Abstract
In order to analyse spatio-temporal variations of surface mass anomalies induced by hydrological mass redistributions at the Earth’s surface we use products from the Gravity Recovery and Climate Experiment (GRACE) satellite mission as well as global hydrological models. As a novelty we identify dominant periodic patterns that are not restricted to the fundamental annual frequency and its overtones, using a method that combines conventional Principal Components Analysis (PCA) with a determination of sine waves of arbitrary periods from the principal components. We assess the significance of the derived spectra taking into account correlated errors of the GRACE data by means of a Monte-Carlo technique. This allows us to create filtered GRACE time series including only the significant terms, which serve for basin-specific calibration of hydrological models with respect to the dominant periodic water storage variations.
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Acknowledgments
The German Ministry of Education and Research (BMBF) supported these investigations within the geoscientific R+D programme GEOTECHNOLOGIEN “Erfassung des Systems Erde aus dem Weltraum” under grant 03F0424A. We thank P.C.D. Milly, Y. Fan and H. van den Dool, M. Rodell as well as P. Döll and J. Alcamo for providing the LaD, H96, GLDAS and WGHM model data, respectively. Thanks also go to D.W. Pierce for his Empirical Orthogonal Functions (EOF) software.
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Petrovic, S., Braun, R., Barthelmes, F., Wünsch, J., Kusche, J., Hengst, R. (2010). Surface Mass Variability from GRACE and Hydrological Models : Characteristic Periods and the Reconstruction of Significant Signals . In: Flechtner, F., et al. System Earth via Geodetic-Geophysical Space Techniques. Advanced Technologies in Earth Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-10228-8_32
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DOI: https://doi.org/10.1007/978-3-642-10228-8_32
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