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Harnessing C$_21$ and S$_21$ coefficients from GRACE and hybrid solutions for comprehensive analysis of polar motion excitation

Nastula, Jolanta, Sliwinska-Bronowicz, Justyna, and Winska, Ma&lstrokgorzata, 2025. Harnessing C$_21$ and S$_21$ coefficients from GRACE and hybrid solutions for comprehensive analysis of polar motion excitation. Journal of Geodesy, 99(6):48, doi:10.1007/s00190-025-01969-z.

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BibTeX

@ARTICLE{2025JGeod..99...48N,
       author = {{Nastula}, Jolanta and {{\'S}liwi{\'n}ska-Bronowicz}, Justyna and {Wi{\'n}ska}, Ma{\l}gorzata},
        title = "{Harnessing C$_{21}$ and S$_{21}$ coefficients from GRACE and hybrid solutions for comprehensive analysis of polar motion excitation}",
      journal = {Journal of Geodesy},
     keywords = {GRACE, GRACE-FO, SLR, Hybrid, Polar motion excitation},
         year = 2025,
        month = jun,
       volume = {99},
       number = {6},
          eid = {48},
        pages = {48},
     abstract = "{Hydrological angular momentum (HAM) is used to quantify the influence of
        mass changes in the continental hydrosphere on variations in
        polar motion. It has important applications in interpreting the
        connections between Earth system phenomena and perturbations in
        the rotation of the planet. In this study we analyse HAM series
        computed from various Gravity Recovery and Climate Experiment
        (GRACE) and GRACE Follow-On (GRACE-FO) solutions as well as from
        hybrid data based on satellite laser ranging (SLR) and a
        combination of GRACE/GRACE-FO and SLR. After decomposing the
        overall HAM time series into seasonal, non-seasonal short-term,
        and non-seasonal long-term variations, we evaluate them using
        hydrological signal in geodetically observed polar motion
        excitation (GAO) as a reference. The analyses are performed for
        two periods: (1) the period of highest quality of GRACE
        measurements and (2) the whole period of GRACE and GRACE-FO
        activity. We demonstrated a high level of correlation (equal to
        0.8 and higher) between GAO and all HAM series for non-seasonal
        long-term variations. For these variations, as well as for
        seasonal oscillations, the use of both single GRACE/GRACE-FO
        solutions and combined solutions achieve a similar level of
        agreement with GAO. The use of hybrid data improves this
        agreement for non-seasonal short-term variations.}",
          doi = {10.1007/s00190-025-01969-z},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGeod..99...48N},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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