| Figure 3a. | Hydrograph of Roberts Creek at Roberts Creek, a hydrometric station in a winter rainfall dominated zone characterized by high winter mean daily discharge. Note that the discharge scale is logarithmic. |
| Figure 3b. | Hydrograph of Cheakamus River above Millar Creek, a hydrometric station in a summer snowmelt dominated zone characterized by high summer mean daily discharge. Note that the discharge scale is logarithmic. |
| Figure 3c. | Hydrograph of Oyster River below Woodhus Creek, a hydrometric station in a transitional zone that is characterized by both high summer mean daily discharge, due to snowmelt, and high winter mean daily discharge, due to rainfall. Note that the discharge scale is logarithmic. |