亚洲上空气溶胶的吸收——使用CAM5.3-Oslo的模式间和模式观测比较研究

L. Frey, F. Höpner, A. Kirkevåg, F. Bender
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引用次数: 1

摘要

气溶胶吸收是气溶胶总辐射效应的一个重要组成部分,因此其在大气环流模式中的表示对于估算辐射强迫至关重要。我们在这里使用多个观测值来评估CAM5.3-Oslo在气溶胶表征方面的性能。CAM5.3-Oslo是地球系统模式NorESM1.2的大气分量,与观测值和其他AeroCom III阶段模式相比,CAM5.3-Oslo平均低估了东亚和南亚的焦点区域的气溶胶吸收,而对沙漠和干旱地区的气溶胶吸收估计过高。探讨了模型扩散的原因,发现其与吸收气溶胶,特别是黑碳和粉尘的柱负荷和停留时间有关。我们使用CAM5.3-Oslo进行进一步的灵敏度模拟,以确定对模拟气溶胶吸收最重要的过程。灵敏度实验的目标是气溶胶光学特性,并将其影响与排放和沉积过程变化以及驱动气象的影响进行对比。通过使用一套精确的发射数据集、瞬态发射和气象观测的同化,发现与观测结果更加吻合。吸收气溶胶的光学性质的变化也可以减少模式中气溶胶吸收的过低估计和过高估计。然而,与AeroCom第三阶段模型间的模式间分布相比,敏感性实验间气溶胶吸收强度的变化较小。
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Absorbing aerosols over Asia – an inter-model and model-observation comparison study using CAM5.3-Oslo
Abstract Aerosol absorption constitutes a significant component of the total radiative effect of aerosols, and hence its representation in general circulation models is crucial to radiative forcing estimates. We use here multiple observations to evaluate the performance of CAM5.3-Oslo with respect to its aerosol representation. CAM5.3-Oslo is the atmospheric component of the earth system model NorESM1.2 and shows on average an underestimation of aerosol absorption in the focus region over East and South Asia and a strong aerosol absorption overestimation in desert and arid regions compared to observations and other AeroCom phase III models. We explore the reasons of the model spread and find that it is related to the column burden and residence time of absorbing aerosols, in particular black carbon and dust. We conduct further sensitivity simulations with CAM5.3-Oslo to identify processes which are most important for modelled aerosol absorption. The sensitivity experiments target aerosol optical properties, and contrast their impact with effects from changes in emissions and deposition processes, and the driving meteorology. An improved agreement with observations was found with the use of a refined emission data set, transient emissions and assimilation of meteorological observations. Changes in optical properties of absorbing aerosols can also reduce the under- and overestimation of aerosol absorption in the model. However, changes in aerosol absorption strength between the sensitivity experiments are small compared to the inter-model spread among the AeroCom phase III models.
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