We explore how atmospheric rivers (ARs) in a summer and a winter case interact with the topography of the Amundsen Sea Embayment, West Antarctica, and deposit significant amounts of precipitation. To do this we use results from three regional climate models (RCMs: MetUM, Polar-WRF, HCLIM) at a spatial resolution of 1 km. Estimates of snowfall associated with both these events from all three RCM simulations compare well against observed snow height measurements over the Thwaites and Pine Island ice shelves. By contrast, snowfall estimates from ERA5 reanalysis for both events are severely underestimated compared to the measurements. Outputs from the RCMs also show that the ARs may be associated with several millimeters of rain in both the summer and winter cases, although in the absence of <em>in situ</em> measurements of rainfall, this result cannot be directly verified. The RCM simulations suggest that the rainfall during these events can fall directly as supercooled drizzle, but also that rainfall is concentrated around steep terrain due to the interaction of ARs with complex orography. We also show that while the amount of RCM-simulated snowfall was comparatively resolution insensitive, the amount of rainfall simulated was not, with rainfall amounts much higher in 1 km simulations compared to 12 km simulations. Our work highlights that kilometer-scale models are useful tools to investigate the total precipitation amount and its partitioning into rain and snow over this globally important and climatically sensitive region, as well as the critical need for <em>in situ</em> observations of rainfall.