Monthly anomalies are derived by subtraction of a deterministic signal model (bias, trend, annual and semi-annual variations)
from the monthly solutions. The signal model is the COST-G GRACE+GRACE-FO FSM, which is based on COST-G GRACE RL01 and COST-G GRACE-FO RL02.
For each spherical harmonic coefficient an individual model is fitted.
For comparisons in the spherical harmonic domain no filter is applied. Low degree anomalies are dominated by
residual signal content (non-seasonal hydrology), while the higher degree anomalies are dominated by noise.
The accuracy assessment (errors) of the combined solutions is derived empirically from the differences to the individual
gontributions.