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Historically unprecedented global glacier decline in the early 21st century

Michael ZempNational Correspondents* for 2 CH, 3 GL,Holger FreyNational Correspondents* for 2 CH, 3 GL,Isabelle Gärtner‐RoerWorld Glacier Monitoring Service (WGMS), Department of Geography, University of Zürich, Zürich, SwitzerlandSamuel U. NussbaumerNational Correspondents* for 2 CH, 3 GL,Martin HoelzleNational Correspondents* for 2 CH, 3 GL,Frank PaulNational Correspondents* for 2 CH, 3 GL,Wilfried HaeberliNational Correspondents* for 2 CH, 3 GL,Florian DenzingerNational Correspondents* for 2 CH, 3 GL,Andreas P. AhlstrømBrian AndersonNZ,Samjwal Ratna BajracharyaNP,Carlo BaroniIT,Ludwig N BraunDE,Bolívar CáceresGino CasassaGuillermo CobosLuzmila DávilaNational Correspondent for Spain (ES) & Antarctica (AQ), Universidad Politécnica de Valencia, Valencia, SpainHugo Delgado GranadosNational Correspondent for Peru (PE), Unidad de Glaciologa y Recursos Hdricos, Huaraz, PeruMichael N. DemuthNational Correspondent for Mxico (MX), Universidad Nacional Autnoma de Mxico, Mxico D.F., MxicoLydia E. EspizúaAndrea FischerNational Correspondent for Canada (CA), Natural Resources Canada, Ottawa, CanadaKoji FujitaFormer National Correspondent for Argentina (AR) & Antarctica (AQ), Instituto Argentino de Nivologa, Glaciologa y Ciencias Ambientales, Mendoza, ArgentinaBogdan GądekNational Correspondent for Austria (AT), sterreichische Akademie der Wissenschaften, Innsbruck, AustriaAli GhazanfarNational Correspondent for Japan (JP), Nagoya University, Nagoya, JapanJon Ove HagenNational Correspondent for Poland (PL), University of Silesia, Sosnowiec, PolandPer HolmlundNeamat KarimiNational Correspondent for Norway (NO), University of Oslo, Oslo, NorwayZhongqin LiNational Correspondent for Switzerland (CH), University of Fribourg, Fribourg, SwitzerlandMauri PeltoNational Correspondent for Sweden (SE), University of Stockholm, Stockholm, SwedenPierre PitteVictor PopovninCésar PortocarreroNational Correspondent for Spain (ES) & Antarctica (AQ), Universidad Politcnica de Valencia, Valencia, SpainR. PrinzNational Correspondent for the United States of America (US), Nichols College, Dudley, MA, USAChandrashekhar V. SangewarNational Correspondent for Russia (RU), Moscow State University, Moscow, RussiaIgor SeverskiyFormer National Correspondent for Peru (PE), Unidad de Glaciologa y Recursos Hdricos, Huaraz, PeruOddur SigurðssonNational Correspondent for Kenya (KE), Tanzania (TZ) & Uganda (UG), University of Innsbruck, Innsbruck, AustriaÁlvaro SorucoFormer National Correspondent for Colombia (CO), Instituto Colombiano de Geologa y Minera, Bogot, ColombiaRyskul UsubalievFormer National Correspondent for Australia (AU), Antarctica (AQ) & Indonesia (ID), Australian Antarctic Division, Victoria, AustraliaChristian VincentNational Correspondent for India (IN), Geological Survey of India, Lucknow, India
2015en
ABI

Annotatsiya

Abstract Observations show that glaciers around the world are in retreat and losing mass. Internationally coordinated for over a century, glacier monitoring activities provide an unprecedented dataset of glacier observations from ground, air and space. Glacier studies generally select specific parts of these datasets to obtain optimal assessments of the mass-balance data relating to the impact that glaciers exercise on global sea-level fluctuations or on regional runoff. In this study we provide an overview and analysis of the main observational datasets compiled by the World Glacier Monitoring Service (WGMS). The dataset on glacier front variations (∼42 000 since 1600) delivers clear evidence that centennial glacier retreat is a global phenomenon. Intermittent readvance periods at regional and decadal scale are normally restricted to a subsample of glaciers and have not come close to achieving the maximum positions of the Little Ice Age (or Holocene). Glaciological and geodetic observations (∼5200 since 1850) show that the rates of early 21st-century mass loss are without precedent on a global scale, at least for the time period observed and probably also for recorded history, as indicated also in reconstructions from written and illustrated documents. This strong imbalance implies that glaciers in many regions will very likely suffer further ice loss, even if climate remains stable.

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