Arid
DOI10.1063/1.4946144
Atmospheric Aerosols Size Distribution Properties In Winter And Pre-Monsoon Over Western Indian Thar Desert Location
Panwar, Chhagan; Vyas, B. M.
通讯作者Panwar, Chhagan
会议名称International Conference on Condensed Matter and Applied Physics (ICC)
会议日期OCT 30-31, 2015
会议地点Bikaner, INDIA
英文摘要

The first ever experimental results over Indian Thar Desert region concerning to height integrated aerosols size distribution function in particles size ranging between 0.09 to 2 mu m such as, aerosols columnar size distribution (CSD), effective radius (R-eff), integrated content of total aerosols (N-t), columnar content of accumulation and coarse size aerosols particles concentration (N-a) (size < 0.5 mu m) and (N-c) (size between 0.5 to 2 mu m) have been described specifically during winter (a stable weather condition and intense anthropogenic pollution activity period) and pre monsoon (intense dust storms of natural mineral aerosols as well as unstable atmospheric weather condition period) at Jaisalmer (26.90 degrees N, 69.90 degrees E, 220 m above surface level (asl)) located in central Thar desert vicinity of western Indian site. The CSD and various derived other aerosols size parameters are retrieved from their average spectral characteristics of Aerosol Optical Thickness (AOT) from-UV to Infrared wavelength spectrum measured from Multi-Wavelength solar Radiometer (MWR).The natures of CSD are, in general, bio-modal character, instead of uniformly distributed character and power law distributions. The observed primary peaks m CSD plots are seen around about 10(13) m(2) mu m(-1) at radius range 0.09-0.20 mu m during both the seasons. But, in winter months, secondary peaks of relatively lower CSD values of 10(10) to 10(11) m(2)/mu m(-1) occur within a lower radius size range 0.4 to 0.6 mu m. In contrast to this, while in dust dominated and hot season, the dominated secondary maxima of the higher CSD of about 10(12) m(2)mu m(-3) is found of bigger aerosols size particles in a rage of 0.6 to 1.0 mu m which is clearly demonstrating the characteristics of higher aerosols laden of bigger size aerosols m summer months relative to their prevailed lower aerosols loading of smaller size aerosols particles (0.4 to 0.6 mu m) in cold months. Several other interesting features of changing nature of monthly spectral AOT, R-eff, N-t, N-a and N-C (particles/m(2)) have been discussed in detail in this paper.


英文关键词Atmospheric aerosols size distribution Thar Desert MWR
来源出版物INTERNATIONAL CONFERENCE ON CONDENSED MATTER AND APPLIED PHYSICS (ICC 2015)
ISSN0094-243X
出版年2016
卷号1728
EISBN978-0-7354-1375-7
出版者AMER INST PHYSICS
类型Proceedings Paper
语种英语
国家India
收录类别CPCI-S
WOS记录号WOS:000375945500093
WOS关键词CLIMATE
WOS类目Physics, Applied ; Physics, Condensed Matter
WOS研究方向Physics
资源类型会议论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/305627
作者单位ML Sukhadia Univ, Dept Phys, Udaipur 313001, India
推荐引用方式
GB/T 7714
Panwar, Chhagan,Vyas, B. M.. Atmospheric Aerosols Size Distribution Properties In Winter And Pre-Monsoon Over Western Indian Thar Desert Location[C]:AMER INST PHYSICS,2016.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Panwar, Chhagan]的文章
[Vyas, B. M.]的文章
百度学术
百度学术中相似的文章
[Panwar, Chhagan]的文章
[Vyas, B. M.]的文章
必应学术
必应学术中相似的文章
[Panwar, Chhagan]的文章
[Vyas, B. M.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。