FIELD: physics.
SUBSTANCE: wind velocity at the crest (V1) and wind velocity on the slope (V2) are first measured on the leeward side of the avalanche-prone slope during a period which is not prone to avalanches, for example, summer. The distance between measuring points (L) is determined and the wind velocity attenuation coefficient for the given slope (K) is calculated using the formula Further, during winter, in standard weather observation conditions according to a 2nd order weather station program, duration of a snowstorm (Tm), rate of the snowstorm (qm) and the amount of precipitation (M) in the calm belt, corresponding to wind velocity of 6 m/s, are determined. Wind velocity at the crest (Vc), the angle between the wind velocity vector and the crest line (α) and the slope angle (β) are simultaneously determined. The maximum increase in thickness of the snow cover (h) on the slope due to precipitation and snowstorm deposits is then determined using the formula
EFFECT: high accuracy of determining increase in thickness of snow cover.
1 dwg
Title | Year | Author | Number |
---|---|---|---|
METHOD TO COLLAPSE SNOW EAVES ON AVALANCHE-PRONE SLOPES | 2011 |
|
RU2482242C2 |
METHOD TO FORECAST START OF SPONTANEOUS COLLAPSE OF SNOW EAVES ON AVALANCHE-PRONE SLOPES | 2011 |
|
RU2482241C2 |
TESTING METHOD OF STABILITY OF SNOW COVER ON AVALANCHE SLOPES | 2011 |
|
RU2478930C1 |
METHOD TO TEST STABILITY OF SNOW COVER ON AVALANCHE-PRONE SLOPES | 2013 |
|
RU2531852C2 |
ANALYZER OF SNOW ACCUMULATION | 2015 |
|
RU2640752C2 |
METHOD OF MECHANISED SNOW CLEARANCE AND CAVING OF SNOW CORNICES IN MOUNTAIN SKI FACILITIES | 2014 |
|
RU2573321C1 |
METHOD FOR REMOTE DETERMINATION OF THICKNESS OF SNOW COVER IN AVALANCHE SITES | 2011 |
|
RU2454651C1 |
DISTANCE-BEARING LASER SNOW RACK | 2018 |
|
RU2702920C1 |
AVIATION ANTI-AVALANCHE SYSTEM | 2011 |
|
RU2471141C1 |
METHOD FOR DETERMINING MARGINAL STABILITY OF SNOW COVER AT AVALANCHE-PRONE SLOPE | 2016 |
|
RU2643382C1 |
Authors
Dates
2013-02-27—Published
2011-07-25—Filed