Ten glaciers exhibit negative surface albedo trends (-0.0005 to -0.005 yr -1 ) during the period 2000–2011, whereas TLMKL has a positive trend (0.0006 yr -1 ) in the Karakoram area ( Fig 3 ).
← all excerpts
Widespread albedo decreasing and induced melting of Himalayan snow and ice in the early 21st century.
1
—
—