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The accumulation zone is found at the highest altitude of the glacier, where accumulation of material is greater than ablation. On a glacier , the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation , ( melting , evaporation , and sublimation ).
The boundary between the accumulation zone and the ablation zone on glaciers is called the "annual snow line". The glacier region below this snow line was subject to melting in the previous season. The term "orographic snow line" is used to describe the snow boundary on surfaces other than glaciers.
Snow accumulation on ground and in tree branches in Germany Snow blowing across a highway in Canada Spring snow on a mountain in France. Classifications of snow describe and categorize the attributes of snow-generating weather events, including the individual crystals both in the air and on the ground, and the deposited snow pack as it changes over time.
Extreme snow accumulation on building roofs. Snow is an important consideration for loads on structures. To address these, European countries employ Eurocode 1: Actions on structures - Part 1-3: General actions - Snow loads. [85] In North America, ASCE Minimum Design Loads for Buildings and Other Structures gives guidance on snow loads. [86]
Snow Depth-This is a measurement from the snow surface to the ground in meters. It is commonly does over a large time span using immobile graduated stakes. Snow Water Equivalency- A measuring tool which represents the vertical depth of water that would accumulate in an area, if all the snow and ice were melted in that given area.
[1] [2] These zones include the dry snow zone, in which the ice entirely retains subfreezing temperatures and no melting occurs. Dry snow zones only occur within the interior regions of the Greenland and Antarctica ice sheets. [3] [4] Below the dry snow zone is the percolation zone, where some meltwater penetrates down into the glacier where it ...
Accumulation zone – where the formation of ice is faster than its removal. Ablation (or wastage) zone – when the sum of melting, calving , and evaporation (sublimation) is greater than the amount of snow added each year.
Sampling the surface of a glacier. There is increasingly dense firn between surface snow and blue glacier ice. Firn field on the top of Säuleck, Hohe Tauern. Firn (/ f ɪər n /; from Swiss German firn "last year's", cognate with before) is partially compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé.