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Wang, Songyun, Wilson, Clark R., Chen, Jianli, and Seo, Ki-Weon, 2025. Annual polar motion and its variability. Journal of Geodesy, 99(7):57, doi:10.1007/s00190-025-01982-2.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025JGeod..99...57W, author = {{Wang}, Songyun and {Wilson}, Clark R. and {Chen}, Jianli and {Seo}, Ki-Weon}, title = "{Annual polar motion and its variability}", journal = {Journal of Geodesy}, keywords = {Polar motion excitation, Earth rotation, GRACE, GRACE Follow-on, SLR, Annual amplitude modulation, Earth Sciences, Oceanography, Engineering, Geomatic Engineering}, year = 2025, month = jul, volume = {99}, number = {7}, eid = {57}, pages = {57}, abstract = "{The annual component is the largest signal in polar motion excitation, with contributions from changes in mass distribution and motion in the atmosphere, oceans, land hydrology and cryosphere. For the period 2002-2023, we examine available estimates and combinations of various contributions to polar motion excitation from data-assimilating numerical models of the atmosphere, oceans, and land hydrology and from satellite gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) \& GRACE Follow-On (GRACE-FO) and Satellite Laser Ranging (SLR). We compare observed annual polar motion with combinations of estimates using a metric that considers both differences in average annual behavior and differences in modulation of the annual component over time. Using this metric, we identify a preferred combination of estimates (National Centers for Environmental Prediction (NCEP) for the atmosphere, Max-Planck-Institute for Meteorology Ocean Model (MPIOM) for the oceans, and GRACE/GRACE-FO satellite gravity observations for land hydrology). Analyzing the average annual variation with its variability over time provides a framework to understand both the amplitude modulation and the distinct pro- and retrograde behaviors of the annual excitation. The persistently smaller retrograde annual excitation is primarily due to out-of-phase atmospheric and oceanic excitations.}", doi = {10.1007/s00190-025-01982-2}, adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGeod..99...57W}, adsnote = {Provided by the SAO/NASA Astrophysics Data System} }
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