The challenge of climate research : linking observations and models Part 2 : Atmospheric and Paleoclimatic studies
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averaged winter season systematic initial tendency errors for temperature tendencies [K/s] based on eight years (1982-89) of ERA assimilations using the slow normal mode insertion (SNMI) technique (uper cross section) and using the simple nudging technique (lower cross section). Figure 1 from the paper: Diagonsis of systematic initial tendency errors in an atmospheric AGCM using slow normal mode data assimilation of ECMWF reanalysis data.
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