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  • Similar pattern is seen between the analysis increments for SWE in (1) the 2D-OI and (2) the SEKF.
  • Note that large differences are seen in some regions due to inconsistency of snow density between the 2D-OI analysis and trajectory (lower limit of 100kg/m3 in the 2D-OI but 50kg/m3 in the model).
  • When SWE from the 2D-OI is assimilated directly in the SEKF (3), such differences are not seen.
    • The trial branch: dako_CY48R1.1_SEKF_tmp

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