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Composition and physical properties of the Asian Tropopause Aerosol Layer and the North American Tropospheric Aerosol Layer

机译:亚洲对流层顶气溶胶层和北美对流层气溶胶层的组成和物理性质

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摘要

Recent studies revealed layers of enhanced aerosol scattering in the upper troposphere and lower stratosphere over Asia (Asian Tropopause Aerosol Layer (ATAL)) and North America (North American Tropospheric Aerosol Layer (NATAL)). We use a sectional aerosol model (Community Aerosol and Radiation Model for Atmospheres (CARMA)) coupled with the Community Earth System Model version 1 (CESM1) to explore the composition and optical properties of these aerosol layers. The observed aerosol extinction enhancement is reproduced by CESM1/CARMA. Both model and observations indicate a strong gradient of the sulfur-to-carbon ratio from Europe to the Asia on constant pressure surfaces. We found that the ATAL is mostly composed of sulfates, surface-emitted organics, and secondary organics; the NATAL is mostly composed of sulfates and secondary organics. The model also suggests that emission increases in Asia between 2000 and 2010 led to an increase of aerosol optical depth of the ATAL by 0.002 on average which is consistent with observations.
机译:最近的研究表明,亚洲(亚洲对流层气溶胶层(ATAL)和北美(对流层气溶胶层(NATAL))的对流层和平流层下部的气溶胶散射增强。我们使用剖面气溶胶模型(大气的大气气溶胶和辐射模型(CARMA))与社区地球系统模型版本1(CESM1)结合,来探索这些气溶胶层的组成和光学性质。 CESM1 / CARMA再现了观察到的气溶胶消光增强。模型和观测都表明,在恒压表面上,从欧洲到亚洲的硫碳比有很强的梯度。我们发现,ATAL主要由硫酸盐,表面发射有机物和仲有机物组成。 NATAL主要由硫酸盐和仲有机物组成。该模型还表明,在2000年至2010年期间,亚洲排放量的增加导致ATAL的气溶胶光学深度平均增加了0.002,这与观察结果一致。

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