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Abstract
This paper introduces a variational assimilation technique for the retrieval of wind elds from Doppler radar data. The assimilated information included both the radial velocity (RV) and the movement of radar echo. In this assimilation technique, the key is transforming the movement of radar echo to a new radar measuring variable -"apparent velocity"(AV). Thus, the information of wind is added, and the indeterminacy of recovering two-dimensional wind only by AV was overcome e ectively by combining RV with AV. By means
of CMA GRAPES-3Dvar and CINRAD data, some experiments were performed. The results show that the method of retrieval of wind fields is useful in obtaining the construction of the weather system.
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