A Correlated‐K Parameterization for O2 Photolysis in the Schumann‐Runge Bands

Author:

Ji Aoshuang1ORCID,Tomazzeli Orlando G.2ORCID,Palancar Gustavo G.345,Chaverot Guillaume6,Barker Mackenzie1,Fernández Rafael P.2ORCID,Minschwaner Kenneth7,Kasting James F.1ORCID

Affiliation:

1. Department of Geosciences Penn State University University Park PA USA

2. Institute for Interdisciplinary Science (ICB) National Research Council (CONICET) FCEN‐UNCUYO Mendoza Argentina

3. INFIQC: Instituto de Investigaciones en Fisicoquímica de Córdoba (CONICET—UNC)—Haya de la Torre y Medina Allende Ciudad Universitaria Córdoba Argentina

4. Departamento de Fisicoquímica Facultad de Ciencias Químicas—Universidad Nacional de Córdoba—Haya de la Torre y Medina Allende Ciudad Universitaria Córdoba Argentina

5. Centro Láser de Ciencias Moleculares Universidad Nacional de Córdoba—Haya de la Torre s/n Pabellón Argentina Ciudad Universitaria Córdoba Argentina

6. Observatoire Astronomique de l'Université de Genève Versoix Switzerland

7. Physics Department New Mexico Institute of Mining and Technology Socorro NM USA

Abstract

AbstractA recent study comparing ozone column depths and methane lifetimes at varied atmospheric O2 (pO2) levels calculated in the Kasting‐group 1‐D photochemical model and the Whole Atmosphere Community Climate Model version 6 (WACCM6) 3‐D model (Ji, Kasting, et al., 2023; https://doi.org/10.1098/rsos.230056) has exposed weaknesses in both models in parameterizing photolysis in the O2 Schumann‐Runge bands, 175–205 nm. WACCM6 does a good job for Earth's present atmosphere but neglects scattering, which becomes important at low pO2. The 1‐D model includes scattering but is based on an out‐of‐date band model, and it neglects the temperature dependence of photolysis at low pO2. We have revised and improved the 1‐D photochemical model by replacing the old O2 photolysis algorithm with a new correlated‐k parameterization, which improves accuracy for all O2 levels and all temperature profiles. The WACCM6 parameterization was also included in the 1‐D model for comparative purposes. The correlated‐k and WACCM6 photolysis algorithms agree well for both the present atmosphere and for an atmosphere containing 10−3 times the present O2 level, but only if multiple scattering is included at low pO2. The correlated‐k parameterization will be made available to photochemical modeling groups who might choose to adopt it.

Funder

Pennsylvania State University

Publisher

American Geophysical Union (AGU)

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