Figure
Maximum historical depletion over the southern hemisphere (9 September 2000) and over the northern hemisphere (22 March 2011)
Figure
Created 29 Feb 2016
Published 29 Aug 2016
Last modified 26 Aug 2017
1
min read
This is an old version, kept for reference only.
Go to latest version
Go to latest version
Topics:
Climate change adaptation
This page was archived on 26 Aug 2017 with reason:
A new version has been published
False-colour view of total ozone over the North (Arctic) and South (Antarctic) poles. The purple and blue colours indicate lowest ozone presence, while yellow and red indicate higher ozone presence. Ozone concentration is commonly measured in Dobson Units. One Dobson Unit is the number of molecules of ozone that would be required to create a layer of pure ozone 0.01 millimetres thick at a temperature of 0 degrees Celsius and a pressure of 1 atmosphere.
Metadata
-
Units:
Dobson 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 (https://www.eea.europa.eu/legal/copyright). Copyright holder: NASA.
-
Owners:
- NASA
-
Processors:
- NASA
-
Figure type:
- Map
Permalinks
- Permalink to this version
- 4efc99ec480f499782011634e5a048ca
- Permalink to latest version
- D7EUD5SKDH
Older versions
Geographic coverage
Temporal coverage
2000
2011
For references, please go to https://www.eea.europa.eu/data-and-maps/figures/maximum-ozone-hole-area-in-3 or scan the QR code.
PDF generated on 25 Jun 2021, 12:53 PM
Topics
Topics:
Climate change adaptation
Document Actions
Share with others