Author
Listed:
- P. K. Patra
(JAMSTEC, Yokohama 236 0001, Japan
CAOS, Graduate School of Studies, Tohoku University, Sendai 980 8578, Japan)
- M. C. Krol
(Wageningen University, Droevendaalsesteeg 3a, 6708 PB, The Netherlands)
- S. A. Montzka
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory)
- T. Arnold
(Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA)
- E. L. Atlas
(The Rosenstiel School of Marine and Atmospheric Science, University of Miami)
- B. R. Lintner
(Rutgers, The State University of New Jersey)
- B. B. Stephens
(National Center for Atmospheric Research (NCAR))
- B. Xiang
(School of Engineering and Applied Science, Harvard University)
- J. W. Elkins
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory)
- P. J. Fraser
(Centre for Australian Weather and Climate Research, Commonwealth Scientific and Industrial Research Organisation (CSIRO) Oceans and Atmosphere Flagship)
- A. Ghosh
(JAMSTEC, Yokohama 236 0001, Japan
National Institute of Polar Research, 10-3, Midoricho, Tachikawa, Tokyo 190-8518, Japan)
- E. J. Hintsa
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory
CIRES, University of Colorado)
- D. F. Hurst
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory
CIRES, University of Colorado)
- K. Ishijima
(JAMSTEC, Yokohama 236 0001, Japan)
- P. B. Krummel
(Centre for Australian Weather and Climate Research, Commonwealth Scientific and Industrial Research Organisation (CSIRO) Oceans and Atmosphere Flagship)
- B. R. Miller
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory
CIRES, University of Colorado)
- K. Miyazaki
(JAMSTEC, Yokohama 236 0001, Japan)
- F. L. Moore
(National Oceanic and Atmospheric Administration (NOAA) Earth System Research Laboratory
CIRES, University of Colorado)
- J. Mühle
(Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA)
- S. O’Doherty
(School of Chemistry, University of Bristol, Cantock’s Close, BS8 1TS, UK)
- R. G. Prinn
(Massachusetts Institute of Technology)
- L. P. Steele
(Centre for Australian Weather and Climate Research, Commonwealth Scientific and Industrial Research Organisation (CSIRO) Oceans and Atmosphere Flagship)
- M. Takigawa
(JAMSTEC, Yokohama 236 0001, Japan)
- H. J. Wang
(School of Earth and Atmospheric Sciences, Georgia Institute of Technology)
- R. F. Weiss
(Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA)
- S. C. Wofsy
(School of Engineering and Applied Science, Harvard University)
- D. Young
(School of Chemistry, University of Bristol, Cantock’s Close, BS8 1TS, UK)
Abstract
Observations of methyl chloroform combined with an atmospheric transport model predict a Northern to Southern Hemisphere hydroxyl ratio of slightly less than 1, whereas commonly used atmospheric chemistry models predict ratios 15–45% higher.
Suggested Citation
P. K. Patra & M. C. Krol & S. A. Montzka & T. Arnold & E. L. Atlas & B. R. Lintner & B. B. Stephens & B. Xiang & J. W. Elkins & P. J. Fraser & A. Ghosh & E. J. Hintsa & D. F. Hurst & K. Ishijima & P. , 2014.
"Observational evidence for interhemispheric hydroxyl-radical parity,"
Nature, Nature, vol. 513(7517), pages 219-223, September.
Handle:
RePEc:nat:nature:v:513:y:2014:i:7517:d:10.1038_nature13721
DOI: 10.1038/nature13721
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