Arid
DOI10.1016/j.jqsrt.2014.10.009
Ceilometer calibration for retrieval of aerosol optical properties
Jin, Yoshitaka1; Kai, Kenji2; Kawai, Kei2; Nagai, Tomohiro3; Sakai, Tetsu3; Yamazaki, Akihiro3; Uchiyama, Akihiro3; Batdorj, Dashdondog4; Sugimoto, Nobuo1; Nishizawa, Tomoaki1
通讯作者Jin, Yoshitaka
来源期刊JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER
ISSN0022-4073
EISSN1879-1352
出版年2015
卷号153页码:49-56
英文摘要

Ceilometers are durable compact backscatter lidars widely used to detect cloud base height. They are also useful for measuring aerosols. We introduced a ceilometer (CL51) for observing dust in a source region in Mongolia. For retrieving aerosol profiles with a backscatter lidar, the molecular backscatter signal in the aerosol free heights or system constant of the lidar is required. Although the system constant of the ceilometer is calibrated by the manufacturer, it is not necessarily accurate,enough for the aerosol retrieval. We determined a correction factor, which is defined as the ratio of true attenuated backscattering coefficient to the measured attenuated backscattering coefficient, for the CL51 ceilometer using a dual-wavelength Mie-scattering lidar in Tsukuba, Japan before moving the ceilometer to Dalanzadgad, Mongolia. The correction factor determined by minimizing the difference between the ceilometer and lidar backscattering coefficients was approximately 1.2 +/- 0.1. Applying the correction to the CL51 signals, the aerosol optical depth (AOD) agreed well with the sky-radiometer AOD during the observation period (13-17 February 2013) in Tsukuba (9 x 10(-3) of mean square error). After moving the ceilometer to Dalanzadgad, however, the AOD observed with the CL51 (calibrated by the correction factor determined in Tsukuba) was approximately 60% of the AErosol RObotic NETwork (AERONET) sun photometer AOD. The possible causes of the lower AOD results are as follows: (1) the limited height range of extinction integration ( < 3 km); (2) change in the correction factor during the ceilometer transportation or with the window contamination in Mongolia. In both cases, on-site calibrations by dual-wavelength lidar are needed. As an alternative method, we showed that the backward inversion method was useful for retrieving extinction coefficients if the AOD was larger than 1.5. This retrieval method does not require the system constant and molecular backscatter signals, and can be applied to severe dust and air pollution aerosol cases in East Asia. (C) 2014 Elsevier Ltd. All rights reserved.


英文关键词Ceilometer Lidar Aerosol Desert dust
类型Article
语种英语
国家Japan ; Mongolia
收录类别SCI-E
WOS记录号WOS:000349883200006
WOS关键词ASIAN DUST ; TAKLIMAKAN DESERT ; LIDAR ; JAPAN ; CHINA ; VALIDATION ; TRANSPORT ; CALIPSO
WOS类目Optics ; Spectroscopy
WOS研究方向Optics ; Spectroscopy
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/188921
作者单位1.Natl Inst Environm Studies, Ctr Environm Measurement & Anal, Tsukuba, Ibaraki 3058506, Japan;
2.Nagoya Univ, Grad Sch Environm Studies, Nagoya, Aichi 4648601, Japan;
3.Japan Meteorol Agcy, Meteorol Res Inst, Ibaraki, Japan;
4.Natl Agcy Meteorol & Environm Monitoring, Div Technol Informat & Mkt, Ulaanbaatar, Mongolia
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GB/T 7714
Jin, Yoshitaka,Kai, Kenji,Kawai, Kei,et al. Ceilometer calibration for retrieval of aerosol optical properties[J],2015,153:49-56.
APA Jin, Yoshitaka.,Kai, Kenji.,Kawai, Kei.,Nagai, Tomohiro.,Sakai, Tetsu.,...&Nishizawa, Tomoaki.(2015).Ceilometer calibration for retrieval of aerosol optical properties.JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER,153,49-56.
MLA Jin, Yoshitaka,et al."Ceilometer calibration for retrieval of aerosol optical properties".JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER 153(2015):49-56.
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