Chinese glaciers melting at 'shocking' pace, scientists say

Meltwater flows over the Laohugou No. 12 glacier in the Qilian mountains, Subei Mongol Autonomous County, in Gansu province, China, on September 27, 2020.

Glaciers in China's bleak Qilian mountains are disappearing at a shocking rate as global warming brings unpredictable change and raises the prospect of crippling, long-term water shortages, scientists say.

The largest glacier in the 800-kilometer (500-mile) mountain chain on the arid northeastern edge of the Tibetan plateau has retreated about 450 meters since the 1950s, when researchers set up China's first monitoring station to study it.
The 20-square kilometer glacier, known as Laohugou No. 12, is criss-crossed by rivulets of water down its craggy, grit-blown surface. It has shrunk by about 7% since measurements began, with melting accelerating in recent years, scientists say.
    Equally alarming is the loss of thickness, with about 13 meters (42 feet) of ice disappearing as temperatures have risen, said Qin Xiang, the director at the monitoring station.
    "The speed that this glacier has been shrinking is really shocking," Qin told Reuters on a recent visit to the spartan station in a frozen, treeless world, where he and a small team of researchers track the changes.
    The Tibetan plateau is known as the world's Third Pole for the amount of ice long locked in the high-altitude wilderness.
    Jin Zizhen, 27, a PhD student of glacial hydrology, and Qin Xiang, the director of the Qilian Shan Station of Glaciology and Ecologic Environment of the Chinese Academy of Sciences, walk towards the Laohugou No. 12 glacier in the Qilian mountains, in Gansu province, China on September 26, 2020.
    But since the 1950s, average temperatures in the area have risen about 1.5 Celsius, Qin said, and with no sign of an end to warming, the outlook is grim for the 2,684 glaciers in the Qilian range.
    Across the mountains, glacier retreat was 50% faster in 1990-2010 than it was from 1956 to 1990, data from the China Academy of Sciences shows.
    "When I first came here in 2005, the glacier was around that point there where the river bends," Qin said, pointing to where the rock-strewn slopes of the Laohugou valley channel the winding river to lower ground.
    The flow of water in a stream near the terminus of the Laohugou No. 12 runoff is about double what it was 60 years ago, Qin said.
    Further downstream, near Dunhuang, once a major junction on the ancient Silk Road, water flowing out of the mountains has formed a lake in the desert for the first time in 300 years, state media reported.

    Dangerous change

    Global warming is also blamed for changes in the weather that have brought other unpredictable conditions.
    Snowfall and rain has at t