Travel time: April
In April, Princeton undergoes a profound transformation as it bridges the gap between the freezing interior winter and the warm, dry Thompson-Okanagan summer. Located in the rain shadow of the Cascade Mountains, the climate here is significantly drier than the coastal regions, but April remains a period of thermal instability. You will experience the "high-country spring," where the valley floors begin to green even as the surrounding peaks retain their winter coat.
The most defining characteristic of Princeton's April weather is the dramatic daily temperature range. Because of the clear mountain air and valley geography, heat escapes rapidly at night.
April is a transitional month for moisture. While it is not the rainiest time of year (that title typically goes to June), it is a period of "mixed bag" precipitation.
Princeton is known for its wind patterns influenced by the narrow Similkameen and Tulameen valleys. In April, as the land warms, thermal winds often pick up in the late afternoon. These breezes are cooling and can make a sunny $13\text{°C}$ day feel much more brisk. Locals call this the "valley draw," where the air moves through the mountain gaps, keeping the humidity low and the air remarkably fresh.
Beyond the thermometer, April in Princeton feels very dry. The low relative humidity means that while the shade remains cool, the sun's intensity is high. Even on a cool day, the solar radiation at this elevation can feel quite powerful on your skin. Conversely, the "dry cold" of the evenings is sharp but lacks the damp, bone-chilling quality found on the coast, provided you are shielded from the wind.