Single ice crystal measurements during nucleation experiments with the depolarization detector IODE

被引:30
作者
Nicolet, M. [1 ]
Stetzer, O. [1 ]
Lueoend, F. [1 ]
Moehler, O. [2 ]
Lohmann, U. [1 ]
机构
[1] ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland
[2] Forschungszentrum Karlsruhe, Inst Meteorol & Climate Sci, Karlsruhe, Germany
基金
瑞士国家科学基金会;
关键词
CHAMBER; PARTICLES; NUCLEI; INSTRUMENT; CLOUDS;
D O I
10.5194/acp-10-313-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In order to determine the efficiency of different aerosol particles to nucleate ice, an Ice Optical DEpolarization detector (IODE) was developed to distinguish between water droplets and ice crystals in ice nucleation chambers. A laser beam polarized linearly (power: 50 mW, wavelength: 407 nm) is directed through the chamber. The scattered light intensity from particles is measured at a scattering angle of I similar to=175 degrees in both polarization components (parallel and perpendicular). The ratio between the perpendicular intensity over the total one yields the depolarization ratio delta. Single particle detection is possible, using a peak detection algorithm. For high particle concentrations, a real-time signal averaging method can also be run simultaneously. The IODE detector was used in connection with the Zurich ice nucleation chamber during the ICIS 2007 workshop where ice nucleation experiments were performed with several aerosol types. In presence of ice crystals, a depolarization ratio could be measured on a particle-by-particle basis. Mean values of delta ranged from 0.24 to 0.37 and agree well with theoretical calculations.
引用
收藏
页码:313 / 325
页数:13
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