Cumulative specific net mass balance of European glaciers

Data Visualization Created 22 Mar 2016 Published 20 Dec 2016 Last modified 03 Jan 2018

1 min read

Topics: Climate change adaptation ,

The figure shows the cumulative specific net mass balance of selected European glaciers, i.e. the change in glacier mass since the first year of their assessment. The start of the time series varies between glaciers.

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Data sources

Fluctuation of Glaciers Database (FoG) provided by World Glacier Monitoring Service (WGMS)

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Permalink to this version: 86643d6bc22c4cd9a6397791b609acd7
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Older versions

07 Apr 2014 - Cumulative net mass balance of European glaciers

18 Mar 2014 - Cumulative net mass balance of European glaciers

12 Jun 2012 - Cumulative specific net mass balance of European glaciers

Geographic coverage

Austria , Cima Careser (Lombardy, Italy) , Col de Sarennes (Auvergne-Rhône-Alpes, France) , Engabreen (Nordland, Norway) , France , Glacier de Saint-Sorlin (Auvergne-Rhône-Alpes, France) , Gries Glacier (Gries Glacier, 3988 Obergoms, Switzerland) , Grosser Vernagtferner (Austria) , Hintereisferner (Hintereisferner, 6458, Austria) , Hofsjökull (Northwest, Iceland) , Iceland , Nigardsbreen (Sogn og Fjordane, Norway) , Norway , Pico de la Maladeta (Aragon, Spain) , Spain , Storbreen (Oppland, Norway) , Storglaciären (Norrbotten, Sweden) , Svalbard and Jan Mayen , Sweden , Switzerland , Ålfotbreen (Ålfotbreen, Norway)

Temporal coverage

1946-2014

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For references, please go to https://www.eea.europa.eu/data-and-maps/daviz/cumulative-specific-net-mass-balance-2 or scan the QR code.

PDF generated on 25 May 2019, 05:35 AM

BISE	Biodiversity Information System for Europe
Climate-ADAPT	Climate Adaptation Platform
Copernicus In Situ	Copernicus in situ component
Copernicus Land	Copernicus land monitoring

European Pollutant Release and Transfer Register	E-PRTR
Information Platform for Chemical Monitoring	IPCHEM
Marine Water Information System for Europe	WISE-Marine
Fresh Water Information System for Europe	WISE-FreshWater

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