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Diagnosing observation error correlations for Doppler radar radial winds in the Met Office UKV model using observation-minus-background and observation-minus-analysis statistics

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Figure

Figure 10 shows that the correlation length scale in- in-creases with range. Again this is likely to be a result of the larger measurement volumes at far range.
Table 2 shows that the average standard deviation for this case is very similar to that of case 1

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