Though the amount of ice on the plateau of Tibet and its surrounding mountains, such as the Himalayas, Karakoram and Pamirs, is a lot smaller than that at the poles, it is still huge. The area’s 46,000 glaciers cover 100,000 square kilometres (40,000 square miles)—about 6% of the area of the Greenland ice cap. Another 1.7m square kilometres is permafrost, which can be up to 130 metres deep. That is equivalent to 7% of the Arctic’s permafrost. Unlike the ice at the poles, the fate of this ice affects a lot of people directly. The area is known by some as Asia’s water tower, because it is the source of ten of the continent’s biggest rivers. About 1.5 billion people, in 12 countries, live in the basins of those rivers. Welcome, then, to the Earth’s “Third Pole”.
Researchers will now monitor a set of bellwether glaciers every six months. They will set up observatories to measure solar radiation, snowfall, meltwater and changes in the soil, as well as air temperature, pressure, humidity and wind. And they plan to take cores from the ice on the Tibetan plateau. These will let them reconstruct the area’s climate over the past few hundred thousand years. Together, these data will give them a better grip on how much—and why—the Third Pole is changing.
Via Committee of 100 for TIbet