Glaciers along the southeastern rim of the Tibetan Plateau temporarily defied a warming climate around 9,000 years ago. Now a new model helps explain how they accumulated ice even though other glaciers in the region waned, scientists say.
Glaciers along the southeastern rim of the Tibetan Plateau temporarily defied a warming climate around 9,000 years ago. Now a new model helps explain how they accumulated ice even though other glaciers in the region waned, scientists say.