Frequently Asked Questions About Ozone (3)
Scientific Assessment of Ozone Depletion: 1998
Executive Summary
World Meteorological Organization Global Ozone Research and Monitoring Project - Report No. 44
National Oceanic and Atmospheric Administration
National Aeronautics and Space Administration
World Meterological Organization
European Commission
United Nations Environment Programme
Does Most of the Chlorine in the Stratosphere Come from Human or Natural Sources?
Most of the chlorine in the stratosphere is there as a result of human activities, as the figure below illustrates.
Many compounds containing chlorine are released at the ground. Those that dissolve in water cannot reach stratospheric altitudes in significant amounts because they are "washed out" of the atmosphere in rain or snow. For example, large quantities of chlorine are released from evaporated ocean spray as sea salt (sodium chloride) particles. However, because sea salt dissolves in water, this chlorine is taken up quickly in clouds or in ice, snow, or rain droplets and does not reach the stratosphere. Another ground-level source of chlorine is from its use in swimming pools and as household bleach. When released, this chlorine is rapidly converted to forms that dissolve in water and therefore are removed from the lower atmosphere. Such chlorine never reaches the stratosphere in significant amounts. Volcanoes can emit large quantities of hydrogen chloride, but this gas is rapidly converted to hydrochloric acid, which dissolves in rain water, ice, and snow and does not reach the stratosphere. Even in explosive volcanic plumes that rise high in the atmosphere, nearly all of the hydrogen chloride is removed by precipitation before reaching stratospheric altitudes. Finally, although the exhaust from the Space Shuttle and from some rockets does inject some chlorine directly into the stratosphere, the quantities are very small (less than 1% of the annual input from halocarbons in the present stratosphere).
In contrast, the major ozone-depleting human-produced halocarbons --such as chlorofluorocarbons (CFCs) and carbon tetrachloride (CCl4)-- do not disolve in water, do not react with snow or other natural surfaces, and are not broken down chemically in the lower atmosphere. Therefore, these and other human-produced substances containing chlorine do reach the stratosphere.
Several pieces of evidence combine to establish human-produced halocarbons as the primary source of stratospheric chlorine. First, measurements have shown that the chlorinated species that rise to the stratosphere are primarily manufactured compounds [mainly CFCs, carbon tetrachloride, methyl chloroform, and the hydrochlorofluorocarbon (HCFC) substitutes for CFCs], together with small amounts of hydrochloric acid (HCl) and methyl chloride (CH3Cl), which are partly natural in origin. Second, researchers have measured nearly all known gases containing chlorine in the stratosphere. They have found that the emissions of the human-produced halocarbons, plus the much smaller contribution from natural sources, could account for all of the stratospheric chlorine. Third, the increase in total stratospheric chlorine measured between 1980 and 1998 corresponds to the known increases in concentrations of human-produced halocarbons during that time.
Primary Sources of Chlorine Entering the Stratosphere in the Early 1990s
Frequently Asked Questions about Ozone
- Introduction
- How can chlorofluorocarbons (CFCs) get to the stratosphere if they're heavier than air?
- What is the evidence that stratospheric ozone is destroyed by chlorine and bromine?
- [Does most of the chlorine in the stratosphere come from human or natural sources?]
- Can natural changes such as the Sun's output and volcanic erruptions be responsible for the observed changes in ozone?
- When did the Antarctic ozone hole first appear?
- Why has an ozone hole appeared over Antarctica when CFCs and halons are released mainly in the Northern Hemisphere?
- Is there an ozone hole over the Arctic?
- Is the depletion of the ozone layer leading to an increase in ground-level ultraviolet radiation?
- Does ozone depletion cause climate change?
- How severe is the ozone depletion now?
- Is the ozone layer expected to recover? If so, when?
Return to the WMO/UNEP Scientific Assessment of Ozone Depletion: 1998
- Executive Summary
- Frequently Asked Questions about Ozone
- List of Authors, Contributors, and Reviewers of the Assessment
The World Wide Web version of the Executive Summary of the WMO/UNEP Scientific Assessment of Ozone Depletion: 1998 was prepared by Catherine A. Burgdorf of the NOAA Aeronomy Lab, Boulder, Colorado, in cooperation with Dr. Daniel L. Albritton and Dr. Christine A. Ennis of the NOAA Aeronomy Laboratory.
The Executive Summary may be reproduced or excerpted, without modification, provided the source is duly and conspicuously acknowledged in every instance as:
World Meteorological Organization, Scientific Assessment of Ozone Depletion: 1998, WMO Global Ozone Research and Monitoring Project - Report No. 44, Geneva, 1998.
Copies of the Executive Summary are available at no charge by writing to:
United Nations Environment Programme
Ozone Secretariat
P.O. Box 30552
Nairobi, Kenya
The Executive Summary was published in print in March 1999. The World Wide Web version was derived directly from the source of the printed edition and was made public in April 1999.