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Chemical characteristics and source apportionment of aerosols over Indian Ocean during INDOEX-1999
by
Vairamani, M.
, Sekar, R.
, Jain, Monika
, Kulshrestha, U. C.
, Sarkar, A. K.
, Parashar, D. C.
in
Aerosols
/ Combustion
/ Cruises
/ INDIAN OCEAN EXPERIMENT
/ Marine
/ Ocean pollution
/ Oceans
/ Principal components analysis
/ Relative humidity
/ Statistical variance
/ Wind direction
/ Wind velocity
2001
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Chemical characteristics and source apportionment of aerosols over Indian Ocean during INDOEX-1999
by
Vairamani, M.
, Sekar, R.
, Jain, Monika
, Kulshrestha, U. C.
, Sarkar, A. K.
, Parashar, D. C.
in
Aerosols
/ Combustion
/ Cruises
/ INDIAN OCEAN EXPERIMENT
/ Marine
/ Ocean pollution
/ Oceans
/ Principal components analysis
/ Relative humidity
/ Statistical variance
/ Wind direction
/ Wind velocity
2001
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Do you wish to request the book?
Chemical characteristics and source apportionment of aerosols over Indian Ocean during INDOEX-1999
by
Vairamani, M.
, Sekar, R.
, Jain, Monika
, Kulshrestha, U. C.
, Sarkar, A. K.
, Parashar, D. C.
in
Aerosols
/ Combustion
/ Cruises
/ INDIAN OCEAN EXPERIMENT
/ Marine
/ Ocean pollution
/ Oceans
/ Principal components analysis
/ Relative humidity
/ Statistical variance
/ Wind direction
/ Wind velocity
2001
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Chemical characteristics and source apportionment of aerosols over Indian Ocean during INDOEX-1999
Journal Article
Chemical characteristics and source apportionment of aerosols over Indian Ocean during INDOEX-1999
2001
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Overview
During INDOEX IFP-99, the samples of aerosols were collected onboard ORV Sagar Kanya over Indian Ocean along the cruise track, for chemical characterization and identification of dominating sources of aerosols. The concentrations of nss-SO4, nss-Ca, nss-Mg, NO3, K, NH4 and SO2 were observed to be significantly higher before ITCZ in northern hemisphere than across ITCZ in southern hemisphere. In this study, variation of concentrations of nss-SO4, nss-Ca and nss-K with respect to change in latitude, wind direction, wind speed and relative humidity have been highlighted. North of ITCZ, nss-SO4 varied from 2.20 to 18.31 μg/m3 and south of ITCZ from 0.50 to 2.79 μg/m3 while nss-Ca varied from 0.02 to 0.72 μg/m3 north of ITCZ and from 0.01 to 0.14 μg/m3 south of ITCZ. nss-K ranged 0.09–1.43 μg/m3 and 0.07–0.60 μg/m3 before ITCZ and across ITCZ respectively. nss-Ca and nss-SO4 were contributed mainly by NNW and ENE winds while nss-K was observed to be contributed mainly by SSW and ENE winds. Wind speed greater than 4.5 m/s negatively influenced the concentration of nss-Ca concentrations. Correlation coefficients of nss-SO4 with SO2 (r = 0.7) and RH (r = 0.5) suggested a significant contribution of nss-SO4 by aqueous phase oxidation of SO2. Using PCA, four major sources namely sea salt, biogenic combustion, secondary SO4 and crustal contribution were identified over Indian Ocean during INDOEX period.
Publisher
Current Science Association
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