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            <gco:CharacterString>The full&amp;#8208;hydrometeor four&amp;#8208;dimensional variational (4D&amp;#8208;Var) assimilation scheme in the Weather Research and Forecasting (WRF) model, based on the WRF single&amp;#8208;moment 6&amp;#8208;class microphysics scheme (WSM6), is utilized to assimilate precipitation data. The focus is on short&amp;#8208;term convective precipitation forecasts influenced by the Northeast China cold vortex (NCCV). Four assimilation experiments were designed to compare the warm rain scheme with the full&amp;#8208;hydrometeor scheme, as well as to examine the differences between assimilating hourly surface rain gauge data and multi&amp;#8208;source integrated precipitation products. Nine cases of intense convective precipitation related to NCCV were analyzed. The results demonstrate that the initial analysis of ice&amp;#8208;phase hydrometeors was satisfactory across the three experiments utilizing the full&amp;#8208;hydrometeor 4D&amp;#8208;Var assimilation scheme. The assimilation of precipitation data using the full&amp;#8208;hydrometeor scheme in WRF 4D&amp;#8208;Var effectively adjusted atmospheric thermodynamic properties and decreased model spin&amp;#8208;up time, leading to improved precipitation forecasts, especially for the 0&amp;#8211;3&amp;#160;hr period. Furthermore, the assimilation of rain gauge data or multi&amp;#8208;source integrated precipitation data has been demonstrated to be an effective approach for enhancing the accuracy of weather forecasts.</gco:CharacterString>
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