Introduction of Water‐Vapor Broadening Parameters and Their Temperature‐Dependent Exponents Into the HITRAN Database: Part I—CO(2), N(2)O, CO, CH(4), O(2), NH(3), and H(2)S

The amount of water vapor in the terrestrial atmosphere is highly variable both spatially and temporally. In the tropics it sometimes constitutes 4–5% of the atmosphere. At the same time collisional broadening of spectral lines by water vapor is much larger than that by nitrogen and oxygen. Therefor...

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Detalles Bibliográficos
Autores principales: Tan, Y., Kochanov, R. V., Rothman, L. S., Gordon, I. E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919420/
https://www.ncbi.nlm.nih.gov/pubmed/31894194
http://dx.doi.org/10.1029/2019JD030929

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6919420/
https://www.ncbi.nlm.nih.gov/pubmed/31894194
http://dx.doi.org/10.1029/2019JD030929

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