We adhere to the surface condition and aloft condition data temps, and if precip is indicated in the METAR, we also depict it accordingly. With +TSRA for example it is common to see heavy rain under and in cloud, with hail possible under the anvil section depending on tstorm intensity and height, other moisture and stability conditions parameters, and some randomness.
Did you expect snow or hail?
Rain doesn't necessarily freeze at 0C. 0C is more of a melting point vs. a freezing point when it comes to icing/freezing of visible moisture. Freezing requires nuclei (small particles, ice crystals, etc.) and when it doesn't freeze you have supercooled water droplets, water not frozen but below 0C. The most dangerous kind is called SLD (supercooled large droplets) and is very common within thunderstorms. This non-frozen water begins to freeze quickly when it contacts the airplane (now having something to freeze to) causing severe icing that runs back over the wing and control surfaces.
It's not until below -40C that supercooled water droplets will certainly freeze without surrfaces/external nuclei. Below -15C there begins to be more frozen ice crystals vs. supercooled water droplets but the unfrozen water still exists.
tl;dr: This is normal and expected, and realistic and dangerous aspect of aviation weather that should be avoided. See
https://www.skybrary.aero/index.php/Supercooled_Water_Droplets