Global Atmosphere Watch: monitoring of the ozone layer

Ozone layer observations

Ozone constitutes a very small part of our atmosphere, but its presence is nevertheless vital to human well-being. Most ozone resides high up in the atmosphere, between 10 and 40km above Earth's surface. This region is called the stratosphere and it contains about 90% of all the ozone in the atmosphere.

Why do we care about atmospheric ozone?

Ozone in the stratosphere absorbs some of the Sun’s biologically harmful ultraviolet radiation. Because of this beneficial role, stratospheric ozone is considered “good” ozone. In contrast, excess ozone at Earth’s surface that is formed from pollutants is considered “bad” ozone because it can be harmful to humans, plants, and animals. The ozone that occurs naturally near the surface and in the lower atmosphere is also beneficial because ozone helps remove pollutants from the atmosphere.

WMO informs about the ozone layer

WMO informs about the state of the ozone layer in several ways:

WMO Antarctic Ozone Bulletins

2008
2007	2006

An Overview of the 2005 Antarctic Ozone Hole,
by Geir O. Braathen (Warning: 26 MByte)

The most recent Antarctic Ozone Bulletin in Spanish 

Ozone web page of the Servicio Meteorológico Nacional of Argentina

WMO Antarctic Ozone Bulletins from earlier years

Background information and summaries (1995-2003) by Andreas Fischer

WMO Arctic Ozone Bulletins

The Secretariat of the World Meteorological Organization, in collaboration with the European Ozone Reserarch Coordinating Unit, issues annual bulletins containing information on the development of the Arctic ozone layer over the course of each winter.  The bulletins are based on data provided by WMO Members that operate atmospheric monitoring stations in the Arctic and satellites to observe ozone and related parameters globally.

2006

The 2006 issue is the first joint WMO/EC Arctic Ozone Bulletin. The next Arctic Ozone Bulletin is planned for June 2007.

The 7th Ozone Research Managers' Meeting: Geneva 18-21 May 2008

Information on the 7th ORM can be found here.

WMO/UNEP Scientific Assessment of Ozone Depletion

2006	2002

More information about the WMO/UNEP Scientific Assessments of Ozone Depletion can be found at the ozone assessment web pages of NOAA.

WMO brochure on the protection of the ozone layer

English

French

WMO coordinates the global ozone observing network

The WMO-GAW ozone observing system comprises more than 100 stations worldwide that measure total column ozone and ozone profiles in the troposphere and stratosphere. The WMO secretariat coordinates training and calibration excercises. The WMO-GAW World Calibration Centre for Dobson total ozone measurements is located at the Global Monitoring Division of NOAA. The WMO-GAW World Calibration Centre for Brewer total ozone measurements is located at Environment Canada.The WMO-GAW World Calibration Centre for ozonesonde measurements is located at Forschungszentrum Jülich, Germany.

The WMO-GAW ozone observing system provides important data for the assessment of the state of the ozone layer and the data are used in the quadrennial WMO/UNEP Scientific Assessment of Ozone Depletion (see above). Data from Antarctica are delivered in near-real time and used in the WMO Antarctic Ozone Bulletins (see above).

Data from the WMO-GAW ozone observing system are collected and stored at the WMO World Ozone and Ultraviolet Radiation Data Centre (WOUDC) at Environment Canada, Toronto.

Contributing Networks

Several observational networks are contributing to the overall GAW system. In the field of ozone observations these two networks are linked to GAW. Click on them to go to their respective web sites.

Network for the Detection of Atmospheric Composition Change (NDACC)
Southern Hemisphere Additional Ozone Sonde Network (SHADOZ)

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