Beijing Climate Center Earth System Model version 1 (BCC-ESM1): model description and evaluation of aerosol simulations
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Published:2020-03-06
Issue:3
Volume:13
Page:977-1005
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ISSN:1991-9603
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Container-title:Geoscientific Model Development
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language:en
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Short-container-title:Geosci. Model Dev.
Author:
Wu TongwenORCID, Zhang Fang, Zhang Jie, Jie Weihua, Zhang Yanwu, Wu FanghuaORCID, Li LaurentORCID, Yan Jinghui, Liu Xiaohong, Lu XiaoORCID, Tan Haiyue, Zhang Lin, Wang JunORCID, Hu AixueORCID
Abstract
Abstract. The Beijing Climate Center Earth System Model version 1 (BCC-ESM1) is the first version of a fully coupled Earth system model with interactive atmospheric chemistry and aerosols developed by the
Beijing Climate Center, China Meteorological Administration. Major aerosol
species (including sulfate, organic carbon, black carbon, dust, and sea salt)
and greenhouse gases are interactively simulated with a whole panoply of
processes controlling emission, transport, gas-phase chemical reactions,
secondary aerosol formation, gravitational settling, dry deposition, and wet
scavenging by clouds and precipitation. Effects of aerosols on radiation,
cloud, and precipitation are fully treated. The performance of BCC-ESM1 in
simulating aerosols and their optical properties is comprehensively
evaluated as required by the Aerosol Chemistry Model Intercomparison Project
(AerChemMIP), covering the preindustrial mean state and time evolution from
1850 to 2014. The simulated aerosols from BCC-ESM1 are quite coherent with
Coupled Model Intercomparison Project Phase 5 (CMIP5)-recommended data, in situ measurements from surface networks (such as
IMPROVE in the US and EMEP in Europe), and aircraft observations. A
comparison of modeled aerosol optical depth (AOD) at 550 nm with satellite
observations retrieved from the Moderate Resolution Imaging Spectroradiometer
(MODIS) and the Multi-angle Imaging SpectroRadiometer (MISR) and surface AOD
observations from the AErosol RObotic NETwork (AERONET) shows reasonable
agreement between simulated and observed AOD. However, BCC-ESM1 shows
weaker upward transport of aerosols from the surface to the middle and upper
troposphere, likely reflecting the deficiency of representing deep
convective transport of chemical species in BCC-ESM1. With an overall good
agreement between BCC-ESM1 simulated and observed aerosol properties, it
demonstrates a success of the implementation of interactive aerosol and
atmospheric chemistry in BCC-ESM1.
Publisher
Copernicus GmbH
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