Solar Radiation, Aerosol, and Multiple Interactions Between Solar Radiation and Atmospheric Substances

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Biosphere/Hydrosphere/Land–Atmosphere Interactions".

Deadline for manuscript submissions: 31 March 2025 | Viewed by 466

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Guest Editor
LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Interests: solar radiation; trace gases; ozone; BVOCs; atmospheric chemistry; carbon balance; climate and climate change; interactions between solar radiation and atmospheric substances
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Guest Editor
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Interests: remote sensing application and numerical model on land-atmosphere interaction; atmospheric boundary layer meteorology
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Special Issue Information

Dear Colleagues,

Solar radiation plays a vital role in the atmosphere, biosphere, hydrosphere, lithosphere, and their interactions on Earth. The atmospheric compositions can vary drastically with the rapid change in human and global activities, for example, in industrial developments, including the agricultural and chemical industries, land use, deforestation, and biomass burning. Such activities either directly emit gases, liquids, and particles (or aerosols) from all kinds of sources or lead to their indirect production through chemical and photochemical reactions in the atmosphere. NOx, SO2, O3, anthropogenic and biogenic volatile organic compounds (AVOCs, BVOCs), organic carbon and black carbon (OC, BC), secondary organic aerosol (SOA), and other components all interact with each other, with other aerosols and clouds, as well as with solar radiation in the UV, visible, and near-infrared regions. Different aerosols show different absorbing and scattering features that depend on the region and source. Investigating the variation in the atmospheric constituents including aerosol, clouds, polluted gases, and particles, along with their interactions with each other and impacts on solar radiation, is particularly important.

To better understand the carbon balance in ecosystems and its roles in climate change, it is necessary to study all components of carbon exchange and their driving factors, along with their variations at different time scales.

Solar radiation controls climate change and ecosystem evolution (including the response of forest ecosystem); in turn, the changes in the atmosphere, ecosystem, and land also influence solar radiation transfer in the atmosphere, along with regional and global climate and climate change through multiple interactions. Therefore, the means with which solar radiation, alongside its interaction with atmospheric substances, contributes to climate change at different time scales (e.g., extending to hundreds or thousands of years) warrants investigation. Until now, surface and satellite observations and model studies have been reliably effective tools to thoroughly study the above natural processes, interactions, and mechanisms.

The purpose of this Special Issue is to collect and exchange current studies concerning the above associated issues to improve our understanding of solar radiation, atmosphere, biosphere, land, and climate, especially their interactions (i.e., between solar radiation and gas, liquid, and particle compositions in the atmosphere), in representative regions (e.g., the three poles) and in the world. All associated submissions are strongly welcome and encouraged.

Prof. Dr. Jianhui Bai
Prof. Dr. Weiqiang Ma
Guest Editors

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Keywords

  • solar radiation (global, UV, visible, near infrared, etc.)
  • aerosol, clouds
  • anthropogenic and biogenic volatile organic compounds (AVOCs, BVOCs)
  • carbon balance (gross primary production (GPP), respiration (Re), and net ecosystem exchange (NEE))
  • climate and climate change
  • paleoclimate
  • in situ observations and remote sensing inversions
  • surface energy budget
  • solar radiation–atmospheric substance interaction
  • land–atmosphere interaction
  • solar radiation–atmospheric substance–climate interactions

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Published Papers (1 paper)

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Research

26 pages, 8084 KiB  
Article
Multiple-Win Effects and Beneficial Implications from Analyzing Long-Term Variations of Carbon Exchange in a Subtropical Coniferous Plantation in China
by Jianhui Bai, Fengting Yang, Huimin Wang, Lu Yao and Mingjie Xu
Atmosphere 2024, 15(10), 1218; https://doi.org/10.3390/atmos15101218 - 12 Oct 2024
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Abstract
To improve our understanding of the carbon balance, it is significant to study long-term variations of all components of carbon exchange and their driving factors. Gross primary production (GPP), respiration (Re), and net ecosystem productivity (NEP) from the hourly to the annual sums [...] Read more.
To improve our understanding of the carbon balance, it is significant to study long-term variations of all components of carbon exchange and their driving factors. Gross primary production (GPP), respiration (Re), and net ecosystem productivity (NEP) from the hourly to the annual sums in a subtropical coniferous forest in China during 2003–2017 were calculated using empirical models developed previously in terms of PAR (photosynthetically active radiation), and meteorological parameters, GPP, Re, and NEP were calculated. The calculated GPP, Re, and NEP were in reasonable agreement with the observations, and their seasonal and interannual variations were well reproduced. The model-estimated annual sums of GPP and Re over 2003–2017 were larger than the observations of 11.38% and 5.52%, respectively, and the model-simulated NEP was lower by 34.99%. The GPP, Re, and NEP showed clear interannual variations, and both the calculated and the observed annual sums of GPPs increased on average by 1.04% and 0.93%, respectively, while the Re values increased by 4.57% and 1.06% between 2003 and 2017. The calculated and the observed annual sums of NEPs/NEEs (net ecosystem exchange) decreased/increased by 1.04%/0.93%, respectively, which exhibited an increase of the carbon sink at the experimental site. During the period 2003–2017, the annual averages of PAR and the air temperature decreased by 0.28% and 0.02%, respectively, while the annual average water vapor pressure increased by 0.87%. The increase in water vapor contributed to the increases of GPP, Re, and NEE in 2003–2017. Good linear and non-linear relationships were found between the monthly calculated GPP and the satellite solar-induced fluorescence (SIF) and then applied to compute GPP with relative biases of annual sums of GPP of 5.20% and 4.88%, respectively. Large amounts of CO2 were produced in a clean atmosphere, indicating a clean atmospheric environment will enhance CO2 storage in plants, i.e., clean atmosphere is beneficial to human health and carbon sink, as well as slowing down climate warming. Full article
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