{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,5,15]],"date-time":"2026-05-15T02:45:06Z","timestamp":1778813106211,"version":"3.51.4"},"reference-count":55,"publisher":"MDPI AG","issue":"18","license":[{"start":{"date-parts":[[2024,9,19]],"date-time":"2024-09-19T00:00:00Z","timestamp":1726704000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["No. U23A2011"],"award-info":[{"award-number":["No. U23A2011"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["No. 2019QZKK0201"],"award-info":[{"award-number":["No. 2019QZKK0201"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["No. XZ202101ZY0001G"],"award-info":[{"award-number":["No. XZ202101ZY0001G"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["No. lzujbky-2022-it25"],"award-info":[{"award-number":["No. lzujbky-2022-it25"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"name":"The Second Tibetan Plateau Scientific Expedition and Research Program (STEP)","award":["No. U23A2011"],"award-info":[{"award-number":["No. U23A2011"]}]},{"name":"The Second Tibetan Plateau Scientific Expedition and Research Program (STEP)","award":["No. 2019QZKK0201"],"award-info":[{"award-number":["No. 2019QZKK0201"]}]},{"name":"The Second Tibetan Plateau Scientific Expedition and Research Program (STEP)","award":["No. XZ202101ZY0001G"],"award-info":[{"award-number":["No. XZ202101ZY0001G"]}]},{"name":"The Second Tibetan Plateau Scientific Expedition and Research Program (STEP)","award":["No. lzujbky-2022-it25"],"award-info":[{"award-number":["No. lzujbky-2022-it25"]}]},{"name":"Science and technology Project of Tibet Autonomous Region","award":["No. U23A2011"],"award-info":[{"award-number":["No. U23A2011"]}]},{"name":"Science and technology Project of Tibet Autonomous Region","award":["No. 2019QZKK0201"],"award-info":[{"award-number":["No. 2019QZKK0201"]}]},{"name":"Science and technology Project of Tibet Autonomous Region","award":["No. XZ202101ZY0001G"],"award-info":[{"award-number":["No. XZ202101ZY0001G"]}]},{"name":"Science and technology Project of Tibet Autonomous Region","award":["No. lzujbky-2022-it25"],"award-info":[{"award-number":["No. lzujbky-2022-it25"]}]},{"name":"Central Universities","award":["No. U23A2011"],"award-info":[{"award-number":["No. U23A2011"]}]},{"name":"Central Universities","award":["No. 2019QZKK0201"],"award-info":[{"award-number":["No. 2019QZKK0201"]}]},{"name":"Central Universities","award":["No. XZ202101ZY0001G"],"award-info":[{"award-number":["No. XZ202101ZY0001G"]}]},{"name":"Central Universities","award":["No. lzujbky-2022-it25"],"award-info":[{"award-number":["No. lzujbky-2022-it25"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Albedo is a primary driver of the glacier surface energy balance and consequent melting. As glacier albedo decreases, it further accelerates glacier melting. Over the past 20 years, glaciers on the Tibetan Plateau have experienced significant melting. However, our understanding of the variations in glacier albedo and its driving factors in this region remains limited. This study used MOD10A1 data to examine the average characteristics and variations in glacier albedo on the Tibetan Plateau from 2001 to 2022; the MOD10A1 snow cover product, developed at the National Snow and Ice Data Center, was employed to analyze spatiotemporal variations in surface albedo. The results indicate that the albedo values of glaciers on the Tibetan Plateau predominantly range between 0.50 and 0.60, with distinctly higher albedo in spring and winter, and lower albedo in summer and autumn. Glacier albedo on the Tibetan Plateau decreased at an average linear regression rate of 0.06 \u00d7 10\u22122 yr\u22121 over the past two decades, with the fastest declines occurring in autumn at an average rate of 0.18 \u00d7 10\u22122 yr\u22121, contributing to the prolongation of the melting period. Furthermore, significant variations in albedo change rates with altitude were found near the snowline, which is attributed to the transformation of the snow and ice surface. The primary factors affecting glacier albedo on the Tibetan Plateau are temperature and snowfall, whereas in the Himalayas, black carbon and dust primarily influence glacier albedo. Our findings reveal a clear decrease in glacier albedo on the Tibetan Plateau and demonstrate that seasonal and spatial variations in albedo and temperature are the most important driving factors. These insights provide valuable information for further investigation into surface albedo and glacier melt.<\/jats:p>","DOI":"10.3390\/rs16183472","type":"journal-article","created":{"date-parts":[[2024,9,19]],"date-time":"2024-09-19T03:34:20Z","timestamp":1726716860000},"page":"3472","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":3,"title":["Variation in Glacier Albedo on the Tibetan Plateau between 2001 and 2022 Based on MODIS Data"],"prefix":"10.3390","volume":"16","author":[{"given":"Ping","family":"Liu","sequence":"first","affiliation":[{"name":"College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China"},{"name":"State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Guangjian","family":"Wu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Bo","family":"Cao","sequence":"additional","affiliation":[{"name":"College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China"},{"name":"Shiyang River Basin Scientific Observing Station, Lanzhou University, Lanzhou 730000, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Xuanru","family":"Zhao","sequence":"additional","affiliation":[{"name":"College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Yuxuan","family":"Chen","sequence":"additional","affiliation":[{"name":"College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1968","published-online":{"date-parts":[[2024,9,19]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"663","DOI":"10.1038\/nclimate1580","article-title":"Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings","volume":"2","author":"Yao","year":"2012","journal-title":"Nat. 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