The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
A persistent imbalance in HOx and NOx photochemistry of the upper troposphere driven by deep tropical convection
Open accessAbstract
Convection in the tropics turns over the upper troposphere at rates (0.08 d−1) comparable to photochemical processes controlling the absolute abundance of HO x (OH + HO 2) and the abundance of NO x (NO + NO 2) relative to HNO 3. Here we identify convection of boundary‐layer CH 3 OOH as a primary source of HO x to the upper troposphere. Turnover of NO x leads to NO/HNO 3 ratios much higher than predicted for local photochemical steady‐state. Through convective transport the upper troposphere is more photochemically active in producing O 3, an important greenhouse gas.
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Cites
Emanuel, K. A. (1994) · doi:10.1093/oso/9780195066302.001.0001 · Cited by 1,205
Cited by
Introduction to Atmospheric Chemistry
Jacob, D. J. (2000) · Princeton University Press eBooks · doi:10.1515/9781400841547 · Cited by 854
Self-citationChemistry of HOx radicals in the upper troposphere
Jaeglé, L. (2001) · Atmospheric Environment · doi:10.1016/s1352-2310(00)00376-9 · Cited by 217
The oxygen to carbon dioxide ratios observed in emissions from a wildfire in northern California
Lueker, T. J., Keeling, R. F., & Dubey, M. K. (2001) · Geophysical Research Letters · doi:10.1029/2000gl011860 · Cited by 26
Metadata
- Authors
- Prather, M. J., & Jacob, D. J.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 1997-12-15
- Volume
- 24
- Issue
- 24
- Pages
- 3189-3192
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2079222644
- Cited by
- 168
- References
- 1
- FWCI
- 7.44
- Type
- journal article
- Language
- en
- Open access
- green
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- Prather, M. J., & Jacob, D. J. (1997). A persistent imbalance in HOx and NOx photochemistry of the upper troposphere driven by deep tropical convection. Geophysical Research Letters. https://doi.org/10.1029/97gl03027
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