Journal of Advances in Modeling Earth Systems (Oct 2023)

An Aerosol Optical Module With Observation‐Constrained Black Carbon Properties for Global Climate Models

  • Ganzhen Chen,
  • Jiandong Wang,
  • Yuan Wang,
  • Jiaping Wang,
  • Yuzhi Jin,
  • Yueyue Cheng,
  • Yan Yin,
  • Hong Liao,
  • Aijun Ding,
  • Shuxiao Wang,
  • Jiming Hao,
  • Chao Liu

DOI
https://doi.org/10.1029/2022MS003501
Journal volume & issue
Vol. 15, no. 10
pp. n/a – n/a

Abstract

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Abstract Atmospheric black carbon (BC) aerosols have been long‐lasting uncertain components in environmental and climate studies. Global climate models (GCMs) potentially overestimate BC absorption efficiency due to a lack of consideration of complex BC microphysical and mixing properties. We extract multiple BC properties from observations and develop an aerosol optical module known as Advanced Black Carbon (ABC) in the framework of the Modal Aerosol Model version 4 (MAM4). The ABC module is implemented in the Community Atmosphere Model version 6 (CAM6) and evaluated by in situ and remote sensing observations. CAM6‐ABC addresses the shortcomings of CAM6‐MAM4 in terms of BC microphysical and mixing properties, particularly their size, mixing state and optical simulations. Sensitivity simulations show that the global BC absorption aerosol optical depth at 550 nm simulated by CAM6‐ABC is reduced by ∼29% compared with that in CAM6‐MAM4. The BC absorption enhancement simulated by CAM6‐ABC is reduced from ∼2.6 of the default MAM4 to ∼1.4, which is closer to the observed values (mostly less than 1.5). With improved BC absorption estimation, the biases of aerosol single‐scattering coalbedo simulations are reduced by 18%–69% compared with global Aerosol Robotic Network observations. Moreover, the globally averaged BC direct radiative effect is reduced from 0.37 to 0.28 W/m2 at the top of the atmosphere. Our new scheme alleviates the overestimation of BC absorption in GCMs by constraining BC microphysical and mixing properties when assessing aerosol radiative and climate effects, and it can be easily implemented in most modal‐based aerosol modules of climate models.

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