Cryosphere
Cryosphere includes the water in frozen state.
Glaciers, ice sheets, ice caps, lake and river ice, permafrost, seasonal snow
and ice crystals in the atmosphere together form cryosphere. Earth’s climate is
highly influenced by the extent of cryosphere as it controls the energy budget
of the earth (Figure 5.2).
Perennial ice cover is found in Greenland and Antarctica as ice sheets, as mountain glaciers and as permafrost in higher latitudes. Permafrost is the condition prevailing when water freezes above and
below the ground, (including rock or soil) for more than two consecutive years.
Most permafrost regions are located in high latitudes, but alpine permafrost
may exist at high mountains in much lower latitudes.
Fact File
Mount Kilimanjaro (5895m) in Tanzania, Africa,
located closer to the equator has permafrost.
Seasonal snow and ice crystals are confined to
middle latitudes and high mountains in lower latitude. Sea ice is frozen ocean water. Its formation, growth and melting
are all confined to the ocean. An ice
shelf is a thick, floating slab of ice that forms where a glacier or ice
flows
The world’s largest ice shelves
are the Ross Ice Shelf and the Filchner-Ronne ice shelf in Antarctica. An iceberg
is ice floating in open water that has
broken off from glaciers or ice shelf.
Cryosphere is a climate indicator. Cryosphere with
its high albedo influences the energy balance of the whole planet. Changes in
cryosphere will alter land cover, surface temperature, soil moisture, air
temperature, radiation, air circulation, clouds, precipitation, sea level, sea
surface temperature, salinity, ocean current, fauna, flora and microbes. There
is a complex interaction and balance among the spheres of the earth which makes
life to flourish in the earth. If there is a change in one sphere it affects
the other spheres as well. Nature maintains this balance. Understanding this
complex interactions and living in harmony with nature will help to mitigate
the environmental problems faced by the earth.
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