In an effort to improve the snowfall situation in the Wasatch Range, I have left Utah for the rest of the cool season.
I'm serving as a guest professor at the University of Innsbruck for their so-called summer semester, which actually runs from March to June. We arrived here on Wednesday. It's been mild and sunny here with high temperatures above 10°C (no °F here) in Innsbruck each day. Today I skied with some friends at Stubai Glacier, which reaches over 3000 meters elevation, to escape the heat. It was a spectacular day.
Like Utah, Austria has had a largely crap snow season and the current warm spell isn't helping. The snowpack on south aspects is pretty much non-existent below 1500 meters and in some areas much higher than that. The snowpack is meager where it exists, even at the highest elevations. Glacier-mounted lift towers today were on large domes of ice. These are usually covered with white blankets (I'm not sure why they are missing currently) to reduce melt. I was wondering if their height at least partially reflects the lack of seasonal snowfall at upper elevations.
I'm teaching graduate course on cool-season precipitation processes and prediction starting on Monday and helping with a weather briefing course which enables me to learn more about Alpine and European meteorology.
Hoping to provide updates from time to time and that in my absence the "Steenburgh Effect" proves productive for Wasatch powder skiing.