Historically unprecedented global glacier decline in the early 21st century
Zemp, Michael; Frey, Holger; Garnert-Roer, Isabelle; Nussbaumer, Samuel U.; Hoelzle, Martin; Paul, Frank; Haeberli, Wilfried; Denzinger, Florian; Anderson, Brian; Bajracharya, Samjwal; Baroni, Carlo; Braun, Ludwing N.; Cáceres, Bolívar E.; Casassa, Gino; Dávila, Luzmila R.; Delgado Granados, Hugo; Demuth, Michael N.; Espizua, Lydia; Fisher, Andrea; Fujita, Koji; Gadek, Bogdan; Ghazanfar, Ali; Hagen, Jon Ovi; Holmlund, Per; Karimi, Neamat; Li, Zhonqin; Pelto, Mauri; Pitte, Pierre; Popovnin, Victor V.; Portocarrero, Cesar A.; Prinz, Rainer; Sangewar, Chandrashekhar; Severskiy, Igor; Sigurdsson, Oddur; Soruco, Alvaro; Usubaliev, Ryskul; Vincent, Christian; Ahlstrom, Andreas P.; Cobos, Guillermo
Date:
2015
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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