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) approach. The vertical localization is configured to force the covariances to 0 at a distance of (a) 2, (b) 4, or (c) 100 scale heights. Fig . 2. As in Fig. 1 , but for a single observation of AMSU-A channel 10. Fig . 3. The analysis increment of temperature from assimilating either (a) the full set of AMSU-A channels (4–10) at the same location used for Figs. 1 and 2 or (b) the vertical profile of temperature observations from a
) approach. The vertical localization is configured to force the covariances to 0 at a distance of (a) 2, (b) 4, or (c) 100 scale heights. Fig . 2. As in Fig. 1 , but for a single observation of AMSU-A channel 10. Fig . 3. The analysis increment of temperature from assimilating either (a) the full set of AMSU-A channels (4–10) at the same location used for Figs. 1 and 2 or (b) the vertical profile of temperature observations from a
