Large contrast in the vertical distribution of aerosol optical properties and radiative effects across the Indo-Gangetic Plain during the SWAAMI–RAWEX campaign
Measurements of the vertical profiles of the optical properties (namely the extinction coefficient and scattering and absorption coefficients respectively σext ∕ σscat ∕ σabs) of aerosols have been made across the Indo-Gangetic Plain (IGP) using an instrumented aircraft operated from three base stat...
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Veröffentlicht in: | Atmospheric chemistry and physics 2018-12, Vol.18 (23), p.17669-17685 |
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Zusammenfassung: | Measurements of the vertical profiles of the optical properties (namely the extinction
coefficient and scattering and absorption coefficients respectively
σext ∕ σscat ∕ σabs)
of aerosols have been made across the Indo-Gangetic Plain (IGP) using an
instrumented aircraft operated from three base stations – Jodhpur (JDR),
representing the semi-arid western IGP; Varanasi (VNS), the central IGP
characterized by significant anthropogenic activities; and the industrialized
coastal location in the eastern end of the IGP (Bhubaneswar, BBR) – just
prior to the onset of the Indian summer monsoon. The vertical profiles
depicted region-specific absorption characteristics, while the scattering
characteristics remained fairly uniform across the region, leading to a
west–east gradient in the vertical structure of single-scattering
albedo (SSA). Integrated from near the ground to 3 km, the highest
absorption coefficient and hence the lowest SSA occurred in the central IGP
(Varanasi). Size distribution, inferred from the spectral variation of the
scattering coefficient, showed a gradual shift from coarse-particle dominance
in the western IGP to strong accumulation dominance in the eastern coast with
the central IGP coming in between, arising from a change in the aerosol type
from a predominantly natural (dust and sea salt) type in the western IGP to a
highly anthropogenic type (industrial emissions, fossil fuel and biomass
combustion) in the eastern IGP, with the central IGP exhibiting a mixture of
both. Aerosol-induced short-wave radiative forcing, estimated using
altitude-resolved SSA information, revealed significant atmospheric warming
in the central IGP, while a top-of-atmosphere cooling is seen, in general, in
the IGP. Atmospheric heating rate profiles, estimated using altitude-resolved
SSA and column-averaged SSA, revealed considerable underestimation in the
latter case, emphasizing the importance and necessity of having
altitude-resolved SSA information as against a single value for the entire
column. |
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ISSN: | 1680-7324 1680-7316 1680-7324 |
DOI: | 10.5194/acp-18-17669-2018 |