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利用多波长激光雷达推导皮纳图博火山平流层气溶胶平均粒径分布

Derivation of Mount Pinatubo stratospheric aerosol mean size distribution by means of a multiwavelength lidar.

作者信息

Guasta M D, Morandi M, Stefanutti L, Stein B, Wolf J P

出版信息

Appl Opt. 1994 Aug 20;33(24):5690-7. doi: 10.1364/AO.33.005690.

Abstract

A multiwavelength lidar operated in Sodankyla, Finland, during the European Arctic Stratospheric Ozone Experiment (December 1991-March 1992). It produced vertical profiles of stratospheric aerosols at four wavelengths. The determination of aerosol mean size distribution has been performed by use of extinction/backscattering ratios as obtained from lidar data processing at 355, 352, and 750 nm. Lognormal distributions of sulfuric particles with mode radius of r(m) = 0.12-0.25 µm and corresponding widths of s = 2-1.6 have been retrieved as best fits of experimental data, in good agreement with in situ measurements. A successful attempt to derive bimodal log-normal distributions is also described, together with the experimental and theoretical problems involved.

摘要

一台多波长激光雷达于1991年12月至1992年3月在芬兰的索丹屈莱运行,用于欧洲北极平流层臭氧实验。它在四个波长下生成了平流层气溶胶的垂直剖面。利用在355、352和750纳米处激光雷达数据处理得到的消光/后向散射比,确定了气溶胶平均粒径分布。已检索到模式半径r(m) = 0.12 - 0.25微米、相应宽度s = 2 - 1.6的硫酸颗粒对数正态分布,作为实验数据的最佳拟合,与现场测量结果吻合良好。还描述了一次成功推导双峰对数正态分布的尝试,以及所涉及的实验和理论问题。

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