Abstract. Landslide is a major natural hazard in Kyrgyzstan and Tajikistan. Knowledge about atmospheric triggering conditions and climatic disposition of landslides in Kyrgyzstan and Tajikistan is limited, even though this topic has already been investigated thoroughly in other parts of the world. In this study, the newly developed, high-resolution High Asia Refined Analysis version 2 (HAR v2) data set generated by dynamical downscaling was combined with historical landslide inventories to analyze atmospheric conditions that initialized landslides in Kyrgyzstan and Tajikistan. The results indicate the crucial role of snowmelt in landslide triggering processes since it contributes to the initialization of 40 % of landslide events. Objective thresholds for rainfall, snowmelt, as well as the sum of rainfall and snowmelt (rainfall + snowmelt) were defined. Peak intensity (Imax) and accumulated amount (Q) of rainfall + snowmelt events yield the best predictive performance. Mean annual exceedance maps were derived from regional thresholds of Imax = 12.8 mm d−1 and Q = 17.2 mm for rainfall + snowmelt. Mean annual exceedance maps depict climatic disposition and have added value in landslide susceptibility mapping. The results reported in this study highlight the potential of dynamical downscaling products generated by regional climate models in landslide prediction.