Short-term tropospheric ozone trend in India
Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jana, P. K. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Anmerkung: |
© Indian Association for the Cultivation of Science 2012 |
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| Übergeordnetes Werk: |
Enthalten in: Indian journal of physics - New Delhi : Springer India, 2009, 86(2012), 11 vom: 15. Juli, Seite 951-960 |
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| Übergeordnetes Werk: |
volume:86 ; year:2012 ; number:11 ; day:15 ; month:07 ; pages:951-960 |
| Links: |
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| DOI / URN: |
10.1007/s12648-012-0156-5 |
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| Katalog-ID: |
SPR026546132 |
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| 520 | |a Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. | ||
| 650 | 4 | |a Tropospheric ozone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Seasonal variation of ozone |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Latitudinal variation of ozone |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Goswami, S. |4 aut | |
| 700 | 1 | |a Midya, S. K. |4 aut | |
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10.1007/s12648-012-0156-5 doi (DE-627)SPR026546132 (SPR)s12648-012-0156-5-e DE-627 ger DE-627 rakwb eng Jana, P. K. verfasserin aut Short-term tropospheric ozone trend in India 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Indian Association for the Cultivation of Science 2012 Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 Goswami, S. aut Midya, S. K. aut Enthalten in Indian journal of physics New Delhi : Springer India, 2009 86(2012), 11 vom: 15. Juli, Seite 951-960 (DE-627)606030921 (DE-600)2508021-0 0974-9845 nnns volume:86 year:2012 number:11 day:15 month:07 pages:951-960 https://dx.doi.org/10.1007/s12648-012-0156-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2012 11 15 07 951-960 |
| spelling |
10.1007/s12648-012-0156-5 doi (DE-627)SPR026546132 (SPR)s12648-012-0156-5-e DE-627 ger DE-627 rakwb eng Jana, P. K. verfasserin aut Short-term tropospheric ozone trend in India 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Indian Association for the Cultivation of Science 2012 Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 Goswami, S. aut Midya, S. K. aut Enthalten in Indian journal of physics New Delhi : Springer India, 2009 86(2012), 11 vom: 15. Juli, Seite 951-960 (DE-627)606030921 (DE-600)2508021-0 0974-9845 nnns volume:86 year:2012 number:11 day:15 month:07 pages:951-960 https://dx.doi.org/10.1007/s12648-012-0156-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2012 11 15 07 951-960 |
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10.1007/s12648-012-0156-5 doi (DE-627)SPR026546132 (SPR)s12648-012-0156-5-e DE-627 ger DE-627 rakwb eng Jana, P. K. verfasserin aut Short-term tropospheric ozone trend in India 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Indian Association for the Cultivation of Science 2012 Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 Goswami, S. aut Midya, S. K. aut Enthalten in Indian journal of physics New Delhi : Springer India, 2009 86(2012), 11 vom: 15. Juli, Seite 951-960 (DE-627)606030921 (DE-600)2508021-0 0974-9845 nnns volume:86 year:2012 number:11 day:15 month:07 pages:951-960 https://dx.doi.org/10.1007/s12648-012-0156-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2012 11 15 07 951-960 |
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10.1007/s12648-012-0156-5 doi (DE-627)SPR026546132 (SPR)s12648-012-0156-5-e DE-627 ger DE-627 rakwb eng Jana, P. K. verfasserin aut Short-term tropospheric ozone trend in India 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Indian Association for the Cultivation of Science 2012 Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 Goswami, S. aut Midya, S. K. aut Enthalten in Indian journal of physics New Delhi : Springer India, 2009 86(2012), 11 vom: 15. Juli, Seite 951-960 (DE-627)606030921 (DE-600)2508021-0 0974-9845 nnns volume:86 year:2012 number:11 day:15 month:07 pages:951-960 https://dx.doi.org/10.1007/s12648-012-0156-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2012 11 15 07 951-960 |
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10.1007/s12648-012-0156-5 doi (DE-627)SPR026546132 (SPR)s12648-012-0156-5-e DE-627 ger DE-627 rakwb eng Jana, P. K. verfasserin aut Short-term tropospheric ozone trend in India 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Indian Association for the Cultivation of Science 2012 Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 Goswami, S. aut Midya, S. K. aut Enthalten in Indian journal of physics New Delhi : Springer India, 2009 86(2012), 11 vom: 15. Juli, Seite 951-960 (DE-627)606030921 (DE-600)2508021-0 0974-9845 nnns volume:86 year:2012 number:11 day:15 month:07 pages:951-960 https://dx.doi.org/10.1007/s12648-012-0156-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 86 2012 11 15 07 951-960 |
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Jana, P. K. |
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Short-term tropospheric ozone trend in India Tropospheric ozone (dpeaa)DE-He213 Seasonal variation of ozone (dpeaa)DE-He213 Latitudinal variation of ozone (dpeaa)DE-He213 |
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Short-term tropospheric ozone trend in India |
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short-term tropospheric ozone trend in india |
| title_auth |
Short-term tropospheric ozone trend in India |
| abstract |
Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. © Indian Association for the Cultivation of Science 2012 |
| abstractGer |
Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. © Indian Association for the Cultivation of Science 2012 |
| abstract_unstemmed |
Abstract The nature of monthly, seasonal and latitudinal short-term variations of tropospheric ozone over different stations in India are presented in this paper. Monthly variations depict that at all stations, the nature of monthly mean tropospheric ozone column was oscillatory and had increasing trends from October, 2004 to June, 2009. At most of the places over India it is observed that tropospheric ozone densities had increased sharply from the month of January, attained the maximum value in the month of May, then decreased steeply achieving the lowest value in the month of August and finally had increased gradually from August to December during this period. Seasonal variations clearly reveal that tropospheric ozone value attained maximum during pre-monsoon time and minimum during monsoon time at all the stations except Simla and Srinagar. Winter, pre-monsoon and post-monsoon tropospheric ozone build up had been observed from 2004 to 2009, whereas monsoon ozone decline had been exhibited for the above period over most of the places in India. Tropospheric monthly mean, pre-monsoon, monsoon and post-monsoon ozone had enhanced with rise in latitude in Indian region. Chemical explanations have been proposed for such variations. © Indian Association for the Cultivation of Science 2012 |
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Short-term tropospheric ozone trend in India |
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https://dx.doi.org/10.1007/s12648-012-0156-5 |
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Goswami, S. Midya, S. K. |
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Goswami, S. Midya, S. K. |
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| doi_str |
10.1007/s12648-012-0156-5 |
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2024-07-03T21:26:20.267Z |
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