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Proceedings of the 2004 ISSW,
Doug Chabot

By Doug Chabot.  Poster presented at the 2004 ISSW, and published in the Proceedings of the 2004 ISSW, Jackson, Wyoming.

Proceedings of the 2002 ISSW,
jimurl

By Ron Johnson and Karl Birkeland. Paper presented at the 2002 ISSW, and published in the Proceedings of the 2002 ISSW, Penticton, British Columbia.

Proceedings of the 2002 ISSW,
Doug Chabot

By Doug Chabot. Paper presented at the 2002 ISSW, and published in the Proceedings of the 2002 ISSW, Penticton, British Columbia.

The Avalanche Review,
Doug Chabot

A few years ago I was climbing in the Alaska Range. My partner and I were stuck 26 pitches up the first ascent of a mixed face five days into a seven-day storm. As I looked down the face covered with rockbands, couloirs and pockets of snow....

Proceedings of the 1998 ISSW,
jimurl

A Comparison Study of the Shredblock and Rutschblock Snow Stablility Tests by Andy Gleason. Presented at the 1998 ISSW, and to be published in the Proceedings of the 1998 ISSW, Sunriver, Oregon.

The Shredblock test is a field test to measure the relative instability of the snowpack in a backcountry setting with minimal equipment. The Shredblock test is based on the Rutschblock test but uses a snowboard instead of skis to load an isolated column of snow.

Methods

Proceedings of the 1998 ISSW,
jimurl

By Karl Birkeland. Paper presented at the 1998 ISSW, and to be published in the Proceedings of the 1998 ISSW, Sunriver, Oregon.

Cyberspace Snow and Avalanche Center,
jimurl

Karl Birkeland1, Ron Johnson2, and Scott Schmidt3

Abstract

Mountain Research and Development,
jimurl

By Karl Birkeland and Cary Mock. Published in 1996 in Mountain Research and Development, 16(3), 281-286.

Eric Knoff

 

From the time snow crystals fall from the sky to time they melt in the spring, the shape and structure of each crystal never stops changing. This is known as snow metamorphism. 

Snow metamorphism determines if individual snow crystals are rounding (becoming stronger) or faceting (becoming weaker). The relationship between snow crystals ultimately dictates what kind of layer, strong or weak, is formed. The interaction between individual layers determines snowpack stability.

Doug Chabot

Published in December issue of CARVE

I never thought I’d be concerned about my electronics while cruising around the backcountry, but I am. Carrying a cell phone, satellite phone, GPS, avalanche beacon, SPOT Messenger, and a VHF radio means my electronic signature rivals a high tension power line. I hope I don’t have to start lugging around a car battery to keep everything powered. Most people in the backcountry are not as wired as me, but a smartphone and beacon are staples for most backcountry travelers. The beacon is a literal lifeline, the most important piece of electronic safety equipment we carry. Its function is crucial to survival. As I slowly added to my electronic arsenal over the years I began to wonder, “Do all these other devices interfere with the function of my avalanche beacon?”