首页> 外文期刊>Journal of the Atmospheric Sciences >Response of Marine Boundary Layer Cloud Properties to Aerosol Perturbations Associated with Meteorological Conditions from the 19-Month AMF-Azores Campaign
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Response of Marine Boundary Layer Cloud Properties to Aerosol Perturbations Associated with Meteorological Conditions from the 19-Month AMF-Azores Campaign

机译:来自19个月AMF-Azores运动的海洋边界层云特性对与气象条件相关的气溶胶扰动的响应

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摘要

This study investigates the response of marine boundary layer (MBL) cloud properties to aerosol loading by accounting for the contributions of large-scale dynamic and thermodynamic conditions and quantifies the first indirect effect (FIE). It makes use of 19-month measurements of aerosols, clouds, and meteorology acquired during the Atmospheric Radiation Measurement Mobile Facility field campaign over the Azores. Cloud droplet number concentrations N-c and cloud optical depth (COD) significantly increased with increasing aerosol number concentration N-a. Cloud droplet effective radius (DER) significantly decreased with increasing N-a. The correlations between cloud microphysical properties [N-c, liquid water path (LWP), and DER] and N-a were stronger under more stable conditions. The correlations between N-c, LWP, DER, and Na were stronger under ascending motion conditions, while the correlation between COD and N-a was stronger under descending-motion conditions. The magnitude and corresponding uncertainty of the FIE {=[-partial derivative ln(DER)/partial derivative ln(N-a) at constant LWP} ranged from 0.060 +/- 0.022 to 0.101 +/- 0.006 depending on the different LWP values. Under more stable conditions, cloud-base heights were generally lower than those under less stable conditions. This enabled a more effective interaction with aerosols, resulting in a larger value for the FIE. However, the dependence of the response of cloud properties to aerosol perturbations on stability varied according to whether ground- or satellite-based DER retrievals were used. The magnitude of the FIE had a larger variation with changing LWP under ascending-motion conditions and tended to be higher under ascending-motion conditions for clouds with low LWP and under descending-motion conditions for clouds with high LWP. A contrasting dependence of FIE on atmospheric stability estimated from the surface and satellite cloud properties retrievals reported in this study underscores the importance of assessing all-level properties of clouds in aerosol cloud interaction studies.
机译:这项研究通过考虑大规模动态和热力学条件的贡献,调查了海洋边界层(MBL)云特性对气溶胶负荷的响应,并量化了第一个间接效应(FIE)。它利用在亚速尔群岛进行的“大气辐射测量移动设施”野外活动中获得的19个月的气溶胶,云和气象测量结果。云雾数浓度N-c和云光学深度(COD)随着气溶胶数浓度N-a的增加而显着增加。随着N-a的增加,云滴有效半径(DER)显着降低。在更稳定的条件下,云的微物理性质[N-c,液态水路径(LWP)和DER]与N-a之间的相关性更强。在上升运动条件下,N-c,LWP,DER和Na之间的相关性较强,而在下降运动条件下,COD和N-a之间的相关性较强。 FIE的大小和相应的不确定性{= [在恒定LWP时的偏导数ln(DER)/偏导数ln(N-a)}}的范围为0.060 +/- 0.022至0.101 +/- 0.006,具体取决于不同的LWP值。在更稳定的条件下,云底高度通常低于不稳定条件下的云底高度。这样可以更有效地与气溶胶相互作用,从而为FIE带来更大的价值。但是,根据使用的是基于地面还是基于卫星的DER检索,云特性对气溶胶扰动的响应对稳定性的依赖性会有所不同。在升运动条件下,FIE的大小随LWP的变化而变化较大;对于低LWP的云,FIE的幅度在上升运动条件下较高;对于LWP高的云,FIE的幅度在下降运动条件下倾向于较高。 FIE对大气稳定性的对比依赖关系,该研究由本研究报告的地表和卫星云特性检索估算得出,这突显了在气溶胶云相互作用研究中评估云的所有级别特性的重要性。

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