Advances in Geodesy and Geoinformation, cilt.71, sa.2, ss.1-15, 2022 (ESCI)
This study discusses how to model the noise in a Gravity Recovery
and Climate Experiment (GRACE)-Mascon derived Equivalent Water Thicknesses
(EWT) time-series. GRACE has provided unique information for monitoring
variations in EWT of continents in regional or basin scale since 2002. To
analyze a GRACE EWT time-series, a standard harmonic regression model is used,
but usually assuming white noise-only stochastic model. However, like almost
all kinds of geodetic time-series, it has been shown that the GRACE EWT
time-series contains temporal correlations causing colored noise in the data.
As well known in geodetic modelling studies, neglecting these correlations
leads to underestimating the uncertainties, and so misinterpreting the
significancy of the parameter estimates such as trend rate, amplitudes of
signals etc. In this study, autoregressive noise modeling, which has some
advantageous compared to the approaches and methods frequently applied in
geodetic studies, is considered for GRACE EWT time series. For this aim, three
important basins, namely theYangtze, Murray–Darling and Amazon basins have been
examined. Among some applied autoregressive models, the ARMA(1,1) model is
obtained as the best-fitting noise model for analyzing the EWT changes in each
basin. The obtained results are discussed in terms of forecasting, significancy
and consistency with GRACE-FO mission.