Most noticable was a crown on an east aspect above 8000', nearby a wind pillow was seen on a NE aspect at the same elevation. "Temperature gradient and initial snow density as controlling factors in the formation and structure of hard depth hoar", Depth Hoar, Avalanches, And Wet Slabs: A Case Study Of The Historic March, 2012 Wet Slab Avalanche Cycle At Bridger Bowl, Montana, The formation rate of depth hoar J. C. Giddings E. LaChapelle, https://en.wikipedia.org/w/index.php?title=Depth_hoar&oldid=999431883, Creative Commons Attribution-ShareAlike License, This page was last edited on 10 January 2021, at 03:50. Persistence: This advisory does not apply to operating ski areas, expires at midnight tonight, and is the sole responsibility of the U.S. Forest Service.... Read more » Sparkly, larger grained, beginning and intermediate facets are square 1-3 mm, advanced facets can be cup-shaped 4-10 mm. The following conditions promote faceting: • Intermountain climates: Common before about January. The ones most likely to fail currently are buried surface hoar and near surface facets. Weak layer fracture: facets and depth hoar I. Reiweger and J. Schweizer I. Reiweger and J. Schweizer . Depth hoar forms when a shallow snowpack, typically less than one meter deep, is exposed to a cold and clear weather pattern that persists for an extended period of time. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs. From large temperature gradients between the warm ground and the cold snow surface. As the new snow builds depth and consolidates these layers are more likely to fail and propagate to larger areas. However this same layer of snow also poses significant danger when a heavy slab of snow settles on top of it. Snow is a wonderful insulator and even with very cold air temperatures it’s common for the snow near the ground to remain damp for most of the season. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Strong winds tonight (Dec 22) and snow fall will increase the danger. Routefinding Considerations: Especially in the early winter, cold temperature often combines with a thin snowpack making the perfect breeding conditions for the dreaded faceted snow near the ground, which we call depth hoar. Depth hoar, also called sugar snow or temperature gradient snow (or TG snow), are large snow-crystals occurring at the base of a snowpack that form when uprising water vapor deposits, or desublimates, onto existing snow crystals. Weak layer fracture: facets and depth hoar I. Reiweger and J. Schweizer I. Reiweger and J. Schweizer . Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Doug Chabot of the GNFAC finds the top six inches of the snowpack consists of near surface facets from the cold clear nights and warmer days. The larger the grain, the more persistent. Makes large and scary avalanches. ECTP27 on facets over 12/1 crust PST 38/100 End on facets 12/1 crust Multiple students got similar results in the vicinity on E aspect. Depth hoar is guilty until proven innocent. Faceted crystals, or facets, are produced when a strong vertical temperature gradient exists. Often makes up the entire snowpack until about February. We dug several pits on SE, SW, and N aspects and were unable to find any recently buried surface hoar. Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. The median persistence in compression tests in-creased to 78 days for facets larger than 2.3 mm. Feels like: Loose, runs through your fingers, granular, crunchy when chewed. The snowpack around Mt Emma is generally heavily wind affected and thinner than when I was in the area 3 weeks ago, except in the most wind loaded spots. Depth hoar persists in areas where the snowpack remains shallow. Snow surfaces are a mix of wind crusts, wind board, sun crusts, and in some select spots, recycled powder. Please upload photos below. Depth hoar forms because of large temperature gradients within the snowpack. Depth hoar crystals bond poorly to each other, increasing the risk for avalanches. 2. Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. Posted by Nathan Boyer-Rechlin on Dec 16, ... Chipmunks, mice, voles, and ermine spend their winter months tunneling through the loose depth hoar, rarely seen above the snowpack. Depth hoar crystals bond poorly to each other, increasing the risk for avalanches. Large cup-shaped facets form and may reach 4-10 mm in size. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Depth hoar forms when a shallow snowpack is exposed to an extended period of cold and clear weather. Depth Hoar Summary: Looks like: Sparkly, larger grained, beginning and intermediate facets are square 1-3 mm, advanced facets can be cup-shaped 4-10 mm. The weak layer in the artificial samples was a thin layer of faceted crystals, whereas the natural samples contained a thick weak layer of large depth hoar crystals. Good morning; this is Jeff Carty with the West Central Montana Avalanche Center’s avalanche advisory for January 2, 2021. Our limited data for facet layers with average grain size less than or equal to 0.7 mm suggests such layers usually do not remain weak for long Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. Surface hoar forms on cold clear nights - it is essentially frozen dew. Granular Phase Transition in Depth Hoar and Facets: A New Approach to Snowpack Failure? Under these conditions, individual snow crystals become faceted and angular, making it very difficult for these grains to bond together. Local collapses BTL in areas with 90cm of snow or more, five days after the storm passed. If the faceting process continues, large, six - sided hollow or filled cup shaped grains called depth hoar are formed. Great to get some fresh air and excercise with @ross.hewitt and @tom_grant_ @salomonfreeski @salomon @smithopticsuk @smithoptics.snow @fatmap_official They can be avoided by sticking to sheltered or wind-scoured areas. If the faceting process continues, large, six - sided hollow or filled cup shaped grains called depth hoar are formed. Understanding near-surface facet development will enable a deeper comprehension of an important aspect of the slab avalanche. Relatively stronger in compression than in shear. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. Percolating melt water in spring often re-activates large-grained depth hoar. Depth Hoar is common in Rocky Mountain climates, around large rocks and high shrubs, and where the snowpack is thin. Tests: 2,000 ft, W , 21° Slope, STE 40cm down on N/O Interface CT11 SP (Simultaneous fractures) 20cm down within New interface 32cm down on buried surface hoar These grains are cohensionless and have a hard time bonding due to their angled structure and large size. We found hard wind slabs on NE aspects above 6500', where these were present we stayed on slopes 30 degrees or less. Warm days with cold nights promote growth due to the temperature fluctuations. These are touchy in some spots and unreactive in others. Depth hoar avalanches usually triggered from a shallow snowpack area–avoid rocks outcropping in the middle of a slope. We therefore performed laboratory experiments with snow samples containing a weak layer consisting of either faceted crystals or depth hoar. • Maritime climates: Rare and usually in the early season. Download PDF: Sorry, we are unable to provide the full text but you may find it at the following location(s): https://doi.org/10.5194/tcd-7-... (external link) They can be avoided by sticking to sheltered or wind-scoured areas. An equally dangerous weak layer is surface hoar. Depth hoar crystals are large, sparkly grains with facets that can be cup-shaped and that are up to 10 mm in diameter. Fails both in collapse and in shear. During these experiments the samples were loaded with different loading rates and at various tilt angles until fracture. Loose, runs through your fingers, granular, crunchy when chewed. Understanding the fracture behavior of weak snow layers is essential for modeling and predicting dry-snow slab avalanches. Areas with slightly thinner snow - sometimes at mid elevations or thinner for other reasons - have the weakest facets which have become striated depth hoar crystals. Shady mid elevation slopes, areas of frequent wind scour, rocky outcroppings, and the bottom of basins where cold air pools remain suspect. The water vapour is moving quickly , and crystal growth happens quickly . We dug a pit near the top of the main east bowl in some trees that provided a little protection from the winds. April 20th, 2013 avalanche that killed 5 people that slide on a depth hoar layer from November 2012. image: CAIC. Typically smaller in size than depth hoar, usually around 1-2mm. The following conditions promote faceting: We toured in the Southern Whitefish Range to try and get a better idea of the distribution of the recently buried surface hoar. At mid latitudes, mainly on shady aspects (NW-NE). Usually requires a thin snowpack combined with a clear sky or cold air temperature. Surface hoar forms on cold clear nights - it is essentially frozen dew. These layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. The most common persistent weak layers involved in deep, persistent slabs are depth hoar, deeply-buried surface hoar, or facets surrounding a deeply-buried crust. An equally dangerous weak layer is surface hoar. to failure in compression, as was previously shown for sam-ples containing a weak layer of surface hoar (Reiweger and. Understanding failure initiation within weak snow layers is essential for modeling and predicting dry-snow slab avalanches. Fascinating Facets of Eagle County Snow Country. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs. Depth Hoar–faceted snow near the ground: There is a soft slab about 8-10 inches thick on top of these facets. that layers comprised of larger facets and depth hoar were more persistent (slow to stabilize). The avalanche danger in the west central Montana backcountry is Moderate, with caution. The process in reverse, however, occurs much slowly because it takes so much energy to create a faceted crystal that when we take the energy source away (the strong temperature gradient) it take a lot of time for the crystal to return to its equilibrium state (rounds). The formation of depth hoar in Arctic or Antarctic firn can cause isotopic changes in the accumulating ice. HS 120-150cm, with bottom 15-25cm fist hard depth hoar/facets. During these experiments the samples were loaded with different loading rates and at various tilt angles until fracture. The Colorado Avalanche Information Center released an early season snow update on their blog a couple of years ago, which still holds true today. Found some great facet holes, depth hoar, surface hoar, and even some sugar snow that you could pretend was powder. Especially nasty when it forms on a hard bed surface. These colder grains first develop sharp corners, then stepped facets. The most common persistent weak layers involved in deep, persistent slabs are depth hoar, deeply-buried surface hoar, or facets surrounding a deeply-buried crust. These colder grains first develop sharp corners, then stepped facets. Forecasting considerations: Persistent, Deep-Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. Weak gradient turns facets back to rounds. Pay attention to what your slope is connected to. facets and depth hoar are more prone to failure in shear than. Basal facets were moist with no striations while nearly non-existent, fragmented depth hoar seems to be rounding at this elevation. Persistent, Deep-Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs. Their message is one of warning, an early-season snowfall that will affect the layers of snow that will fall on top of this one for … Also called: Depth Hoar in snow. Extremely persistent in the snowpack from several days to several weeks, depending on temperature. In very cold climates, forms on warmer slopes (sun exposed, near fumaroles, non permafrost areas). Common persistent layers include surface hoar, depth hoar, near-surface facets, or faceted snow. Carefully measure temperature gradients across the weak layer. Good focus for days to come. Grows best at snow temperatures from -2 deg C to -15 deg C. Mechanical Properties: Click here for help on resizing images. The only exception to this is in permafrost areas (very high elevations at mid latitudes or arctic latitudes) or in areas with a very thin snow cover combined with very cold temperatures. The loading experiments were performed at a tempera- ture of −5 C with the apparatus shown in Fig. • Continental climates: extremely common throughout the season. They can be avoided by sticking to sheltered or wind-scoured areas. Depth hoar, also called sugar snow or temperature gradient snow (or TG snow), are large snow-crystals occurring at the base of a snowpack that form when uprising water vapor deposits, or desublimates, onto existing snow crystals.Depth hoar crystals are large, sparkly grains with facets that can be cup-shaped and that are up to 10 mm in diameter. The specific surface hoar layer we were hunting for is a layer that is found throughout the Swan and Flathead Ranges. 2 Laboratoire de Glaciologie et Géophysique de l'Environnement, 54 rue Molière, 38402 - Saint Martin d'Hères cedex, France. Contrary to popular belief, as long as the ground has an insulating blanket of snow, the ground is almost always warm–near freezing–even with very cold air temperatures. Snowpack total depth 47" with 2" depth hoar at the ground. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. Alain Duclos1, Stéphane Caffo1, Marc Bouissou1, Jane R. Blackford3, François Louchet2, Joachim Heierli3 1Data-avalanche.org, 15 Rue de la Buidonnière, 73500 Aussois, France. Looks like: Large-grained, faceted, cup-shaped crystals near the ground. Also called: Depth hoar crystals are large, sparkly grains with facets that can be cup-shaped and that are up to 10 mm in diameter. Commonly propagates long distances, around corners and easily triggered from the bottom–your basic nightmare. The top of the snow surface, on the other hand, can become extremely cold–especially when exposed to a clear sky–thus creating one of the most common temperature gradient conditions. Behaves like a stack of champagne glasses. They have sharp angles and form from large temperature gradients within the snowpack. Near surface facets are smaller in size than depth hoar (1-2 mm) but they are quite pesky and can persist in the snowpack for long periods of time. At arctic and equatorial latitudes, it shows much less preference for aspect. Once this layer is buried by subsequent snowfalls, it is preserved, and can even deteriorate further to become a layer of depth hoar. The rule of thumb is that faceting takes place when the temperature gradient is larger than 1°C per 10 cm depth, or equivalently 10°C per metre. Understanding failure initiation within weak snow layers is essential for modeling and predicting dry-snow slab avalanches. *See Snowpilot for details* Photos & Video. Feels like: Formed: Depth Hoar is common in Rocky Mountain climates, around large rocks and high shrubs, and where the snowpack is thin. Image: Agricultural Research Service, U.S. Department of Agriculture Understand and Managing Depth Hoar: By: Eric Trenbeath When the first significant storm paints the peaks white and we’re getting stoked for winter, it’s time to start thinking about how that first layer will affect snowpack stability during the upcoming season. We therefore performed laboratory experiments with snow samples containing a weak layer consisting of either faceted crystals or depth hoar. The snowpack was the usual facet-crust-depth hoar except for a few terrain features. This can influence analysis of ice cores in scientific research. Toured up the Camas Drainage for a few days. Near surface facets are smaller in size than depth hoar (1-2 mm) but they are quite pesky and can persist in the snowpack for long periods of time. Temperature Gradient (TG) (but this is an outdated term) sugar snow, squares, sometimes incorrectly called “hoar frost” by old, rural geezers. Never underestimate the persistence of faceted snow as a weak layer. Facets– Facets, or squares as they are sometimes referred to, are associated with most the avalanche fatalities. Maximum of 5 megabytes per image. The result is a snow pack that deteriorates into a layer of facets. Easily triggered from the bottom of a slope or from an adjacent flat area. We therefore performed laboratory experiments with snow samples containing a weak layer consisting of either faceted crystals or depth hoar. It is possible to trigger avalanches on this layer. to failure in compression, as was previously shown for sam-ples containing a weak layer of surface hoar (Reiweger and. surface facets compared to 31% for surface hoar and 6% for depth hoar. facets and depth hoar are more prone to failure in shear than. During these experiments the samples were loaded with different loading rates and at various tilt angles until fracture. In my travels over the years in a depth hoar plagued mountain range, I've had to learn to scale back my expectations significantly. Distribution Pattern: The wind slabs are also sitting atop persistent weak layers, and slides that fail on buried facets and depth hoar could be up to 4 feet deep at upper elevations and 18 inches deep at low elevations. 1 and de- … Depth hoar, also called sugar snow[1] or temperature gradient snow (or TG snow),[2] are large snow-crystals occurring at the base of a snowpack that form when uprising water vapor deposits, or desublimates, onto existing snow crystals. Large gradients mean the snow will remain weak, small gradients mean the snow is gaining strength but it takes several days to several weeks depending on temperature. Regional Differences: Required/Recommended Avalanche Safety Gear This snow lurks silently at the base of our snowpack until activated by a larger snowfall event. 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