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A global inventory of stratospheric fluorine in 2004 based on Atmospheric Chemistry Experiment Fourier transform spectrometer (ACE-FTS) measurements

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Published copy (DOI)

Author(s)

  • R. Nassar
  • P. F. Bernath
  • C. D. Boone
  • S. D. McLeod
  • R. Skelton
  • K. A. Walker
  • C. P. Rinsland
  • P. Duchatelet

Department/unit(s)

Publication details

JournalJournal of Geophysical Research
DatePublished - 30 Nov 2006
Issue numberD22
Volume111
Number of pages10
Pages (from-to)-
Original languageEnglish

Abstract

[1] Total fluorine (F-TOT) in the stratosphere has been determined using Atmospheric Chemistry Experiment Fourier transform spectrometer (ACE-FTS) measurements of HF, COF2, COClF, CF4, CCl3F (CFC-11), CCl2F2 (CFC-12), CHClF2 (HCFC-22), CCl2FCClF2 (CFC-113), CH3CClF2 (HCFC-142b), CH2FCF3 (HFC-134a), and SF6. The retrieval of HFC-134a (CH2FCF3) from spaceborne measurements had not been carried out prior to this work. Measurements of these species have been supplemented by data from models to extend the altitude range of the profiles and have also been complemented by estimates of 15 minor fluorine species. Using these data, separate fluorine budgets were determined in five latitude zones (60 degrees - 82 degrees N, 30 degrees - 60 degrees N, 30 degrees S - 30 degrees N, 30 degrees - 60 degrees S, and 60 degrees - 82 degrees S) by averaging over the period of February 2004 to January 2005 inclusive, when possible. Stratospheric FTOT profiles in each latitude zone are nearly linear, with mean stratospheric FTOT values ranging from 2.50 to 2.59 ppbv (with a 1 sigma precision of 0.04 - 0.07 ppbv and an estimated accuracy of 0.15 ppbv) for each zone. The highest mean F-TOT value occurred in the tropics, which is qualitatively consistent with increasing levels of stratospheric fluorine and the mean stratospheric circulation pattern.

    Research areas

  • HALOGEN OCCULTATION EXPERIMENT, CROSS-SECTIONS, CHLORINE, HYDROHALOCARBONS, LIFETIMES, BUDGET, MODEL

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