Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study

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 (Diwal...

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Main Authors: B. P. Singh, A. K. Srivastava, S. Tiwari, S. Singh, R. K. Singh, D. S. Bisht, D. M. Lal, A. K. Singh, R. K. Mall, Manoj K. Srivastava
Format: Article
Language:English
Published: Wiley 2014-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2014/197072
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author B. P. Singh
A. K. Srivastava
S. Tiwari
S. Singh
R. K. Singh
D. S. Bisht
D. M. Lal
A. K. Singh
R. K. Mall
Manoj K. Srivastava
author_facet B. P. Singh
A. K. Srivastava
S. Tiwari
S. Singh
R. K. Singh
D. S. Bisht
D. M. Lal
A. K. Singh
R. K. Mall
Manoj K. Srivastava
author_sort B. P. Singh
collection DOAJ
description 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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spelling doaj-art-61e9da7dafba42b5b5763354bd21605f2025-02-03T01:09:48ZengWileyAdvances in Meteorology1687-93091687-93172014-01-01201410.1155/2014/197072197072Radiative Impact of Fireworks at a Tropical Indian Location: A Case StudyB. P. Singh0A. K. Srivastava1S. Tiwari2S. Singh3R. K. Singh4D. S. Bisht5D. M. Lal6A. K. Singh7R. K. Mall8Manoj K. Srivastava9Department of Geophysics, Banaras Hindu University, Varanasi 221005, IndiaIndian Institute of Tropical Meteorology (Branch), Prof. Ram Nath Vij Marg, New Delhi 110060, IndiaIndian Institute of Tropical Meteorology (Branch), Prof. Ram Nath Vij Marg, New Delhi 110060, IndiaRadio and Atmospheric Sciences Division, National Physical Laboratory, New Delhi 110012, IndiaDepartment of Geophysics, Banaras Hindu University, Varanasi 221005, IndiaDepartment of Geophysics, Banaras Hindu University, Varanasi 221005, IndiaDepartment of Geophysics, Banaras Hindu University, Varanasi 221005, IndiaDepartment of Physics, Banaras Hindu University, Varanasi 221005, IndiaInstitute of Environment and Sustainable Development, Banaras Hindu University, Varanasi 221005, IndiaDepartment of Geophysics, Banaras Hindu University, Varanasi 221005, IndiaDuring 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.http://dx.doi.org/10.1155/2014/197072
spellingShingle B. P. Singh
A. K. Srivastava
S. Tiwari
S. Singh
R. K. Singh
D. S. Bisht
D. M. Lal
A. K. Singh
R. K. Mall
Manoj K. Srivastava
Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
Advances in Meteorology
title Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
title_full Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
title_fullStr Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
title_full_unstemmed Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
title_short Radiative Impact of Fireworks at a Tropical Indian Location: A Case Study
title_sort radiative impact of fireworks at a tropical indian location a case study
url http://dx.doi.org/10.1155/2014/197072
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