| Autor: |
Zhu, Yunqian1,2 (AUTHOR) yunqian.zhu@colorado.edu, Yu, Pengfei3 (AUTHOR), Wang, Xinyue4 (AUTHOR), Bardeen, Charles5 (AUTHOR), Borrmann, Stephan6,7 (AUTHOR), Höpfner, Michael8 (AUTHOR), Mahnke, Christoph6,9 (AUTHOR), Weigel, Ralf7 (AUTHOR), Krämer, Martina7,10 (AUTHOR), Deshler, Terry11,12 (AUTHOR), Bian, Jianchun10,13 (AUTHOR), Bai, Zhixuan13 (AUTHOR), Vernier, Hazel14,15 (AUTHOR), Portmann, Robert W.2 (AUTHOR), Rosenlof, Karen H.2 (AUTHOR), Kloss, Corinna14,16 (AUTHOR), Pan, Laura L.5 (AUTHOR), Smith, Warren5 (AUTHOR), Honomichl, Shawn5 (AUTHOR), Zhang, Jun5 (AUTHOR) |
| Předmět: |
|
| Zdroj: |
Journal of Geophysical Research. Atmospheres. 10/16/2024, Vol. 129 Issue 19, p1-15. 15p. |
| Abstrakt: |
The Asian Summer Monsoon (ASM) convection transports aerosols and their precursors from the boundary layer to the upper troposphere and lower stratosphere (UTLS). This process forms an annually recurring aerosol layer near the tropopause. Recent observations have revealed a distinct property of the aerosol layer over the ASM region, it is nitrate‐rich. We present a newly implemented aerosol formation algorithm that enhances the representation of nitrate aerosol in the Community Aerosol and Radiation Model for Atmospheres (CARMA) coupled with the Community Earth System Model (CESM). The simulated aerosol chemical composition, as well as vertical distributions of aerosol size and mass, are evaluated using in situ and remote sensing observations. The simulated concentrations (ammonium, nitrate, and sulfate) and size distributions are generally within the error bars of data. We find nitrate, organics, and sulfate contribute significantly to the UTLS aerosol concentration between 15°–45°N and 0°–160°E. The two key formation mechanisms of nitrate‐containing aerosols in the ATAL are ammonium neutralization to form ammonium nitrate in regions where convection is active, and condensation of nitric acid in regions of cold temperature. Furthermore, including nitrate formation in the model doubles the surface area density in the tropical tropopause region between 15°–45°N and 0°–160°E, which alters the chlorine partitioning and subsequently impacts the rate of ozone depletion. Plain Language Summary: The Asian Summer Monsoon can efficiently transport pollutants into the upper troposphere and form a layer of aerosols called the Asian Tropopause Aerosol Layer (ATAL). This research investigates the two key formation mechanisms for nitrate aerosol in the ATAL: one is due to cold temperature, and one is due to ammonium neutralization. The simulations are validated against in situ measurements. It also found that O3 chemistry inside ATAL is influenced by nitrate aerosol. Key Points: A new nitrate aerosol formation algorithm is implemented for the community model CARMA to represent the Asian Tropopause Aerosol LayerThe simulated aerosol size distributions and compositions are within error bars of observationsIncluding the new nitrate formation scheme doubles the simulated surface area, changing the chlorine partitioning and ozone depletion [ABSTRACT FROM AUTHOR] |
| Databáze: |
GreenFILE |
| Externí odkaz: |
|
Plný text