{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,11,8]],"date-time":"2025-11-08T18:02:16Z","timestamp":1762624936904,"version":"build-2065373602"},"reference-count":56,"publisher":"MDPI AG","issue":"21","license":[{"start":{"date-parts":[[2022,10,28]],"date-time":"2022-10-28T00:00:00Z","timestamp":1666915200000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001809","name":"Natural Science Foundation of China","doi-asserted-by":"publisher","award":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"],"award-info":[{"award-number":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"name":"Second Tibetan Plateau Scientific Expedition and Research (STEP)","award":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"],"award-info":[{"award-number":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"]}]},{"DOI":"10.13039\/501100007129","name":"Natural Science Foundation of Shandong Province","doi-asserted-by":"publisher","award":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"],"award-info":[{"award-number":["41971073","42271145","42171121","41901088","42101120","2019QZKK0106","ZR2021QD138"]}],"id":[{"id":"10.13039\/501100007129","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>A long-series mass balance (MB) of glaciers can be used to study glacier\u2013climate relationships. Using a distributed simplified energy balance model (SEBM) and an enhanced temperature-index model (ETIM), the MB of Laohugou Glacier No. 12 (LHG12) was reconstructed from 1980 to 2020, driven by a calibrated ERA5 reanalysis dataset. The simulation of SEBM performs better than that of ETIM. The results showed that the annual MB of LGH12 is a fluctuating trend of declining from 1980 to 2020, with annual means of \u22120.39 \u00b1 0.28 m w.e. a\u22121 and cumulative value of \u221216 \u00b1 4 m w.e. During 1980\u20131990, the annual MB fluctuated in a small range, while after 1990, LHG12 accelerated melting owing to rising air temperature, with annual means of \u22120.48 m w.e. a\u22121, three times as large as that of 1980\u20131990. The largest mass loss occurred during 2001\u20132010 at an average rate of \u22120.57 m w.e. a\u22121. The average equilibrium line altitude (ELA) was 4976 m a.s.l., and since 1980, the ELA has been increasing at a rate of 37.5 m\/10 a. LHG12 is most sensitive to air temperature, and the MB sensitivity reaches \u22120.51 m w.e. a\u22121 with air temperature increase of 1 \u00b0C. The sensitivity of MB to incoming shortwave radiation (+10%) simulated by SEBM is \u22120.30 m w.e. a\u22121, three times larger than that simulated by ETIM. This is mainly because the two models have different conditions for controlling melting. Melting is controlled only by air temperature for ETIM, while for SEBM, it is controlled by air temperature and incoming shortwave radiation.<\/jats:p>","DOI":"10.3390\/rs14215424","type":"journal-article","created":{"date-parts":[[2022,10,30]],"date-time":"2022-10-30T09:01:42Z","timestamp":1667120502000},"page":"5424","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":5,"title":["Mass Balance Reconstruction for Laohugou Glacier No. 12 from 1980 to 2020, Western Qilian Mountains, China"],"prefix":"10.3390","volume":"14","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-8114-3924","authenticated-orcid":false,"given":"Jiake","family":"Wu","sequence":"first","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"given":"Weijun","family":"Sun","sequence":"additional","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"given":"Baojuan","family":"Huai","sequence":"additional","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1142-6598","authenticated-orcid":false,"given":"Minghu","family":"Ding","sequence":"additional","affiliation":[{"name":"Institute of Global Change and Polar Research, Chinese Academy of Meteorological Sciences, Beijing 100081, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4742-7127","authenticated-orcid":false,"given":"Lei","family":"Wang","sequence":"additional","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3564-6787","authenticated-orcid":false,"given":"Yuzhe","family":"Wang","sequence":"additional","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"given":"Junlong","family":"Zhang","sequence":"additional","affiliation":[{"name":"College of Geography and Environment, Shandong Normal University, Jinan 250014, China"}]},{"given":"Wentao","family":"Du","sequence":"additional","affiliation":[{"name":"Qilian Shan Station of Glaciology and Eco-Environment, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"given":"Jizu","family":"Chen","sequence":"additional","affiliation":[{"name":"Qilian Shan Station of Glaciology and Eco-Environment, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]},{"given":"Xiang","family":"Qin","sequence":"additional","affiliation":[{"name":"Qilian Shan Station of Glaciology and Eco-Environment, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China"}]}],"member":"1968","published-online":{"date-parts":[[2022,10,28]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"59","DOI":"10.5194\/tc-8-59-2014","article-title":"Feedbacks and mechanisms affecting the global sensitivity of glaciers to climate change","volume":"8","author":"Marzeion","year":"2014","journal-title":"Cryosphere"},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"195","DOI":"10.1016\/j.earscirev.2017.09.019","article-title":"Rapid decline of snow and ice in the tropical Andes\u2014Impacts, uncertainties and challenges ahead","volume":"176","author":"Vuille","year":"2018","journal-title":"Earth Sci. 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