东北太平洋上空气溶胶粒子的光学特性。

J. Marshall, U. Lohmann, W. Leaitch, N. Shantz, L. Phinney, D. Toom‐Sauntry, Sangeeta Sharma
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引用次数: 9

摘要

2002年7月,作为亚北极生态系统对铁增强响应研究(SERIES)的一部分,在东北太平洋进行了大气气溶胶测量。测量了气溶胶的粒径分布、三个波长下的颗粒散射系数和后向散射系数、一个波长下的颗粒吸收系数和粒径分离的颗粒化学成分。利用Mie理论计算气溶胶粒子的散射和吸收系数,根据粒径分布和化学测量,不能得到与测量光学系数的封闭。散射系数和后向散射系数的计算值与实测值之间的差异主要是由于浊度计只测量7°到170°之间的散射。由于缺少前向散射(0°-7°)和后向散射,本研究中超过90%的总散射和50%的后向散射没有被浊度计测量到。
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Optical Properties of Aerosol Particles over the Northeast Pacific.
Abstract In July 2002, atmospheric aerosol measurements were conducted over the northeast Pacific Ocean as part of the Subarctic Ecosystem Response to Iron Enhancement Study (SERIES). The following aerosol quantities were measured: particle number size distribution, particle scattering and backscattering coefficients at three wavelengths, particle absorption coefficient at one wavelength, and size-segregated particle chemical composition. Using Mie theory to calculate the aerosol particle scattering and absorption coefficients from the size distribution and chemical measurements, closure with the measured optical coefficients is not attained. Discrepancies between the calculated and measured scattering and backscattering coefficients are largely a result of the fact that the nephelometer measures scattering only between 7° and 170°. Over 90% of the total scattering and 50% of the backscattering in this study was not measured by the nephelometer because of the missing forward-scattering (0°–7°) and backsca...
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