Influence of air temperature on air composition in Moscow
Abstract Empirical relations between T and surface concentrations of CO 2 and five minor air gases have been studied on a base of hourly data during 12 years. In wide range -6…+15 °C significant changes of minor gases are absent. Real tendencies are increase of O 3 and, vice versa, fall of NO and NO...
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crioppubl:10.1088/1755-1315/1040/1/012007 2024-06-02T08:02:21+00:00 Influence of air temperature on air composition in Moscow Lokoshchenko, M A Bogdanovich, A Yu Elansky, N F 2022 http://dx.doi.org/10.1088/1755-1315/1040/1/012007 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012007 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012007/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 1040, issue 1, page 012007 ISSN 1755-1307 1755-1315 journal-article 2022 crioppubl https://doi.org/10.1088/1755-1315/1040/1/012007 2024-05-07T14:06:41Z Abstract Empirical relations between T and surface concentrations of CO 2 and five minor air gases have been studied on a base of hourly data during 12 years. In wide range -6…+15 °C significant changes of minor gases are absent. Real tendencies are increase of O 3 and, vice versa, fall of NO and NO 2 with increasing T from +15.+17 to +38 °C. Both effects are a consequence of unstable stratification that enhances vertical mixing. In cool weather -7.-18 °C O 3 falls whereas nitrogen oxides grow with decreasing T due to frequent inversions and slowing down the NO oxidation rate. At an even lower temperature up to -30 °C NO and NO 2 , vice versa, decrease with decreasing T – probably, due to strong cold advection of clean Arctic air. Unlike minor gases, CO 2 decreases with increasing T up to 25 °C due to photosynthesis intensification from winter to summer. Seeming growth of CO at T>27 °C is fully explained by smoky haze during heat waves in 2010 and 2002. The CO 2 growth in hot weather is also created by heat stress of trees. Thus, except only oxidation rate, any influence of T is indirect as a result of stratification, photosynthesis, smoky haze, advection, etc. Article in Journal/Newspaper Arctic IOP Publishing Arctic IOP Conference Series: Earth and Environmental Science 1040 1 012007 |
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Abstract Empirical relations between T and surface concentrations of CO 2 and five minor air gases have been studied on a base of hourly data during 12 years. In wide range -6…+15 °C significant changes of minor gases are absent. Real tendencies are increase of O 3 and, vice versa, fall of NO and NO 2 with increasing T from +15.+17 to +38 °C. Both effects are a consequence of unstable stratification that enhances vertical mixing. In cool weather -7.-18 °C O 3 falls whereas nitrogen oxides grow with decreasing T due to frequent inversions and slowing down the NO oxidation rate. At an even lower temperature up to -30 °C NO and NO 2 , vice versa, decrease with decreasing T – probably, due to strong cold advection of clean Arctic air. Unlike minor gases, CO 2 decreases with increasing T up to 25 °C due to photosynthesis intensification from winter to summer. Seeming growth of CO at T>27 °C is fully explained by smoky haze during heat waves in 2010 and 2002. The CO 2 growth in hot weather is also created by heat stress of trees. Thus, except only oxidation rate, any influence of T is indirect as a result of stratification, photosynthesis, smoky haze, advection, etc. |
format |
Article in Journal/Newspaper |
author |
Lokoshchenko, M A Bogdanovich, A Yu Elansky, N F |
spellingShingle |
Lokoshchenko, M A Bogdanovich, A Yu Elansky, N F Influence of air temperature on air composition in Moscow |
author_facet |
Lokoshchenko, M A Bogdanovich, A Yu Elansky, N F |
author_sort |
Lokoshchenko, M A |
title |
Influence of air temperature on air composition in Moscow |
title_short |
Influence of air temperature on air composition in Moscow |
title_full |
Influence of air temperature on air composition in Moscow |
title_fullStr |
Influence of air temperature on air composition in Moscow |
title_full_unstemmed |
Influence of air temperature on air composition in Moscow |
title_sort |
influence of air temperature on air composition in moscow |
publisher |
IOP Publishing |
publishDate |
2022 |
url |
http://dx.doi.org/10.1088/1755-1315/1040/1/012007 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012007 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012007/pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
IOP Conference Series: Earth and Environmental Science volume 1040, issue 1, page 012007 ISSN 1755-1307 1755-1315 |
op_rights |
http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining |
op_doi |
https://doi.org/10.1088/1755-1315/1040/1/012007 |
container_title |
IOP Conference Series: Earth and Environmental Science |
container_volume |
1040 |
container_issue |
1 |
container_start_page |
012007 |
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1800746848783171584 |