variations (around 0.6) and non-seasonal long-term variations (around 0.9). These results highlight the significant potential of hybrid data for analyzing PM excitation, especially in the non-seasonal spectral band. The undeniable advantage of hybrid solutions compared to GRACE/GRACE-FO data is their significantly longer observation time series and the fact that their quality does not experience periodic declines as significant as those observed for GRACE/GRACE-FO.
Facultad de Ciencias Astronómicas y Geofísicas
description Hydrological angular momentum (HAM) is used to quantify the effect of mass changes in the continental hydrosphere on variations in polar motion (PM). It plays a key role in understanding the links between Earth system processes and changes in the planet’s rotation. In this study, we analyze HAM time series computed from various Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) solutions, satellite laser ranging (SLR) data, as well as hybrid datasets combining SLR. and GRACE/GRACE-FO solutions. Our results show that most HAM series derived from hybrid solutions closely match the hydrological signal observed in geodetic PM excitation (GAO). HAM derived from hybrid solutions generally performs similarly to, or better than the series based on single GRACE/GRACE-FO or SLR. solutions. For seasonal oscillations, the agreement between HAM and GAO is similar for both combined and single-technique solutions, while hybrid datasets show greater consistency in the non-seasonal spectral band. We find strong correlations between GAO and HAM from combined solutions for non-seasonal short-term variations (around 0.6) and non-seasonal long-term variations (around 0.9). These results highlight the significant potential of hybrid data for analyzing PM excitation, especially in the non-seasonal spectral band. The undeniable advantage of hybrid solutions compared to GRACE/GRACE-FO data is their significantly longer observation time series and the fact that their quality does not experience periodic declines as significant as those observed for GRACE/GRACE-FO.
publishDate 2025
dc.date.none.fl_str_mv 2025-08
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Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
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