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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Wiley
2014-01-01
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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. |
format | Article |
id | doaj-art-61e9da7dafba42b5b5763354bd21605f |
institution | Kabale University |
issn | 1687-9309 1687-9317 |
language | English |
publishDate | 2014-01-01 |
publisher | Wiley |
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series | Advances in Meteorology |
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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