Why are there large differences between models in global budgets of tropospheric ozone
By Shiliang Wu, L. Mickley, D. J. Jacob, J. Logan, R. Yantosca, D. Rind. 2007
312 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/9b5fed055036be5d93b8e2bd008a48ea4bca403d
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Randall V. Martin
- Xiong Liu
- A. Donkelaar
- D. Rasmussen
- S. J. McGinnis
- Paul I. Palmer
- A. Fiore
- V. Naik
In Global and Planetary Change
- Xiong Liu
- Randall V. Martin
- A. Donkelaar
- Paul I. Palmer
- Kelly Chance
- L. Jaeglé
- Martin G. Schultz
- Shiliang Wu
Citations in the corpus
- Transport impacts on atmosphere and climate: Aviation (2009, unknown): “Wu et al.”
- Global health and economic impacts of future ozone pollution (2009, methodology): “Climate changes are simulated by the NASA/GISS GCM 3 (Rind et al 2007) and are used to drive GEOS-Chem as described by Wu et al (2007).”
- Optimized regional and interannual variability of lightning in a global chemical transport model constrained by LIS/OTD satellite data (2012, unknown): “Hamid et al. [2001] noted that lightning frequencies in the tropics are very sensitive to small increases in surface air temperature [ Williams , 1992] and that the surface temperature over the tropical land generally increases during the positive phase of ENSO [ Hansen and Lebedeff , 1987].”
- Surface ozone-temperature relationships in the eastern US: A monthly climatology for evaluating chemistry-climate models (2011, background): “…chemistry likely contributes; surface O3 over the eastern US is highly sensitive to the treatment of isoprene nitrate (RONO2) chemistry and whether isoprene nitrates represent a terminal or interim sink for NOx (Fiore et al., 2005; Horowitz et al., 2007; Ito et al., 2009; Wu et al., 2007).”
- Remote sensed and in situ constraints on processes affecting tropical tropospheric ozone (2006, background): “Cloud optical depths are smaller in GEOS-4 than GEOS-3 leading to more active photochemistry (Liu et al., 2006; Wu et al., 2007).”