A Multiresolution Technique for the Classification of Precipitation Echoes in Radar Data

A new method for separating convective, intermediate, and stratiform rainfall based on the wavelet scale analysis is presented. A robust classification has resulted from the two choices: 1) the transformation of radar reflectivities to rain rates and 2) the inclusion of the intermediate class. The method uses á trous wavelet transform (WT) to separate heterogeneous convective features from the relatively smooth stratiform field. The heterogeneous region is further split into a convective class for the large wavelet coefficients and an intermediate class for the small wavelet coefficients. There is an improvement in the estimation of convective-stratiform fraction and frequency distribution of rain rates in comparison to the wellestablished Steiner method. The new method correctly reclassified a significant fraction of Steiner's convective regions, which had low mean rain rates of 5.5 mm · h
^-1
, as stratiform regions. Similarly, Steiner's stratiform regions, which had high mean rain rates of 15 mm · h
^-1
, are classified as convective by the wavelet method. The method is tested and evaluated over the Indian region during monsoon, and it is found that the three wavelet classes have distinct raindrop-size distributions.