Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module

This study analyses the wide-band algorithm, Cloud-J v.8.0, from the point of view of the validity of the choice of wide spectral intervals to accelerate the calculations of photolysis rates in the lower and middle atmosphere, considering the features of solar radiation propagation, and to assess th...

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Main Authors: Anastasia Imanova, Eugene Rozanov, Sergei Smyshlyaev, Vladimir Zubov, Tatiana Egorova
Format: Article
Language:English
Published: MDPI AG 2025-01-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/16/1/58
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author Anastasia Imanova
Eugene Rozanov
Sergei Smyshlyaev
Vladimir Zubov
Tatiana Egorova
author_facet Anastasia Imanova
Eugene Rozanov
Sergei Smyshlyaev
Vladimir Zubov
Tatiana Egorova
author_sort Anastasia Imanova
collection DOAJ
description This study analyses the wide-band algorithm, Cloud-J v.8.0, from the point of view of the validity of the choice of wide spectral intervals to accelerate the calculations of photolysis rates in the lower and middle atmosphere, considering the features of solar radiation propagation, and to assess the influence of the processes of reflection and scattering on molecules, aerosols, and clouds. The results show that the calculations performed using Cloud-J v.8.0 are in agreement with the data obtained using the high-resolution LibRadtran model. The study also considers the factors influencing the propagation of the solar flux through the atmosphere in Cloud-J v.8.0, which occurs following theoretical concepts. It is shown that the presence of cloud layers can increase photolysis rates by up to 40% in the above-cloud layer and decrease them by up to 20% below the cloud layer. The presence of volcanic aerosol can increase the photolysis rates in the upper part of the layer and above it by up to 75% and decrease them by up to 75% in the underlying atmosphere. Rayleigh scattering can both enhance photolysis rates in the troposphere and reduce them at large zenith angles. Thus, Cloud-J offers a robust method for modelling atmospheric photodissociation processes with high computational efficiency.
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spelling doaj-art-31e5e06d4b074bbcabf179ebfd0423af2025-01-24T13:21:52ZengMDPI AGAtmosphere2073-44332025-01-011615810.3390/atmos16010058Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J ModuleAnastasia Imanova0Eugene Rozanov1Sergei Smyshlyaev2Vladimir Zubov3Tatiana Egorova4Laboratory for the Study of the Ozone Layer and the Upper Atmosphere, Saint-Petersburg State University, 199034 Saint Petersburg, RussiaLaboratory for the Study of the Ozone Layer and the Upper Atmosphere, Saint-Petersburg State University, 199034 Saint Petersburg, RussiaFaculty of Meteorology, Russian State Hydrometeorological University, 195196 Saint Petersburg, RussiaVoeikov Main Geophysical Observatory, 194021 Saint Petersburg, RussiaPhysical-Meteorological Observatory Davos/World Radiation Center (PMOD/WRC), CH-7260 Davos, SwitzerlandThis study analyses the wide-band algorithm, Cloud-J v.8.0, from the point of view of the validity of the choice of wide spectral intervals to accelerate the calculations of photolysis rates in the lower and middle atmosphere, considering the features of solar radiation propagation, and to assess the influence of the processes of reflection and scattering on molecules, aerosols, and clouds. The results show that the calculations performed using Cloud-J v.8.0 are in agreement with the data obtained using the high-resolution LibRadtran model. The study also considers the factors influencing the propagation of the solar flux through the atmosphere in Cloud-J v.8.0, which occurs following theoretical concepts. It is shown that the presence of cloud layers can increase photolysis rates by up to 40% in the above-cloud layer and decrease them by up to 20% below the cloud layer. The presence of volcanic aerosol can increase the photolysis rates in the upper part of the layer and above it by up to 75% and decrease them by up to 75% in the underlying atmosphere. Rayleigh scattering can both enhance photolysis rates in the troposphere and reduce them at large zenith angles. Thus, Cloud-J offers a robust method for modelling atmospheric photodissociation processes with high computational efficiency.https://www.mdpi.com/2073-4433/16/1/58photolysis ratesstratospheric chemistrycloud and aerosol scatteringRayleigh scattering
spellingShingle Anastasia Imanova
Eugene Rozanov
Sergei Smyshlyaev
Vladimir Zubov
Tatiana Egorova
Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
Atmosphere
photolysis rates
stratospheric chemistry
cloud and aerosol scattering
Rayleigh scattering
title Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
title_full Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
title_fullStr Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
title_full_unstemmed Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
title_short Investigation of the Influence of Atmospheric Scattering on Photolysis Rates Using the Cloud-J Module
title_sort investigation of the influence of atmospheric scattering on photolysis rates using the cloud j module
topic photolysis rates
stratospheric chemistry
cloud and aerosol scattering
Rayleigh scattering
url https://www.mdpi.com/2073-4433/16/1/58
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AT eugenerozanov investigationoftheinfluenceofatmosphericscatteringonphotolysisratesusingthecloudjmodule
AT sergeismyshlyaev investigationoftheinfluenceofatmosphericscatteringonphotolysisratesusingthecloudjmodule
AT vladimirzubov investigationoftheinfluenceofatmosphericscatteringonphotolysisratesusingthecloudjmodule
AT tatianaegorova investigationoftheinfluenceofatmosphericscatteringonphotolysisratesusingthecloudjmodule