An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India

Columnaraerosol size distributions, retrieved from spectral AOD (aerosol optical depth) esti mates over a northeastern location of India (Dibrugarh) are, ingeneral, bimodal with the occurrence of primary (broad) mode at 0.04 - 0.17 m and the secondary mode at 0.88 - 1.29 m. The physical parameters o...

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Main Authors: Mukunda Madhab Gogoi, Pradip Kumar Bhuyan, Krishnaswamy Krishna Moorthy
Format: Article
Language:English
Published: Chinese Geoscience Union 2009-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v203p511.pdf
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spelling doaj-6acdd9170ba540109d57f0b71bede1f22020-11-25T03:36:25ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802009-01-0120351110.3319/TAO.2008.06.11.01(A)854An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern IndiaMukunda Madhab GogoiPradip Kumar BhuyanKrishnaswamy Krishna MoorthyColumnaraerosol size distributions, retrieved from spectral AOD (aerosol optical depth) esti mates over a northeastern location of India (Dibrugarh) are, ingeneral, bimodal with the occurrence of primary (broad) mode at 0.04 - 0.17 m and the secondary mode at 0.88 - 1.29 m. The physical parameters of size distributions representing the microphysical properties of aerosols show distinct sea sonal variations with the highest value of the effec tiveradii (~ 0.55 m) during pre-mon soon (March to May) season which, along with the highest value of AOD (~ 0.46 ¡__n0.09) during the same season, is attributed to the maxi mum abundance of coarsepa ticles. Examining the re sults in the light of the HYSPLIT back tra jectory analy sis and the peruliar to pogr phy of northeast India allowing advection only from the Indo-Gangetic plains or Bay-of-Ben gal, it appears that the strong presence of the coarse mode aerosols are associated with either mineral dust or marine aerosol components or both. http://tao.cgu.org.tw/images/attachments/v203p511.pdf Aero soloptical depthColumnar size distributionMultiwavelength solar radiometerHYSPLIT
collection DOAJ
language English
format Article
sources DOAJ
author Mukunda Madhab Gogoi
Pradip Kumar Bhuyan
Krishnaswamy Krishna Moorthy
spellingShingle Mukunda Madhab Gogoi
Pradip Kumar Bhuyan
Krishnaswamy Krishna Moorthy
An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
Terrestrial, Atmospheric and Oceanic Sciences
Aero soloptical depth
Columnar size distribution
Multiwavelength solar radiometer
HYSPLIT
author_facet Mukunda Madhab Gogoi
Pradip Kumar Bhuyan
Krishnaswamy Krishna Moorthy
author_sort Mukunda Madhab Gogoi
title An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
title_short An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
title_full An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
title_fullStr An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
title_full_unstemmed An Investigation of Aerosol Size Distribution Properties at Dibrugarh: North-Eastern India
title_sort investigation of aerosol size distribution properties at dibrugarh: north-eastern india
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2009-01-01
description Columnaraerosol size distributions, retrieved from spectral AOD (aerosol optical depth) esti mates over a northeastern location of India (Dibrugarh) are, ingeneral, bimodal with the occurrence of primary (broad) mode at 0.04 - 0.17 m and the secondary mode at 0.88 - 1.29 m. The physical parameters of size distributions representing the microphysical properties of aerosols show distinct sea sonal variations with the highest value of the effec tiveradii (~ 0.55 m) during pre-mon soon (March to May) season which, along with the highest value of AOD (~ 0.46 ¡__n0.09) during the same season, is attributed to the maxi mum abundance of coarsepa ticles. Examining the re sults in the light of the HYSPLIT back tra jectory analy sis and the peruliar to pogr phy of northeast India allowing advection only from the Indo-Gangetic plains or Bay-of-Ben gal, it appears that the strong presence of the coarse mode aerosols are associated with either mineral dust or marine aerosol components or both.
topic Aero soloptical depth
Columnar size distribution
Multiwavelength solar radiometer
HYSPLIT
url http://tao.cgu.org.tw/images/attachments/v203p511.pdf
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