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Lan, Wen-Hau, Lee, Chi-Ming, Kuo, Chung-Yen, Lin, Li-Ching, and Handoko, Eko Yuli, 2025. Regional sea level budget around Taiwan and Philippines over 2002‒2021 inferred from GRACE, altimetry, and in-situ hydrographic data: Regional sea level budget around Taiwan and Philippines\textellipsis. Journal of Geodesy, 99(1):5, doi:10.1007/s00190-024-01928-0.
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@ARTICLE{2025JGeod..99....5L,
author = {{Lan}, Wen-Hau and {Lee}, Chi-Ming and {Kuo}, Chung-Yen and {Lin}, Li-Ching and {Handoko}, Eko Yuli},
title = "{Regional sea level budget around Taiwan and Philippines over 2002â2021 inferred from GRACE, altimetry, and in-situ hydrographic data: Regional sea level budget around Taiwan and Philippines{\textellipsis}}",
journal = {Journal of Geodesy},
keywords = {Sea level budget, Satellite altimetry, GRACE, In-situ hydrographic data, Earth Sciences, Oceanography},
year = 2025,
month = jan,
volume = {99},
number = {1},
eid = {5},
pages = {5},
abstract = "{The regional sea level budget and interannual sea level changes around
Taiwan and Philippines are studied using altimetry, GRACE, and
in-situ hydrographic data during 1993â2021. Results show that
the average sea level trend around Taiwan and Philippines during
1993{\textendash}2021 derived from the altimetric data is 3.6
{\ensuremath{\pm}} 0.2 mm/yr. Over 2002{\textendash}2021, the
study shows closure of sea level budget in the eastern ocean of
Taiwan and Philippines within the observed data uncertainties,
and the ocean mass accounts for 88\%{\textendash}100\% of the
observed sea level rise. In contrast, the sea level budget is
not closed in the western ocean of Taiwan and Philippines,
probably due to the lack of complete coverage by in-situ ocean
observing systems. In addition, both regional sea level
anomalies and their steric component around Taiwan and
Philippines exhibit pronounced interannual and decadal
variabilities. The trade wind stress associated with El
Ni{\~n}o{\textendash}Southern Oscillation and Pacific Decadal
Oscillation offers a compelling explanation for the interannual
and decadal signals of sea level anomalies in the southern ocean
of Taiwan, with negative correlations of â 0.78 to â 0.64,
indicating that trade wind stress makes a negative contribution
to interannual-to-decadal sea level variability. In the
northwestern ocean of Taiwan, the sea level variation is
strongly influenced by the local monsoon system and shallow
bathymetry with an annual amplitude of 90.3 {\ensuremath{\pm}}
2.9 mm, larger than those in other regions around Taiwan and
Philippines, where ocean mass is dominant with a high
correlation with the sea level (+ 0.75 to + 0.78).}",
doi = {10.1007/s00190-024-01928-0},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGeod..99....5L},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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