Improving BC Mixing State and CCN Activity Representation With Machine Learning in the Community Atmosphere Model Version 6 (CAM6)

Author:

Shen Wenxiang12ORCID,Wang Minghuai12ORCID,Riemer Nicole3ORCID,Zheng Zhonghua4ORCID,Liu Yawen12ORCID,Dong Xinyi125ORCID

Affiliation:

1. School of Atmospheric Sciences Nanjing University Nanjing China

2. Joint International Research Laboratory of Atmospheric and Earth System Sciences and Institute for Climate and Global Change Research Nanjing University Nanjing China

3. Department of Atmospheric Sciences University of Illinois Urbana‐Champaign Urbana IL USA

4. Department of Earth and Environmental Sciences The University of Manchester Manchester UK

5. Frontiers Science Center for Critical Earth Material Cycling Nanjing University Nanjing China

Abstract

AbstractRepresenting mixing state of black carbon (BC) is challenging for global climate models (GCMs). The Community Atmosphere Model version 6 (CAM6) with the four‐mode version of the Modal Aerosol Module (MAM4) represents aerosols as fully internal mixtures with uniform composition within each aerosol mode, resulting in high degree of internal mixing of BC with non‐BC species and large mass ratio of coating to BC (RBC, the mass ratio of non‐BC species to BC in BC‐containing particles). To improve BC mixing state representation, we coupled a machine learning (ML) model of BC mixing state index trained on particle‐resolved simulations to the CAM6 with MAM4 (MAM4‐ML). In MAM4‐ML, we use RBC to partition accumulation mode particles into two new modes, BC‐free particles and BC‐containing particles. We adjust RBC to make the modeled BC mixing state index (χmode) match the one predicted by the ML model (χML). On a global average, the mass fraction of BC‐containing particles in accumulation mode decreases from 100% (MAM4‐default) to 48% (MAM4‐ML). The globally averaged χmode decreases from 78% (MAM4‐default) to 63% (MAM4‐ML, 19% reduction) and agrees well with χML (66%). The RBC decreases by 52% for accumulation mode and better agrees with observations. The hygroscopicity drops by 9% for BC‐containing particles in accumulation mode, leading to a 20% reduction in the BC activation fraction. The surface BC concentration increases most (6.9%) in the Arctic, and the BC burden increases by 4%, globally. Our study highlights the application of the ML model for improving key aerosol processes in GCMs.

Funder

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

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