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Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
Author(s) -
Bhupender Singh,
A. K. Srivastava,
S. Tiwari,
Sachchidanand Singh,
Rajeev Kumar Singh,
D. S. Bisht,
D. M. Lal,
Abhay Kumar Singh,
R. K. Mall,
Manoj Srivastava
Publication year - 2014
Publication title -
advances in meteorology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.482
H-Index - 32
eISSN - 1687-9317
pISSN - 1687-9309
DOI - 10.1155/2014/197072
Subject(s) - fireworks , aerosol , atmospheric sciences , atmosphere (unit) , environmental science , radiative forcing , radiative transfer , climatology , forcing (mathematics) , geography , meteorology , physics , geology , archaeology , quantum mechanics
During Diwali festival, extensive burning of crackers and fireworks is made. Weeklong intensive observational campaign for aerosol study was carried out at a representative urban location in the eastern Indo-Gangetic Plain (IGP), Varanasi (25.3°N, 83.0°E), from October 29 to November 04, 2005 (Diwali on November 01, 2005), to investigate behavioral change of aerosol properties and radiative forcing between firework affected and nonaffected periods. Results show a substantial increase (~27%) in aerosol optical depth, aerosol absorption coefficients, and aerosol scattering coefficients during affected period as compared to non-affected periods. Magnitudes of radiative forcing at top of atmosphere during affected and non-affected periods are found to be +10 ± 1 and +12 ± 1 Wm−2, respectively, which are −31 ± 7 and −17 ± 5 Wm−2, respectively, at surface. It suggests an additional cooling of ~20% at top of atmosphere, ~45% cooling at surface, and additional atmospheric heating of 0.23 Kday−1 during fireworks affected period, which is ~30% higher than the non-affected period average

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