Ice is melting and permafrost is thawing in the Nepal HimalayaPermafrost thaw slump in the Kali Gandaki River, Nepal HimalayaThe moraine-dammed proglacial lake of the largest valley Laigu Glacier, TibetHigh summer melt flow and sediment from the Dongkemadi Glacier, Tibetan Plateau (photo by S.Wang).Ice avalanche and landslide into moraine-dammed glacial lakes may trigger displacement waves and GLOFs (The Bienong Tsho, Jiali county, Tibet)A dying valley glacier in Ranwu, southeastern TibetThermal subsidence in the headwater of the Yangzte RiverLarge-scale permafrost thaw slumps in the Fenghuoshan region on the Tibetan Plateau (34. 71N, 92.90E) (Photo by C. Song)Thermal erosion landforms in the source region of the Yangtze River, central Tibetan PlateauProglacial area in the headwater of the Yangtze RiverBraided channel of the Buqu river, originating from the Jiangendiru Glacier, Tibetan PlateauBank erosion in Buqu River, central Tibetan PlateauDongfeng Li surveying the river channel of the headwater of the Mekong using UAV and RTKDongfeng Li and colleagues surveying the river channel of the headwater of the Yangtze using UAV and RTK
Viewing Message: 1 of 1. Warning
Blog.nus accounts will move to SSO login soon. Once implemented, only current NUS staff and students will be able to log in to Blog.nus. Public blogs remain readable to non-logged in users. (More information.)