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Hi Andreas, I guess to be consistent with icgem it's probably best to get the scaling coefficients from https://github.com/strawpants/GRACE-filter and use these in a lookup table in Line 225 in 85f6202 All the best,, Roelof |
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Following a discussion in #4, the DDK filter definition was changed to follow the implementation as used by ICGEM (http://icgem.gfz-potsdam.de) and the power laws given in https://github.com/strawpants/GRACE-filter/.
These deviate from the original power law progression in Kusche (2007) and Kusche et al. (2009), which are now available in the DDKGeneric class.
Cheers,
Andreas
Kusche, J. Approximate decorrelation and non-isotropic smoothing of time-variable GRACE-type gravity field models. J Geod 81, 733–749 (2007). https://doi.org/10.1007/s00190-007-0143-3
Kusche, J., Schmidt, R., Petrovic, S. et al. Decorrelated GRACE time-variable gravity solutions by GFZ, and their validation using a hydrological model. J Geod 83, 903–913 (2009). https://doi.org/10.1007/s00190-009-0308-3
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