A shifting hydrological regime : a field investigation of snowmelt runoff processes and their connection to summer baseflow, Sunshine Coast, B.C.
The annual hydrographs in British Columbia rivers are either characterized by glacial, nival, pluvial or “hybrid” (both pluvial and nival) sources of runoff. Climate change scenarios for the 2050s indicate that snow-water-equivalent (SWE) will diminish by 50 to 80% in lower snowfed-dominated basins...
| Main Author: | |
|---|---|
| Language: | English |
| Published: |
University of British Columbia
2011
|
| Online Access: | http://hdl.handle.net/2429/31299 |