7 citations as recorded by crossref.

1. Tree-ring density inferred late summer temperature variability over the past three centuries in the Gaoligong Mountains, southeastern Tibetan Plateau M. Li et al. https://doi.org/10.1016/j.palaeo.2015.01.003
2. Picea schrenkiana tree ring blue intensity reveal recent glacier mass loss in High Mountain Asia is unprecedented within the last four centuries W. Yue et al. https://doi.org/10.1016/j.gloplacha.2023.104210
3. Late summer temperature reconstruction based on tree-ring density for Sygera Mountain, southeastern Tibetan Plateau M. Li et al. https://doi.org/10.1016/j.gloplacha.2018.02.005
4. Himalayan glaciers experienced significant mass loss during later phases of little ice age M. Shekhar et al. https://doi.org/10.1038/s41598-017-09212-2
5. Central Himalayan tree-ring isotopes reveal increasing regional heterogeneity and enhancement in ice mass loss since the 1960s N. Singh et al. https://doi.org/10.5194/tc-15-95-2021
6. Linkages of the dynamics of glaciers and lakes with the climate elements over the Tibetan Plateau J. Sun et al. https://doi.org/10.1016/j.earscirev.2018.06.012
7. Post‐industrial late summer warming recorded in tree‐ring density in the eastern Tibetan Plateau J. Duan et al. https://doi.org/10.1002/joc.6239