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Mark Buehner, P. L. Houtekamer, Cecilien Charette, Herschel L. Mitchell, and Bin He

. These observations are typically related to temperature and/or humidity over many vertical levels as modeled by a radiative transfer model. Without covariance localization and assuming the observation is linearly related to the analysis vector, the analysis increment from using the EnKF to assimilate a single observation is proportional to 𝗕 ens h T , where 𝗕 ens is the sample covariance matrix computed from the EnKF ensemble and h is a row vector corresponding to the observation operator

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