Seasonal and Interannual Variability of Aerosol Characteristics According to the Data of Long-Term (2011–2021) Measurements at the Russian Scientific Center on the Spitzbergen Archipelago
— The results of the analysis of seasonal and interannual variability of the aerosol optical depth of the atmosphere (AOD), the aerosol volume concentration, and the mass concentration of black carbon in the surface layer obtained at observations in Barentsburg (Spitzbergen archipelago) in 2011–2021...
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| Veröffentlicht in: | Atmospheric and oceanic optics 2023-12, Vol.36 (6), p.645-654 |
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| container_issue | 6 |
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| container_title | Atmospheric and oceanic optics |
| container_volume | 36 |
| creator | Kabanov, D. M. Maslovsky, A. S. Radionov, V. F. Sakerin, S. M. Sidorova, O. R. Chernov, D. G. |
| description | —
The results of the analysis of seasonal and interannual variability of the aerosol optical depth of the atmosphere (AOD), the aerosol volume concentration, and the mass concentration of black carbon in the surface layer obtained at observations in Barentsburg (Spitzbergen archipelago) in 2011–2021 are presented. The annual behavior of all parameters is characterized by two maxima: spring (or winter-spring) and summer, apparently due to the transport of pollutants from the middle latitudes in the winter-spring period and smoke aerosol in summer. In the interannual variability, there are significant negative trends in the fine AOD component (−0.012 over 11 years) and the mass concentration of the absorbing substance (by 46.7 ng/m
3
over 10 years). |
| doi_str_mv | 10.1134/S1024856023060106 |
| format | Article |
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The results of the analysis of seasonal and interannual variability of the aerosol optical depth of the atmosphere (AOD), the aerosol volume concentration, and the mass concentration of black carbon in the surface layer obtained at observations in Barentsburg (Spitzbergen archipelago) in 2011–2021 are presented. The annual behavior of all parameters is characterized by two maxima: spring (or winter-spring) and summer, apparently due to the transport of pollutants from the middle latitudes in the winter-spring period and smoke aerosol in summer. In the interannual variability, there are significant negative trends in the fine AOD component (−0.012 over 11 years) and the mass concentration of the absorbing substance (by 46.7 ng/m
3
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The results of the analysis of seasonal and interannual variability of the aerosol optical depth of the atmosphere (AOD), the aerosol volume concentration, and the mass concentration of black carbon in the surface layer obtained at observations in Barentsburg (Spitzbergen archipelago) in 2011–2021 are presented. The annual behavior of all parameters is characterized by two maxima: spring (or winter-spring) and summer, apparently due to the transport of pollutants from the middle latitudes in the winter-spring period and smoke aerosol in summer. In the interannual variability, there are significant negative trends in the fine AOD component (−0.012 over 11 years) and the mass concentration of the absorbing substance (by 46.7 ng/m
3
over 10 years).</description><subject>Aerosols</subject><subject>Archipelagoes</subject><subject>Black carbon</subject><subject>Hydrosoles</subject><subject>Lasers</subject><subject>Optical analysis</subject><subject>Optical Devices</subject><subject>Optical thickness</subject><subject>Optics</subject><subject>Optics of Clusters</subject><subject>Photonics</subject><subject>Physics</subject><subject>Physics and Astronomy</subject><subject>Pollution dispersion</subject><subject>Pollution transport</subject><subject>Spring</subject><subject>Spring (season)</subject><subject>Summer</subject><subject>Surface layers</subject><subject>Variability</subject><subject>Winter</subject><issn>1024-8560</issn><issn>2070-0393</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp1kc1u1DAQgC1EJZaWB-BmiQscUsY_cZLjavmrtKgSW7hGjjPJusrai-0cyol34Hl4GZ6kTheJA-ppbM_3zVgzhLxkcMmYkG93DLisSwVcgAIG6glZcaigANGIp2S1pIsl_4w8j_EWQJVNyVbk9w519E5PVLueXrmEQTs35_s3Hazu7GTTHfUDXWPw0U90s9dBm4zZmKyJdG2MD711I02epj3SdzrpRdh6NxY3GA70NQfG_vz8xYGzN_RzbjgHPKBLker04HyZY7Ta0Z2x-dkO1tANLn-h3j0Au6NNPzoMIzq6DmZvjzjp0V-Qs0FPEV_8jefk64f3N5tPxfb649VmvS2MYCoVqFQnOsPkUJUlh6EUoIUUAkWNlVlCZ2TVSCN73QsmQdRV3wwI-Yyq6cQ5eXWqewz--4wxtbd-DnlqseUNUyDrStWZYifK5FHFgEN7DPagw13LoF221P63pezwkxMz60YM_yo_Lt0DD4-ViA</recordid><startdate>20231201</startdate><enddate>20231201</enddate><creator>Kabanov, D. M.</creator><creator>Maslovsky, A. S.</creator><creator>Radionov, V. F.</creator><creator>Sakerin, S. M.</creator><creator>Sidorova, O. R.</creator><creator>Chernov, D. G.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20231201</creationdate><title>Seasonal and Interannual Variability of Aerosol Characteristics According to the Data of Long-Term (2011–2021) Measurements at the Russian Scientific Center on the Spitzbergen Archipelago</title><author>Kabanov, D. M. ; Maslovsky, A. S. ; Radionov, V. F. ; Sakerin, S. M. ; Sidorova, O. R. ; Chernov, D. G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-e66b3bc14f75520f530a3433e38e7c3e38bc4794c4dad3140387d9fe0314e69b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Aerosols</topic><topic>Archipelagoes</topic><topic>Black carbon</topic><topic>Hydrosoles</topic><topic>Lasers</topic><topic>Optical analysis</topic><topic>Optical Devices</topic><topic>Optical thickness</topic><topic>Optics</topic><topic>Optics of Clusters</topic><topic>Photonics</topic><topic>Physics</topic><topic>Physics and Astronomy</topic><topic>Pollution dispersion</topic><topic>Pollution transport</topic><topic>Spring</topic><topic>Spring (season)</topic><topic>Summer</topic><topic>Surface layers</topic><topic>Variability</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kabanov, D. M.</creatorcontrib><creatorcontrib>Maslovsky, A. S.</creatorcontrib><creatorcontrib>Radionov, V. F.</creatorcontrib><creatorcontrib>Sakerin, S. M.</creatorcontrib><creatorcontrib>Sidorova, O. R.</creatorcontrib><creatorcontrib>Chernov, D. G.</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Atmospheric and oceanic optics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kabanov, D. M.</au><au>Maslovsky, A. S.</au><au>Radionov, V. F.</au><au>Sakerin, S. M.</au><au>Sidorova, O. R.</au><au>Chernov, D. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Seasonal and Interannual Variability of Aerosol Characteristics According to the Data of Long-Term (2011–2021) Measurements at the Russian Scientific Center on the Spitzbergen Archipelago</atitle><jtitle>Atmospheric and oceanic optics</jtitle><stitle>Atmos Ocean Opt</stitle><date>2023-12-01</date><risdate>2023</risdate><volume>36</volume><issue>6</issue><spage>645</spage><epage>654</epage><pages>645-654</pages><issn>1024-8560</issn><eissn>2070-0393</eissn><abstract>—
The results of the analysis of seasonal and interannual variability of the aerosol optical depth of the atmosphere (AOD), the aerosol volume concentration, and the mass concentration of black carbon in the surface layer obtained at observations in Barentsburg (Spitzbergen archipelago) in 2011–2021 are presented. The annual behavior of all parameters is characterized by two maxima: spring (or winter-spring) and summer, apparently due to the transport of pollutants from the middle latitudes in the winter-spring period and smoke aerosol in summer. In the interannual variability, there are significant negative trends in the fine AOD component (−0.012 over 11 years) and the mass concentration of the absorbing substance (by 46.7 ng/m
3
over 10 years).</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1024856023060106</doi><tpages>10</tpages></addata></record> |
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| ispartof | Atmospheric and oceanic optics, 2023-12, Vol.36 (6), p.645-654 |
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| source | Springer Nature - Complete Springer Journals |
| subjects | Aerosols Archipelagoes Black carbon Hydrosoles Lasers Optical analysis Optical Devices Optical thickness Optics Optics of Clusters Photonics Physics Physics and Astronomy Pollution dispersion Pollution transport Spring Spring (season) Summer Surface layers Variability Winter |
| title | Seasonal and Interannual Variability of Aerosol Characteristics According to the Data of Long-Term (2011–2021) Measurements at the Russian Scientific Center on the Spitzbergen Archipelago |
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