Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India
The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rama Gopal, K. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Schlagwörter: |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction - Nassar, M.K. ELSEVIER, 2021, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:84 ; year:2014 ; pages:294-306 ; extent:13 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.atmosenv.2013.10.014 |
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ELV022970851 |
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| 520 | |a The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. | ||
| 520 | |a The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. | ||
| 650 | 7 | |a Ozone |2 Elsevier | |
| 650 | 7 | |a Nitrogen oxides |2 Elsevier | |
| 650 | 7 | |a UV radiation and chemical box model |2 Elsevier | |
| 650 | 7 | |a Boundary layer |2 Elsevier | |
| 700 | 1 | |a Lingaswamy, A.P. |4 oth | |
| 700 | 1 | |a Arafath, S.Md. |4 oth | |
| 700 | 1 | |a Balakrishnaiah, G. |4 oth | |
| 700 | 1 | |a Pavan Kumari, S. |4 oth | |
| 700 | 1 | |a Uma Devi, K. |4 oth | |
| 700 | 1 | |a Siva Kumar Reddy, N. |4 oth | |
| 700 | 1 | |a Raja Obul Reddy, K. |4 oth | |
| 700 | 1 | |a Reddy, R.R. |4 oth | |
| 700 | 1 | |a Abdul Azeem, P. |4 oth | |
| 700 | 1 | |a Lal, Shyam |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Nassar, M.K. ELSEVIER |t The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction |d 2021 |g Amsterdam [u.a.] |w (DE-627)ELV00656139X |
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10.1016/j.atmosenv.2013.10.014 doi GBVA2014018000020.pica (DE-627)ELV022970851 (ELSEVIER)S1352-2310(13)00767-X DE-627 ger DE-627 rakwb eng 550 690 550 DE-600 690 DE-600 610 VZ 44.65 bkl Rama Gopal, K. verfasserin aut Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. Ozone Elsevier Nitrogen oxides Elsevier UV radiation and chemical box model Elsevier Boundary layer Elsevier Lingaswamy, A.P. oth Arafath, S.Md. oth Balakrishnaiah, G. oth Pavan Kumari, S. oth Uma Devi, K. oth Siva Kumar Reddy, N. oth Raja Obul Reddy, K. oth Reddy, R.R. oth Abdul Azeem, P. oth Lal, Shyam oth Enthalten in Elsevier Science Nassar, M.K. ELSEVIER The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction 2021 Amsterdam [u.a.] (DE-627)ELV00656139X volume:84 year:2014 pages:294-306 extent:13 https://doi.org/10.1016/j.atmosenv.2013.10.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.65 Chirurgie VZ AR 84 2014 294-306 13 045F 550 |
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10.1016/j.atmosenv.2013.10.014 doi GBVA2014018000020.pica (DE-627)ELV022970851 (ELSEVIER)S1352-2310(13)00767-X DE-627 ger DE-627 rakwb eng 550 690 550 DE-600 690 DE-600 610 VZ 44.65 bkl Rama Gopal, K. verfasserin aut Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. Ozone Elsevier Nitrogen oxides Elsevier UV radiation and chemical box model Elsevier Boundary layer Elsevier Lingaswamy, A.P. oth Arafath, S.Md. oth Balakrishnaiah, G. oth Pavan Kumari, S. oth Uma Devi, K. oth Siva Kumar Reddy, N. oth Raja Obul Reddy, K. oth Reddy, R.R. oth Abdul Azeem, P. oth Lal, Shyam oth Enthalten in Elsevier Science Nassar, M.K. ELSEVIER The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction 2021 Amsterdam [u.a.] (DE-627)ELV00656139X volume:84 year:2014 pages:294-306 extent:13 https://doi.org/10.1016/j.atmosenv.2013.10.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.65 Chirurgie VZ AR 84 2014 294-306 13 045F 550 |
| allfields_unstemmed |
10.1016/j.atmosenv.2013.10.014 doi GBVA2014018000020.pica (DE-627)ELV022970851 (ELSEVIER)S1352-2310(13)00767-X DE-627 ger DE-627 rakwb eng 550 690 550 DE-600 690 DE-600 610 VZ 44.65 bkl Rama Gopal, K. verfasserin aut Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. Ozone Elsevier Nitrogen oxides Elsevier UV radiation and chemical box model Elsevier Boundary layer Elsevier Lingaswamy, A.P. oth Arafath, S.Md. oth Balakrishnaiah, G. oth Pavan Kumari, S. oth Uma Devi, K. oth Siva Kumar Reddy, N. oth Raja Obul Reddy, K. oth Reddy, R.R. oth Abdul Azeem, P. oth Lal, Shyam oth Enthalten in Elsevier Science Nassar, M.K. ELSEVIER The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction 2021 Amsterdam [u.a.] (DE-627)ELV00656139X volume:84 year:2014 pages:294-306 extent:13 https://doi.org/10.1016/j.atmosenv.2013.10.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.65 Chirurgie VZ AR 84 2014 294-306 13 045F 550 |
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10.1016/j.atmosenv.2013.10.014 doi GBVA2014018000020.pica (DE-627)ELV022970851 (ELSEVIER)S1352-2310(13)00767-X DE-627 ger DE-627 rakwb eng 550 690 550 DE-600 690 DE-600 610 VZ 44.65 bkl Rama Gopal, K. verfasserin aut Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. Ozone Elsevier Nitrogen oxides Elsevier UV radiation and chemical box model Elsevier Boundary layer Elsevier Lingaswamy, A.P. oth Arafath, S.Md. oth Balakrishnaiah, G. oth Pavan Kumari, S. oth Uma Devi, K. oth Siva Kumar Reddy, N. oth Raja Obul Reddy, K. oth Reddy, R.R. oth Abdul Azeem, P. oth Lal, Shyam oth Enthalten in Elsevier Science Nassar, M.K. ELSEVIER The internal pudendal artery turnover (IPAT) flap: A new, simple and reliable technique for perineal reconstruction 2021 Amsterdam [u.a.] (DE-627)ELV00656139X volume:84 year:2014 pages:294-306 extent:13 https://doi.org/10.1016/j.atmosenv.2013.10.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.65 Chirurgie VZ AR 84 2014 294-306 13 045F 550 |
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seasonal heterogeneity in ozone and its precursors (no x ) by in-situ and model observations on semi-arid station in anantapur (a.p), south india |
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Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India |
| abstract |
The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. |
| abstractGer |
The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. |
| abstract_unstemmed |
The continuous measurements of surface ozone (O3) and oxides of nitrogen (NO x ) present in the ambient air were carried out on a semi-arid rural area in Anantapur [14.62° N, 77.65° E], South India during the period beginning from March 2012 to February 2013. The diurnal variation of surface ozone (O3) showed a minimum at sun rise and late evenings and maximum at noon time, due to slow titration of O3 with oxides of nitrogen (NO x ). The monthly average minimum/maximum of O3 observed in August/March was 19.9 ± 0.3/55.8 ± 2.9 ppbv. The monthly average variation of NO x was found to be high (6.67 ± 0.8) in November and noticed low (2.07 ± 0.2) concentrations in May. The monthly mean maximum of O3 during day time (night time) was observed as 64.9 ± 5.3 (45.3 ± 4.1) ppbv in March, and mean low concentration was about 19.9 ± 1.02 (12.8 ± 0.9) ppbv in August. The monthly mean enhanced concentration of NO x during the day time/night time was about 5.0 ± 0.6/8.7 ± 0.9 in November and the fallen concentration was noticed 1.5 ± 0.2/2.7 ± 0.3 in May. The spatial distribution of O3 was associated with the air flow pattern, air mass trajectories and boundary layer heights. The water vapor content also played a significant role in the diurnal variation of O3 in addition to photo chemistry. The diurnal variation of UV radiation with O3 and NO x has been analyzed and the results are reported. And the diurnal and seasonal variations in boundary layer height have also been discussed. The monthly mean variation of aerosol optical depth (AOD) is similar to that of tropospheric ozone, with a correlation coefficient of r = 0.60. The diurnal and seasonal patterns of ozone were simulated using the chemical box model (NCAR Mater Mechanism) and when compared with the observed ones, the results are found to be in good agreement with the observed ones. |
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| title_short |
Seasonal heterogeneity in ozone and its precursors (NO x ) by in-situ and model observations on semi-arid station in Anantapur (A.P), South India |
| url |
https://doi.org/10.1016/j.atmosenv.2013.10.014 |
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| author2 |
Lingaswamy, A.P. Arafath, S.Md Balakrishnaiah, G. Pavan Kumari, S. Uma Devi, K. Siva Kumar Reddy, N. Raja Obul Reddy, K. Reddy, R.R. Abdul Azeem, P. Lal, Shyam |
| author2Str |
Lingaswamy, A.P. Arafath, S.Md Balakrishnaiah, G. Pavan Kumari, S. Uma Devi, K. Siva Kumar Reddy, N. Raja Obul Reddy, K. Reddy, R.R. Abdul Azeem, P. Lal, Shyam |
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| doi_str |
10.1016/j.atmosenv.2013.10.014 |
| up_date |
2024-07-06T17:37:24.429Z |
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