By Annah Young, graduate student in the Institute’s 15th cohort.
I wedged myself between two boulders on the summit of Silver Star Mountain in Okanagan County, Washington and peered out over the North Cascades range. It was May 1, 2016. Mount Baker was crystal clear some 100 miles to the west across the snow cover peaks. The mountains were shimmering, almost blindingly so, in all directions with miles and miles of snowfields. The day was hot, almost 60 degrees in the sun at an elevation of 8,875 feet. Our ski boots were standing on a snowpack of over 8 feet deep I was trying to fathom the amount of frozen water surrounding me. Looking to the east I saw the Methow Valley and Okanagan County expanding into the horizon and tried to imagine the journey that the water molecules beneath my feet will make, providing habitat for migrating steelhead trout, nourishing Cottonwoods, and irrigating crops that become food to nourish the people. I chugged the last bit of water that was in my Nalgene, filled it to the brim with snow, stuffed the bottle in my pack and skied down 5,000 feet of glorious spring corn snow.
Snowpack in the North Cascades has declined between 20% and 40% since 1950 (Stoelinda, Albright, Mass, 2009, p. 1). Snowpack in the mountains is stored water that provides life to all organisms including humans by irrigating and growing the food we eat. Snowpack is declining due to natural climate fluctuations and anthropogenic global warming.