A photochemical model for the Venus atmosphere at 47–112 km
By V. Krasnopolsky. 2011
161 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/f7b3908daeb8c8df8c5dbd957231e3001b739957
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Aerospace Engineering
In Astronomy and Astrophysics
- A. Lincowski
- V. Meadows
- J. Lustig-Yaeger
- Giada N. Arney
- David Crisp
- N. Ignatiev
- V. Wilquet
- K. McGouldrick
Citations in the corpus
- Clouds and Hazes of Venus (2018, background): “26, potentially including hundreds of possible reactions (Krasnopolsky 2012; Zhang et al. 2012), produce sulphuric acid vapour in the middle atmosphere of Venus.”
- Evolved Climates and Observational Discriminants for the TRAPPIST-1 Planetary System (2018, methodology): “…is typically modeled in sections: by thermochemistry, which dominates the lower atmosphere below the cloud deck (e.g., Krasnopolsky 2013), and by photochemistry, which is responsible for the directly observable altitudes at and above the cloud deck (e.g., Krasnopolsky 2012; Zhang et al. 2012).”