Dry to really, really dry

The Okanagan Basin is dry because it lies in the rain shadow of the Coast Mountains. This high mountain chain strips moisture from Pacific storms, leaving little for the basin. The farther south you go, the drier it gets. Cacti grow in the Okanagan Basin!

Our upland snow catchers

Most water enters the Okanagan Basin as winter snow on the highlands. During the spring, snowmelt infiltrates into the ground or flows in streams to highland reservoirs and valley lakes.

White Lake, west of Okanagan Falls, completely evaporates in summer, leaving behind a dry lake floor of white mineral salts. (R.J.W. Turner, GSC 2006-150)

The Okanagan River at Penticton. This is the main river of the Okanagan Valley. Not very big! (R.J.W. Turner, GSC 2006-151)

Highland snowpack along road to Big White ski area east of Kelowna (R.J.W. Turner, GSC 2006-149)

We lose most of what we get

Only 15% of the rain and snow that falls in the basin flows to our lakes and remains there. The rest leaves the basin through transpiration from forests and crops, and evaporation from lakes.