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A Melting Planet Essay

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A Melting Planet

Although most glaciers and ice sheets reside in areas that man does not inhabit, they are nevertheless important for society and the global environment. Due to anthropogenic activities over the past two centuries, the temperature of the earth is rising at an alarming rate. This rise in temperatures has resulted in an overall loss of ice mass worldwide, including a rapid depletion in mountain glaciers. The effects of glacial melt will have a significant impact on the future of the human race, so it is therefore important to have a firm understanding of glaciers.

In order for a glacier to form, all of three conditions must be met. Firstly, the climate of the area must be cold enough so that snow that falls during …show more content…

For glaciers in warmer climates, the lower melting point means that the ice on the bottom of the glacier will melt. This thin layer of water, combined with melt water that seeps through cracks in the glacier, allows for the glacier to move, sometimes at a rapid rate. However, the Antarctic ice sheet is so cold that despite the great pressure on the base of the sheet due to its immense depth, it is frozen solid to the surface.

The equilibrium line, or snow line, is very important for the dynamics of a glacier. At higher latitudes, the snow line can be as low as sea level, whereas near the equator the snow line can be as high as 5 km. Above the snow line is the zone of accumulation, where snow will accumulate over many years and eventually turn into glacial ice. Below the snow line is the zone of ablation, where sublimation, the evaporation of ice into water vapor, along with melting and calving results in the loss of glacial ice mass(Marshak 674). If the rate at which snow accumulates in the zone of accumulation exceeds the rate of ablation, then the increasing pressure from the upper part of the glacier will cause the toe of the glacier to move forward into previously unglaciated terrain. This process is called glacial advance. Conversely, if the rate of ablation exceeds the rate of accumulation, the toe of the glacier will retreat back up the mountain toward the snow line. This process is called glacial retreat. Depending on variations in yearly temperatures,

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