The cloud microphysical properties of a stratiform cloud in Shanxi on 27 May 2010 were analyzed based on the airbrone DMT probes and Parsivel laser precipitation particle spectrometer.The results showed that the vertical and horizontal structure of clouds was uneven.The maximum concentration values sampled by CDP and CIP were 165.20 cm^-3 and 1.08 cm^-3 respectively.Average value of microphysical features of surface raindrops indicated that it was a typical stratiform cloud precipitation.Rainfall intensity is mostly decided by raindrop concentration.Temporal distribution of raindrop microphysical parameters was not even.The correlations between the rainfall intensity(I) and the radar reflectivity(Z),the rainwater content(W),the raindrop concentration(N),parameter N₀ and parameter λ were established.There was a very good correlation between I and Z and W,but N、parameter N₀ and parameter λ were poorly correlated to I.The surface raindrop size distributions were narrower and steeper than the upper raindrop size distributions.The precipitation was the coexistence of cold cloud and warm cloud precipitation.