Surface ozone-temperature relationships in the eastern US: A monthly climatology for evaluating chemistry-climate models

By D. Rasmussen, A. Fiore, V. Naik, L. Horowitz, S. J. McGinnis, Martin G. Schultz. 2011

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1. Bernhard Schölkopf
2. Dominik Janzing
3. Jan Peters
4. Joris M. Mooij
5. David Lopez-Paz
6. Kun Zhang
7. Yoshua Bengio
8. Sergey Levine

Citations in the corpus

• Distinguishing Cause from Effect Using Observational Data: Methods and Benchmarks (2014, background): “Lower atmosphere ozone (O3) is a secondary pollutant that is produced by the photochemical oxidation of carbon monoxide (CO), methane (CH4), and non-methane volatile organic compounds (NMVOCs) by OH in the presence of nitrogen oxides (NOx, NO + NO2) (Rasmussen et al., 2012).”
• Distinguishing Cause from Effect Using Observational Data: Methods and Benchmarks (2014, background): “For instance, isoprene emissions of plants increase with increasing temperature and isoprene can play a similar role in the generation of O3 as NOx (Rasmussen et al., 2012).”