Upper Colorado SnoWatch page |
Our West Slope watersheds start to show snowmelt at least a couple of weeks before our East Slope watersheds. This is counterintuitive since the West Slope watersheds are at a higher elevation. But solar radiation is a big driver of snowmelt activity, and West Slope watersheds have more southerly and westerly exposures than the East Slope.
Examples of low-elevation sites to watch are Stillwater Creek and Phantom Valley, both located in watersheds tributary to Lake Granby. Our Upper Colorado SnoWatch page tracks the action if you want to see it for yourself.