The National Weather Service Forecasts-

TODAY...LOCALLY WINDY. MOSTLY SUNNY. HIGHS AROUND 32. NORTHEAST
WIND 15 TO 25 MPH. WIND GUSTS AROUND 45 MPH NEAR DOWNTOWN JUNEAU AND DOUGLAS DIMINISHING IN THE AFTERNOON.

TONIGHT...CLEAR. LOWS 16 TO 23...RANGING TO AROUND 12 IN WIND
SHELTERED AREAS. NORTHEAST WIND 10 TO 20 MPH DIMINISHING LATE.

THURSDAY...SUNNY. HIGHS AROUND 28. NORTHEAST WIND 10 MPH.

The snowpack in the region continues to remain stable. The current cold weather and dry conditions in the region are keeping conditions fairly constant.

Avalanche danger will remain low until there is a significant change in the weather.

We will continue to see moderate TAKU wind activity but with essentially no snow available for transport avalanche danger will remain low.

Weak Interface:

A poor bond between two adjacent layers of snow.

Weak Interface:

Usually, avalanches fracture within a discrete weak layer but occasionally, the fracture can form along a thin boundary between two stronger layers. A common example is when a slab slides on an ice crust. Also see ?weak layer?.

Fracture

Fracture is the process of crack propagation. When fracture occurs in a layer of snow underneath a slab sitting on a steep slope, a slab avalanche will occur.

How Snow Fails and fractures:

Avalanches don't \"strike without warning\", as we so often read in the press. They are only the most spectacularly visible event in a long series of precursors leading up to the grand finale.

It all begins many hours--or even days--before, usually when new snow or wind-blown snow begins to pile weight on top of a buried weak layer. Added weight causes the underlying snow to deform; rapidly added weight causes snow to rapidly deform. On an inclined slope, the deformation tends to concentrate within buried weak layers in the form of shear.
Inside of a weak-layer under stress, we can think of this as a race between bonds being broken and bonds being re-formed. Let's look at three different rates of deformation, slow medium and fast:

Slow deformation rate
If the weak-layer deforms slowly, it either deforms the bonds between the ice grains or more bonds form than break. This means that the weak-layer adjust to its load and actually gains strength. Snow can lazily drape over the terrain like a cat draped over the back of the couch?like a limp rubber band?and if you?ve every tried to cut a limp rubber band with a knife, you know what a stable snowpack is like.

Medium deformation rate
With an increasing rate of deformation, we reach a point where nearly as many crystalline bonds break as form and the strength of the weak layer remains about the same. With sensitive microphones we can actually hear the rupture of individual bonds between the ice grains, like the sound of slowly ripping Velcro.

Rapid deformation rate
If deformation occurs too rapidly--past a critical threshold--then more bonds break than form. The weak-layer inexorably looses strength and begins the slippery slide towards disaster. We call this \"failure\"--when the snow begins to progressively loose strength. We also call this \"strain softening.\" To understand failure and strain softening, do this experiment: Take a paper clip and bend it in the same place repeatedly, and after about ten bends you'll notice that it is getting weaker (failure) and after about 15 bends, it snaps right off (fracture). Got that, the difference between failure and fracture?

Having said this, scientists still don't know exactly how avalanches fail and fracture because snow is such a devilishly difficult substance to study. First, large variations commonly exist over both distance and time and second, as you can imagine, catching a natural avalanche in the act is stupendously difficult and dangerous, or as Monty Atwater put it, \"an occupation something like trailing a wounded African buffalo.\" So ten or twenty years from now, the following paragraphs--like so many of the \"facts\" we believe about avalanches--may seem like yet more quaint, geezer-ramblings. Nevertheless, this is what scientists generally believe about how avalanches fail and fracture.

Fracture

Failure occurs slowly at perhaps centimeters per hour; whereas, fracture occurs catastrophically and has been measured at around 20 meters per second. Whamo! The slope shatters like glass.

When a person triggers an avalanche, it means that they have found a trigger point of the avalanche. Perhaps it?s a place where the slab is thinner allowing more of the victim?s weight to tickle the weak layer. Perhaps it?s a place where the weak layer is more poorly bonded than the rest of the slope. I don?t think anyone knows for sure. But we do know that snow is very sensitive to the rate at which it is deformed and the extremely rapid deformation caused by the weight of a person is exactly the kind of thump needed to intiate the fracture process.

Without this final trigger, unstable slopes can teeter on the brink of disaster for quite some time, giving us the illusion that all is well. After a storm, we never know how many slopes would come down if they just had a proper trigger. But with enough good snowmobiles and skilled riders, we can certainly find out. As avalanche researcher Rand Decker likes to say, \"Avalanches are like a bar room brawl. No matter how much tension you have, you need to give somebody a thump to get things going.\"