Measuring drought is a complex process, particularly in mountain regions due to their geographic diversity and complex regional microclimates. Drought is commonly subdivided into meteorological drought (rainfall deficit), soil moisture drought (below-normal soil moisture levels), and hydrological drought (below-normal (sub)surface water availability), where “normal” defined by a percentile of the climatology of the variable of interest, and frequency, severity and duration of drought events evaluated. Analysis of previous droughts in British Columbia (BC) indicates that there are three major factors involved with drought occurrence: low winter snow accumulation, spring weather, and summer weather. For drought to occur, often two of the three factors need to exist. The BC Drought Response Plan is organized around four successive levels (Levels 1-4) of drought. BC’s drought indicators refer to the causative factors (snow conditions, spring and summer precipitation, preceding drought) and the resultant factors (stream flow, lake and reservoir levels). Aquifer (groundwater) levels are supplemental indicators, although there are no associated quantitative thresholds.