With a couple of possible weather events this coming week, wanted to get a sense of the snow surface. Two tours this weekend:
- 1/5/2013: Mid and upper Mineral Fork.
- 1/6/2013: Upper LCC/BCC.
I remain underwhelmed with the snowpack in Mineral. It is still generally thin, only exceeding a meter (~3') in the upper elevations. Pole plants still are easily identifying the facet/crust sandwiches buried 60-90 cms down in the snowpack. Lack of a slab with any energy is keeping dormant weak layers at bay in thinner snowpack areas. Was finding surface hoar down low in drainage bottoms.
Snowpack looks much better in the upper LCC and BCC drainages. Was interested in the snow surface as well as snow depths. Generally 1- 1.5 meters deep, although thinner in steep, rocky areas. Weak facets (.5 - 1 mm) in the top 10-30 cms of snow are prevalent in wind and sun sheltered areas. Beneath that the slab goes from 4F down to a stout 1F slab. Was not finding any surface hoar today, and the strong sun seems to have destroyed any faceted crystals from radiation recrystallization that I was finding on southerly aspects earlier this week.