The ABC's of Glaciology
Glacial ice is formed from highly compressed snow. In areas of the world where more snow falls
each year than can melt or evaporate, the snow builds up and its structure gradually changes.
On the most minute level, a snowflake's delicate hexagonal shape breaks apart under the weight
of more snow.
The flakes, continually compressed by layers of snow on top of them, are eventually reshaped
into rounded grains, with a texture and size similar to coarse sugar. The pockets of air
between the grains of snow likewise become smaller and smaller. In time, the compressed snow,
known as firn, is transformed to glacial ice. This process, repeated hundreds of times
over, is what forms the built-up ice mass of a glacier.
Glaciers and the Water Cycle
As much as 80 percent of the world's fresh water is locked up inside glaciers. The ice sheets that
cover Antarctica and Greenland hold the great majority of this water supply. When summer temperatures
bring about the rapid melting of a glacier, the meltwaters that flow downhill release the stored
fresh water, replenishing the overall water supply.
The glaciers in the Himalaya are not just sliding downhill, they also appear to be melting faster
than they can be replenished. Why this is happening is one of the great puzzles of global climate
change. The ice is critical for Nepal because it feeds many of the rivers which are Nepal's primary
source of drinking and irrigation water. If these ice fields and glaciers disappear, Nepal and
India will have to depend on the unreliable monsoon rains for water.