Reconstructed histories of the annual mean atmospheric mole fractions for the halocarbons CFC-11 CFC-12, CFC-113, and carbon tetrachloride

Annual mean mixing ratios for the halocarbons CFC‐11 (CCl3F), CFC‐12 (CCl2F2), CFC‐113 (CClF2CCl2F), and carbon tetrachloride (CCl4) have been determined from their first year of industrial production through 1998. From the late 1970s (in the case of CFC‐11 and CFC‐12) or early 1980s (in the case of...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of Geophysical Research 2000-06, Vol.105 (C6), p.14285-14296
Hauptverfasser: Walker, S. J., Weiss, R. F., Salameh, P. K.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Annual mean mixing ratios for the halocarbons CFC‐11 (CCl3F), CFC‐12 (CCl2F2), CFC‐113 (CClF2CCl2F), and carbon tetrachloride (CCl4) have been determined from their first year of industrial production through 1998. From the late 1970s (in the case of CFC‐11 and CFC‐12) or early 1980s (in the case of CFC‐113 and carbon tetrachloride) the reported mixing ratios have been determined from experimental observations made by the Atmospheric Lifetime Experiment/Global Atmospheric Gases Experiment/Advanced Global Atmospheric Gases Experiment program. For years prior to these times we have used estimates of industrial emissions and atmospheric lifetimes to calculate historic concentrations. The likely error bounds of the annual mean values are also reported here. Errors in the annual mean mixing ratio may primarily be a result of incorrect industrial emissions data, an incorrect atmospheric lifetime, or uncertainty in the ALE/GAGE/AGAGE observations. Each of these possible sources of error has been considered separately. These results show that atmospheric concentrations for each of these compounds have experienced a rapid rise in the early part of their production. It is only within the past decade that rise rates have decreased sharply and (except in the case of CFC‐12) in the past few years that atmospheric concentrations have begun to decrease. The uncertainties in the reconstructed histories are a similar proportion for each of the chlorofluorocarbons (
ISSN:0148-0227
2169-9275
2156-2202
2169-9291
DOI:10.1029/1999JC900273