4.7 Article

Global distribution of Asian, Middle Eastern, and North Atrican dust simulated by CESM1/CAKMA

期刊

ATMOSPHERIC CHEMISTRY AND PHYSICS
卷 22, 期 20, 页码 13659-13676

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-22-13659-2022

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资金

  1. second Tibetan Plateau Scientific Expedition and Research Program [2019QZKK0604]
  2. Guangdong Innovative and Entrepreneurial Research Team Program [2019ZT08G669]
  3. National Natural Science Foundation of China [42175089, 42121004]
  4. NSF award [1853932]
  5. NOAA
  6. NASA award [NNH15AB12I]
  7. Div Atmospheric & Geospace Sciences
  8. Directorate For Geosciences [1853932] Funding Source: National Science Foundation

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Dust aerosols have a significant impact on the radiative and energy balance at local and global scales. This study improves the simulated size distribution of dust aerosol and finds that North African, Middle Eastern, and Asian dust contribute the most to global dust emissions, with Asian dust dominating the dust mass budget in the upper troposphere and lower stratosphere.
Dust aerosols affect the radiative and energy balance at local and global scales by scattering and absorbing sunlight and infrared light. A previous study suggests that dust size distribution is one of the major sources of uncertainty in modeling the dust global distribution. Climate models overestimate the fine dust (<= 5 mu m) by an order of magnitude, while underestimates of the coarse dust (>= 5 mu m) range between 0.5 to 1.5 orders of magnitude compared with the global observations. Here we improved the simulated size distribution of dust aerosol using a sectional aerosol model (Community Aerosol and Radiation Model for Atmospheres) coupled with the Community Earth System Model (CESM1/CARMA). Simulated dust mass size distributions peak at around 2-3 mu m in diameter and increase by 4 orders of magnitude from 0.1 to 2 mu m. Our model demonstrates that North African, Middle Eastern, and Asian dust accounts for similar to 59.7 %, 12.5 %, and 13.3 % of the global annual mean dust emissions, with the remaining 14.5 % originating from scattered smaller dust sources. The model dust vertical distributions are validated against the NASA Atmospheric Tomography (ATom) field campaign datasets. Both simulations and ATom in situ measurements during the ATom field campaign suggest that dust mass concentrations over the remote ocean drop by 2 to 3 orders of magnitude from the surface to the upper troposphere (200 hPa). Our model suggests that Asian dust contributes to more than 40 % of annual mean dust mass abundances in the global upper troposphere and lower stratosphere (UTLS). The model suggests that Asian dust dominates the dust mass budget in the UTLS of the Asian summer monsoon (ASM) region, with a relative contribution 1-2 orders of magnitude higher than the dust originating from the North African and Middle Eastern deserts.

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