13 citations as recorded by crossref.

1. Multi-Temporal Variations in Surface Albedo on Urumqi Glacier No.1 in Tien Shan, under Arid and Semi-Arid Environment X. Yue et al. 10.3390/rs14040808
2. Assessment of winter season land surface temperature in the Himalayan regions around the Kullu area in India using landsat-8 data D. Varade & O. Dikshit 10.1080/10106049.2018.1520928
3. Comparing simple albedo scaling methods for estimating Arctic glacier mass balance S. Williamson et al. 10.1016/j.rse.2020.111858
4. Large-area high spatial resolution albedo retrievals from remote sensing for use in assessing the impact of wildfire soot deposition on high mountain snow and ice melt A. Bertoncini et al. 10.1016/j.rse.2022.113101
5. Changes in glacier albedo and the driving factors in the Western Nyainqentanglha Mountains from 2001 to 2020 S. Ren et al. 10.1017/jog.2023.45
6. Remote sensing of earth’s energy budget: synthesis and review S. Liang et al. 10.1080/17538947.2019.1597189
7. Anisotropy Parameterization Development and Evaluation for Glacier Surface Albedo Retrieval from Satellite Observations S. Ren et al. 10.3390/rs13091714
8. A Multilayer Surface Temperature, Surface Albedo, and Water Vapor Product of Greenland from MODIS D. Hall et al. 10.3390/rs10040555
9. Lateglacial and Holocene sedimentary dynamics in northwestern Baffin Bay as recorded in sediment cores from Cape Norton Shaw Inlet (Nunavut, Canada) N. Stevenard et al. 10.1111/bor.12575
10. Albedo reduction as an important driver for glacier melting in Tibetan Plateau and its surrounding areas Y. Zhang et al. 10.1016/j.earscirev.2021.103735
11. Influence of recent warming and ice dynamics on glacier surface elevations in the Canadian High Arctic, 1995–2014 C. MORTIMER et al. 10.1017/jog.2018.37
12. Spatiotemporal Variability of Land Surface Albedo over the Tibet Plateau from 2001 to 2019 X. Lin et al. 10.3390/rs12071188
13. Variation in Albedo and Its Relationship With Surface Dust at Urumqi Glacier No. 1 in Tien Shan, China X. Yue et al. 10.3389/feart.2020.00110