Change in global mean sea level

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Created : Oct 18, 2012 Published : Nov 08, 2012 Last modified : Nov 29, 2012 11:42 AM

The figure shows the global mean sea level from 1860 to 2009 as estimated from coastal and island sea-level data (1880 – 2009, blue) and from satellite altimeter data (1993 – 2009, grey).

This is the latest published version. .

http://www.eea.europa.eu/data-and-maps/figures/change-in-global-mean-sea/fig3.6_cz01_change_in_global_mean_sea_level_jc.xlsx/image_original

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CZ01_change_in_global_mean_sea_level_JC.xlsx

Metadata

Last upload:

18 Oct 2012

Dynamic

Temporal coverage:

1880-2009

Tags:

climate change | coastal zones | sea level

Geographical coverage:

[+] Show Map

Arctic Ocean Atlantic Ocean Austria Baltic Sea Belgium Black Sea Bulgaria Cyprus Czech Republic Denmark Estonia Finland France Germany Greece Hungary Indian Ocean Ireland Italy Latvia Lithuania Luxembourg Malta Netherlands North Atlantic Ocean North Sea Pacific Ocean Poland Portugal Romania Slovakia Slovenia South Atlantic Ocean Tonga Southern Ocean Spain Sweden United Kingdom

Methodology:

http://www.springerlink.com/content/h2575k28311g5146/fulltext.pdf

Units:

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: European Environment Agency (EEA).

Owners:

European Environment Agency (EEA)

Processors:

Commonwealth Scientific and Industrial Research Organisation (CSIRO)

Permalink to this version: ef65b51f17d44b329fe0d27d836e264a
Permalink to latest version: NP871ZTVA0

Figure type:

Graph

Additional information

Geographical coverage is global.

“While we attempted the reconstruction back to 1860, the results showed greater sensitivity to details of the method prior to the 1880s when the first southern hemisphere record is available (see below for further discussion). As a result, while we show the reconstruction back to 1860, we restricted the subsequent analysis (computation of trends, etc.) to after 1880.
“Prior to 1880 when there were less than 15 locations available and none in the southern hemisphere, there was considerably greater sensitivity to the parameter choice than for the rest of the record and hence we focus on results after 1880.”

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