Mica Creek Experimental Watershed

 
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Snow Deposition and Ablation Processes


Snow deposition and melt cycles in mountainous regions dominate hydrological processes in much of the western United States. Water stored in winter snowpacks represent a valuable commodity for wildland, agricultural, and direct human use. The timing and magnitude of snowmelt is therefore critical with regard to water quantity (water yield), and quality. Current work at the Mica Creek Experimental Watershed (MCEW) will lead to a better understanding of, a) climate alteration as influenced by variations in elevation, aspect, slope, and cover (e.g. clearcut/thinning), b) how current management practices impact snow deposition and melt processes with specific topographic attributes, and c) how harvest treatments influence snow deposition and ablation processes when influenced by persistent localized temperature inversions.

Primary Contacts: Jason Hubbart (web page), Tim Link (web page)

Snowmelt Time Lapse Photography for the 2006 Melt Season

 

MCEW Snowmelt - Current Snow Water Equivalent (SWE)

 

Figure. Current Snowmelt (SWE) at the Mica Creek Experimental Watershed (MCEW). Snow courses listed 1-14 (map <right click, save as>) relative to the Mica Creek SnoTel.
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