MACv2气溶胶气候学

S. Kinne
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引用次数: 48

摘要

MAC气溶胶气候学定义了气溶胶性质的月度全球地图。中可见光和微物理特性的定义与AERONET和MAN地面网络的太阳光度计多年观测数据密切相关。由于可用的统计数据在空间上是稀疏的,因此添加了自下而上的全局建模的上下文。现在的第二版纳入了海洋MAN参考数据,假设了不同的较低人为成分,并改进了数据统计的合并。因此,现在只合并绝对属性,并通过区域校正代替局部域有限校正赋予可信光度计数据更强的权重。全球平均中可见光(550 mn)气溶胶的光学深度(AOD)为0.12,单散射反照率(SSA)为0.94,不对称因子(ASY)为0.7。亚微米(细模式)和超微米(粗模式)气溶胶粒径的平均值分别为0.063 (AODf)和0.058 (AODc), 0.92 (SSAf)和0.965 (SSAc), 0.64 (ASYf)和0.77 (ASYc)。一个新的元素是天空/太阳光度计对气溶胶吸收(AAOD)的细模和粗模贡献的分离。这些特性以及精细模式有效半径与来自全球模型的背景数据合并,得到全球平均值分别为0.0051 (AAODf)、0.0021 (AAODc)和0.18 μm (RE,f)。本地月模式细节现在允许(以“自上而下”的方法)提取气溶胶成分数量和大小的全球分布。由于煤烟(BC)、有机物(OC)、非吸收精细模式(SU)、海盐(SS)和矿物粉尘(DU)等成分具有预定义的光谱分辨特性,因此,根据宽带辐射传输应用的要求,除中可见波长外的光学特性将自动定义。利用组分信息(如数量、组成和大小),也可以对CCN和IN浓度进行MAC估计,并提出了一个基于MAC的简单气溶胶反演模型。
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The MACv2 aerosol climatology
Abstract The MAC aerosol climatology defines monthly global maps for aerosol properties. The definition of mid-visible optical and microphysical properties is strongly linked to multi-year statistics of observations by sun-photometers of the AERONET and MAN ground networks. As available statistics are spatially sparse, context from bottom-up global modelling is added. Now in its second version, oceanic MAN reference data are included, a different lower anthropogenic fraction is assumed and the merging of the data-statistics is improved. Hereby, now only absolute properties are merged and trusted photometer data are given stronger weights via regional corrections in place of local domain limited corrections. Global average mid-visible (550 mn) aerosol properties are 0.12 for the aerosol optical depth (AOD), 0.94 for the single scattering albedo (SSA) and 0.7 for the asymmetry-factor (ASY). Averages for sub-micrometer (fine-mode) and super-micrometer (coarse-mode) aerosol sizes are 0.063 (AODf) and 0.058 (AODc), 0.92 (SSAf) and 0.965 (SSAc) and 0.64 (ASYf) and 0.77 (ASYc), respectively. A new element is the separation of aerosol absorption (AAOD) by sky-/sun-photometers into fine-mode and coarse-mode contributions. These properties as well as the fine-mode effective radii were merged with background data from global modelling yielding global averages of 0.0051 (AAODf), 0.0021 (AAODc) and 0.18 μm (RE,f). Local monthly mode detail now allows (in a ‘top-down’ approach) to extract global distributions for aerosol component amounts and sizes. As the considered components for soot (BC), organics (OC), non-absorbing fine-mode (SU), sea-salt (SS) and mineral dust (DU) have pre-defined spectrally resolved properties, optical properties at other than mid-visible wavelengths are automatically defined – as required in broadband radiative transfer applications. With component information (e.g. amount, composition and size) also MAC estimates for CCN and IN concentrations are possible and also a simple MAC based aerosol retrieval model for satellite sensor data is suggested.
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