The Third Pole: A brief introduction
Identified
by frozen features (cryosphere), the Third Pole refers to the region consisting
of Tibetan Plateau and its surrounding areas located in, and around, the
Himalayas. The region covers over 5 million square kilometres, with an
elevation of over 4,000 meters above sea level. The Third Pole is the largest,
and highest, mountain region on Earth. Similar to the Arctic and Antarctic, the
Third Pole contains an estimated 100,000 square kilometres of glaciers, which
hold the world's largest concentrated stock of ice outside the Arctic and
Antarctic. The region comprises approximately 46,000 glaciers. Like other polar
regions, the Third Pole is also sensitive to rising temperatures linked to global
climate change.
Because
of its location in a high altitude mountain region, the impact of climatic
change is increasing more rapidly than the global average, hence contributing
to the rapid melting of glaciers. Research suggests that, since 2005, more than
500 small glaciers have disappeared, and many more are threatened in the future
unless impacts of climate change are mitigated. The impacts of changes in the
Third Pole region significantly influence climates globally. The complex
interactions of natural processes affect biodiversity, ecosystem functions and the
hydrologic cycle. The implications are significant at the regional and global
levels.
Regionally,
more than 1.5 billion people in more than 10 countries (Afghanistan,
Bangladesh, Bhutan, China, India, Kazakhstan, Kyrgyzstan, Myanmar, Nepal,
Pakistan, Tajikistan and Uzbekistan) are affected by declining freshwater
supplies. As regional environmental transformation continues, future changes could
threaten not only natural ecological processes, but also the distribution of
resources, and social and economic sustainability. Such a threat raises the prospect
of regional conflicts among countries in the region that are politically fragile.
As in the polar regions, the melting of glaciers in the Third Pole contributes
to sea level rise with long-term devastating effects on low-lying regions and the
people living there.
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