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You are here: Home / Data and maps / Maps and graphs / Observed and projected Arctic September sea-ice extent, 1900–2100

Observed and projected Arctic September sea-ice extent, 1900–2100

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Created : Jan 12, 2011 Published : Jan 13, 2011 Last modified : Nov 29, 2012 11:36 AM

Topics: Climate change ,

Observed and projected Arctic September sea-ice extent

This is the latest published version. .
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Sep 30, 2008 - Observed and projected Arctic September sea-ice extent 1900-2100

http://www.eea.europa.eu/data-and-maps/figures/observed-and-projected-arctic-september/ccs108_fig2-6.eps/image_original

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Metadata

Last upload:

29 Nov 2010

Dynamic

Temporal coverage:

1900-2098

Tags:

SOER2010 | climate change | thematic assessment | sea | ice extend | understanding climate change

Geographical coverage:

[+] Show Map

Arctic Ocean Norway

Rights:

EEA standard re-use policy: unless otherwise indicated, re-use of content on the EEA website for commercial or non-commercial purposes is permitted free of charge, provided that the source is acknowledged (http://www.eea.europa.eu/legal/copyright). Copyright holder: National Snow and Ice Data Center (NSIDC).

Owners:

National Snow and Ice Data Center (NSIDC)

Permalink to this version: 2244fb5c0c06afcd8b952641b3cb5e48
Permalink to latest version: UJBOV820GA

Figure type:

Graph

Additional information

The geographical coverage is Polar and Arctic areas, 1990 – 2100 (projections), September Ice extent

Related content

Used in publications

Understanding climate change — SOER 2010 thematic assessment

Understanding climate change — SOER 2010 thematic assessment Average global air and ocean temperatures are rising, leading to the melting of snow and ice and rising global mean sea level. Ocean acidification results from higher CO2 concentrations. With unabated greenhouse gas emissions, climate change could lead to an increasing risk of irreversible shifts in the climate system with potentially serious consequences. Temperature rises of more than 1.5–2 °C above pre-industrial levels are likely to cause major societal and environmental disruptions in many regions. The atmospheric CO2 concentration needs to be stabilised at 350–400 parts per million (ppm) in order to have a 50 % chance of limiting global mean temperature increase to 2 °C above pre-industrial levels (according to the IPCC in 2007, and confirmed by later scientific insights).

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Filed under: SOER2010, climate change, thematic assessment, sea, ice extend, understanding climate change

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