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We evaluated the impact of climate warming on snowmelt rates using the GlobSnow v2.0 and the second Modern\u2010Era Retrospective analysis for Research and Applications data sets over the Northern Hemisphere (NH) during the past 38\u00a0years (1980\u20132017). Higher ablation rates were found in the locations with deeper snow water equivalent (SWE) because high snow melt rates occurred in late spring and early summer in deep snowpack regions. In addition, due to the reduction of SWE in deep snowpack regions, moderate and high snow ablation rates showed a decreasing trend. Therefore, slower snowmelt rates were found over the entire NH in a warmer climate in general. Based on projections of SWE in Representative Concentration Pathways 2.6, 4.5, and 8.5 climate scenarios, slower snowmelt rates in the NH may continue to happen in the future.<\/jats:p>","DOI":"10.1029\/2018gl079511","type":"journal-article","created":{"date-parts":[[2018,11,5]],"date-time":"2018-11-05T21:10:45Z","timestamp":1541452245000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":54,"title":["Slower Snowmelt in Spring Along With Climate Warming Across the Northern Hemisphere"],"prefix":"10.1029","volume":"45","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-8559-1599","authenticated-orcid":false,"given":"Xuejiao","family":"Wu","sequence":"first","affiliation":[{"name":"State Key Laboratory of Cryospheric Science, Cold and Arid Regions Environmental and Engineering Research Institute Chinese Academy of Sciences  Lanzhou China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6848-7271","authenticated-orcid":false,"given":"Tao","family":"Che","sequence":"additional","affiliation":[{"name":"Key Laboratory of Remote Sensing of Gansu Province, Heihe Remote Sensing Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute Chinese Academy of Sciences  Lanzhou China"},{"name":"Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-2999-9818","authenticated-orcid":false,"given":"Xin","family":"Li","sequence":"additional","affiliation":[{"name":"Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences  Beijing China"},{"name":"Institute of Tibetan Plateau Research Chinese Academy of Sciences  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Ninglian","family":"Wang","sequence":"additional","affiliation":[{"name":"Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences  Beijing China"},{"name":"Institute of Earth Surface System and Hazards, College of Urban and Environmental Sciences Northwestern University  Xi'an China"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7030-7516","authenticated-orcid":false,"given":"Xiaofan","family":"Yang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science Beijing Normal University  Beijing China"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"13","published-online":{"date-parts":[[2018,11,20]]},"reference":[{"key":"e_1_2_7_2_1","doi-asserted-by":"publisher","DOI":"10.1007\/s00382-017-3955-8"},{"key":"e_1_2_7_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0959-3780(98)00015-6"},{"key":"e_1_2_7_4_1","doi-asserted-by":"publisher","DOI":"10.1038\/nature04141"},{"key":"e_1_2_7_5_1","doi-asserted-by":"publisher","DOI":"10.1002\/2016GL069690"},{"key":"e_1_2_7_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jhydrol.2015.03.025"},{"key":"e_1_2_7_7_1","doi-asserted-by":"publisher","DOI":"10.1007\/s13280-012-0310-5"},{"key":"e_1_2_7_8_1","unstructured":"Bosilovich M. 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