Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China

The Yinchuan area, which lies in the eastern part of Northwest China, is one of the main transportation paths and origins of sand dust in China. In order to investigate the aerosol number size distribution and its temporal-spatial evolution over this area, direct solar radiation data taken from Sept...

Full description

Saved in:
Bibliographic Details
Main Authors: Jiandong Mao, Hongjiang Sheng, Hu Zhao, Chunyan Zhou
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2014/157645
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832555959027761152
author Jiandong Mao
Hongjiang Sheng
Hu Zhao
Chunyan Zhou
author_facet Jiandong Mao
Hongjiang Sheng
Hu Zhao
Chunyan Zhou
author_sort Jiandong Mao
collection DOAJ
description The Yinchuan area, which lies in the eastern part of Northwest China, is one of the main transportation paths and origins of sand dust in China. In order to investigate the aerosol number size distribution and its temporal-spatial evolution over this area, direct solar radiation data taken from September 2012 to October 2013 by a sun photometer CE-318 located at Beifang University of Nationalities (106°29′E, 38°13′N) were analyzed. The particle number size distributions were retrieved from the aerosol optical depth (AOD) by use of the extinction inversion method. The experiment results show that although the averaged size distribution satisfies basically the Junge function, there are two obvious peaks at the particle radius of 0.6 μm and 1.4 μm, respectively. Because sand-dust weather occurs frequently, the particle size distribution in Spring is obviously larger than that in other seasons, which coincides with AOD variation tendency. Moreover, in sand-dust weather the particles number concentration is larger than that of background weather with one order of magnitude, especially for the number of concentration of large particles and giant particles. The research results have very important reference value for quantitative study of the influence of aerosol on atmosphere physics and chemistry process and monitoring of sand-dust weather and air pollution of this area.
format Article
id doaj-art-d3b30793ff26413692feaac8bd54ce8c
institution Kabale University
issn 1687-9309
1687-9317
language English
publishDate 2014-01-01
publisher Wiley
record_format Article
series Advances in Meteorology
spelling doaj-art-d3b30793ff26413692feaac8bd54ce8c2025-02-03T05:46:43ZengWileyAdvances in Meteorology1687-93091687-93172014-01-01201410.1155/2014/157645157645Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, ChinaJiandong Mao0Hongjiang Sheng1Hu Zhao2Chunyan Zhou3School of Electrical and Information Engineering, Beifang University of Nationalities, Yinchuan 750021, ChinaSchool of Electrical and Information Engineering, Beifang University of Nationalities, Yinchuan 750021, ChinaSchool of Electrical and Information Engineering, Beifang University of Nationalities, Yinchuan 750021, ChinaSchool of Electrical and Information Engineering, Beifang University of Nationalities, Yinchuan 750021, ChinaThe Yinchuan area, which lies in the eastern part of Northwest China, is one of the main transportation paths and origins of sand dust in China. In order to investigate the aerosol number size distribution and its temporal-spatial evolution over this area, direct solar radiation data taken from September 2012 to October 2013 by a sun photometer CE-318 located at Beifang University of Nationalities (106°29′E, 38°13′N) were analyzed. The particle number size distributions were retrieved from the aerosol optical depth (AOD) by use of the extinction inversion method. The experiment results show that although the averaged size distribution satisfies basically the Junge function, there are two obvious peaks at the particle radius of 0.6 μm and 1.4 μm, respectively. Because sand-dust weather occurs frequently, the particle size distribution in Spring is obviously larger than that in other seasons, which coincides with AOD variation tendency. Moreover, in sand-dust weather the particles number concentration is larger than that of background weather with one order of magnitude, especially for the number of concentration of large particles and giant particles. The research results have very important reference value for quantitative study of the influence of aerosol on atmosphere physics and chemistry process and monitoring of sand-dust weather and air pollution of this area.http://dx.doi.org/10.1155/2014/157645
spellingShingle Jiandong Mao
Hongjiang Sheng
Hu Zhao
Chunyan Zhou
Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
Advances in Meteorology
title Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
title_full Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
title_fullStr Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
title_full_unstemmed Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
title_short Observation Study on the Size Distribution of Sand Dust Aerosol Particles over Yinchuan, China
title_sort observation study on the size distribution of sand dust aerosol particles over yinchuan china
url http://dx.doi.org/10.1155/2014/157645
work_keys_str_mv AT jiandongmao observationstudyonthesizedistributionofsanddustaerosolparticlesoveryinchuanchina
AT hongjiangsheng observationstudyonthesizedistributionofsanddustaerosolparticlesoveryinchuanchina
AT huzhao observationstudyonthesizedistributionofsanddustaerosolparticlesoveryinchuanchina
AT chunyanzhou observationstudyonthesizedistributionofsanddustaerosolparticlesoveryinchuanchina