SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA
In the present study, 3-D chemical transport model, MOZART-4 (Model for Ozone and Related chemical Tracers-Version-4) has been used to study the seasonal and spatial distribution of surface ozone (O<sub>3</sub>) over India. To illustrate the capabilities of model, the simulations are com...
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Copernicus Publications
2018-11-01
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Series: | ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences |
Online Access: | https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/IV-5/375/2018/isprs-annals-IV-5-375-2018.pdf |
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author | Y. Yarragunta Y. Yarragunta S. Srivastava D. Mitra H. C. Chandola |
author_facet | Y. Yarragunta Y. Yarragunta S. Srivastava D. Mitra H. C. Chandola |
author_sort | Y. Yarragunta |
collection | DOAJ |
description | In the present study, 3-D chemical transport model, MOZART-4 (Model for Ozone and Related chemical Tracers-Version-4) has been used to study the seasonal and spatial distribution of surface ozone (O<sub>3</sub>) over India. To illustrate the capabilities of model, the simulations are compared with the ground-based observations. The model reproduces the principal features present in ground-based observations. However, model is unable to simulate very low concentration of O<sub>3</sub> during monsoon months. The model simulations are used to quantify the contribution of background ozone and Indian anthropogenic emissions to the variability of surface O<sub>3</sub>. The spatial distribution of total O<sub>3</sub> (TO) shows maximum over Indo-Gangetic plains (IGP) and Eastern India while minimum over southern Indian region. The seasonal cycle of TO vary from 34.2 ± 7.6 to 51.9 ± 4.9 ppbv over the Indian landmass region due to changes in its topography and ozone lifetime. Annual mean total background O<sub>3</sub> (TBO) over India shows highest during spring (29.3 ± 5.0 ppbv) and lowest during monsoon (19.6 ± 3.4 ppbv). Both Natural background O<sub>3</sub> (NBO) and pollution background O<sub>3</sub> (PBO) shows a minimum in summer which are essentially following the seasonal changes of total ozone. Significant variation of India pollution O<sub>3</sub> (IPO) is found over India and the spatial variation of IPO follows the spatial variation of TO as well as spatial variation of emission of ozone precursors. |
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issn | 2194-9042 2194-9050 |
language | English |
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publishDate | 2018-11-01 |
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spelling | doaj.art-77f10b0c4a414d8995d361c3743bc6802022-12-22T02:52:59ZengCopernicus PublicationsISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences2194-90422194-90502018-11-01IV-537538110.5194/isprs-annals-IV-5-375-2018SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIAY. Yarragunta0Y. Yarragunta1S. Srivastava2D. Mitra3H. C. Chandola4Indian Institute of Remote Sensing, ISRO, Dehradun, IndiaDepartment of Physics, Kumaun University, Nainital, IndiaIndian Institute of Remote Sensing, ISRO, Dehradun, IndiaIndian Institute of Remote Sensing, ISRO, Dehradun, IndiaDepartment of Physics, Kumaun University, Nainital, IndiaIn the present study, 3-D chemical transport model, MOZART-4 (Model for Ozone and Related chemical Tracers-Version-4) has been used to study the seasonal and spatial distribution of surface ozone (O<sub>3</sub>) over India. To illustrate the capabilities of model, the simulations are compared with the ground-based observations. The model reproduces the principal features present in ground-based observations. However, model is unable to simulate very low concentration of O<sub>3</sub> during monsoon months. The model simulations are used to quantify the contribution of background ozone and Indian anthropogenic emissions to the variability of surface O<sub>3</sub>. The spatial distribution of total O<sub>3</sub> (TO) shows maximum over Indo-Gangetic plains (IGP) and Eastern India while minimum over southern Indian region. The seasonal cycle of TO vary from 34.2 ± 7.6 to 51.9 ± 4.9 ppbv over the Indian landmass region due to changes in its topography and ozone lifetime. Annual mean total background O<sub>3</sub> (TBO) over India shows highest during spring (29.3 ± 5.0 ppbv) and lowest during monsoon (19.6 ± 3.4 ppbv). Both Natural background O<sub>3</sub> (NBO) and pollution background O<sub>3</sub> (PBO) shows a minimum in summer which are essentially following the seasonal changes of total ozone. Significant variation of India pollution O<sub>3</sub> (IPO) is found over India and the spatial variation of IPO follows the spatial variation of TO as well as spatial variation of emission of ozone precursors.https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/IV-5/375/2018/isprs-annals-IV-5-375-2018.pdf |
spellingShingle | Y. Yarragunta Y. Yarragunta S. Srivastava D. Mitra H. C. Chandola SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences |
title | SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA |
title_full | SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA |
title_fullStr | SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA |
title_full_unstemmed | SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA |
title_short | SEASONAL AND SPATIAL VARIABILITY OF OZONE INFERRED FROM GLOBAL CHEMISTRY TRANSPORT MODEL SIMULATIONS OVER INDIA |
title_sort | seasonal and spatial variability of ozone inferred from global chemistry transport model simulations over india |
url | https://www.isprs-ann-photogramm-remote-sens-spatial-inf-sci.net/IV-5/375/2018/isprs-annals-IV-5-375-2018.pdf |
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