September
2007- If I compare this land to what it used to be in the
1960s, it is difficult for me to recognize it, recalls Qi Mei
Duo Jie, a 71-year-old nomadic herder from Yanshiping in China's
central-western Qinghai Province. "Glaciers are melting,
temperatures are rising and rainy seasons have become unpredictable."
Yanshiping is the last town on the Qinghai-Tibet Highway before
entering Tibet. At an altitude of 4700 metres, its landscape in
summer is marked by shaggy yaks grazing in the green alpine pastures
and the transparent blue waters of Buqu River - a tributary of
the Yangtze. Winters are white and freezing, with temperatures
reaching as low as -20°C.
It is no surprise that
people welcome a warmer, more comfortable climate in this remote
region. But there is another side to the changing climate story.
Pressure on the
Plateau
Nomadic groups of
Tibetans have
been moving around this area for time immemorial, following the
natural rhythm of the seasons and availability
of grassland to raise their livestock.
Qi
Mei Duo Jie's family has
been raising yaks for at least three generations.
"This year has been very
dry, and with less grassland it will take longer to properly feed
and raise livestock," he says. "This will mean a lower
income for us."
To compound the situation, warmer
climate conditions are attracting more cattle and sheep farmers
to this harsh but beautiful high-altitude area, putting additional
pressure on the already fragile alpine landscape. This pressure
is also starting to squeeze out local wildlife, such as Tibetan
antelopes, that depend on the grasslands too. There have even
been reports of brown bears wandering close to villages in search
of food.
And if bears roaming around town
aren't enough to lose sleep over, the remote rural region is experiencing
pollution from greenhouse gases that have been emitted from big
cities as far away as Beijing and Shanghai.
These are some of the consequences
of climate change on the Qinghai-Tibetan Plateau.
Monitoring the river
"It is only by reducing greenhouse gases across the country,
as well as worldwide, that vulnerable ecosystems can be preserved
and continue to function
as a source of livelihood for people living here and downstream,"
stresses Dr Li Lin, Head of Conservation Strategies
at WWF China.
"With global warming hitting
hard, our efforts must
be extended to find ways for this region
to adapt to climate change."
WWF, the global conservation
organization, is embarking on a series of studies on how high-altitude
wetlands in the Yangtze
source area - including the Qinghai-Tibetan Plateau and parts
of the Kunlun Mountains - can cope with changing climate conditions.
Results of the studies will help WWF and its Chinese partners
come up with practical solutions to protect vulnerable ecosystems
from the adverse affects of climate change.
At the village of Tuotuohe -
also along the Qinghai-Tibet Highway and one of the first places
to cross the Yangtze by bridge
- a hydro-geological station monitors the river's water levels.
This year, despite an increase in precipitation, water depth has
slightly decreased. One spring that used to supply drinking water
has already dried up.
"The water level decrease
is a direct result of rising temperatures," explains Professor
Li Shijie from Nanjing's Institute of Geography and Limnology.
"With warmer weather, evaporation
is happening at a rate faster than the melting of the glaciers
that supplies water to the river. Overall, this means a less supply
of water for local inhabitants."
Melting glaciers
Some 150 kilometres to
the east, in the permafrost area of Fenguoshan, average precipitation
has been
increasing
only
in certain months of
the year, while the general trend points toward drier periods.
The evidence is found in the
permafrost itself, the overlying ground surface layer which freezes
in the winter and thaws
in the summer.
"In the last 20 years, larger
portions of frozen ground have melted during summer," says
Professor Li. "With less water and more sand on the ground,
desertification is just one step away."
"Warming temperatures will
certainly continue, but weather events such as rain, snow and
wind are becoming less predictable," Professor Li adds.
Experts today agree on one trend:
Glaciers, rivers, wetlands and lakes - all elements of the fragile
high-altitude ecosystem - are being altered at a speed never seen
before.
Professor Li has personally witnessed
the retreat of Yuzhu glacier, the highest peak in the Eastern
Kunlun Mountains.
"I was in Xidatan, near
Yuzhu Peak, for the first time in the 1980s, and when I went back,
ten years later, the tongue of the glacier had retreated by 50
metres," he says. "Nowadays it is about 100m higher
than it used to be."
According to scientists, projected
climate change over the next century will further increase the
rate at which glaciers melt. In particular, glaciers in China,
as well as Nepal and India, are receding at an average rate of
10-15 metres per year.
"Once destroyed, it will
be extremely difficult to restore the high-altitude ecosystems,"
adds WWF's Dr Li Lin.
"If industrialized and developing
countries will not focus their efforts on cutting emissions, some
of this land will be lost forever and local populations will be
displaced. What we need is commitment to continue and increase
the efforts of reducing warming pollution so that the next generations
will inherit a healthier environment."
In early June 2007, China released
its first Climate Change National Action Plan. The plan is the
first formal acknowledgement of China's goal to reduce CO2 emissions
through a cut of energy consumption by 20 per cent per unit of
GDP by 2010.
For WWF, this clarification of
the country's basic stand on the issue is expected to play a positive
role and stimulate an international agreement on greenhouse gases
emission cuts in the future.
* Claudia Delpero is
Communications Manager with WWF's European Policy Office.