Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer
The influence of increased concentrations of submicron aerosol produced by forest fires on thermal characteristics of the atmospheric boundary layer (ABL) in Moscow and its remote vicinity (the town of Zvenigorod) are analyzed on the basis of regular remote measurements of the ABL temperature profil...
Gespeichert in:
| Veröffentlicht in: | Izvestiya. Atmospheric and oceanic physics 2006-12, Vol.42 (6), p.715-721 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 721 |
|---|---|
| container_issue | 6 |
| container_start_page | 715 |
| container_title | Izvestiya. Atmospheric and oceanic physics |
| container_volume | 42 |
| creator | Khaikin, M N Kuznetsova, IN Kadygrov, EN |
| description | The influence of increased concentrations of submicron aerosol produced by forest fires on thermal characteristics of the atmospheric boundary layer (ABL) in Moscow and its remote vicinity (the town of Zvenigorod) are analyzed on the basis of regular remote measurements of the ABL temperature profile with the use of MTP-5 profilers. In the air basin of a large city, additional aerosol and accompanying pollutants in early morning hours (at small heights of the Sun) most frequently did not cause substantial changes in the ABL thermal structure. In the locality remote from the megalopolis (Zvenigorod), the atmospheric pollution by aerosol led to noticeable changes in the ABL thermal characteristics. Especially strong changes were observed in the daytime, during the maximum supply of solar radiation. In morning hours, the heating rate of the lower 100-m layer of the polluted air exceeded the heating rate of a relatively pure air by more than one degree. In higher layers, the differences between the rates of temperature changes in a relatively clean atmosphere and in an atmosphere polluted by aerosol (in the suburb) were insignificant. |
| doi_str_mv | 10.1134/S0001433806060065 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_902342140</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2177304841</sourcerecordid><originalsourceid>FETCH-LOGICAL-c335t-d2bdf34447321369dafe20a85348d38b5ba53300226e8014e16a36d43da882363</originalsourceid><addsrcrecordid>eNp9kcFKxDAQhoMouK4-gLfgQU_VJJOk6VEWVxcWPKjgraRN6nZpmzVJD_v2pq4nBZkZBub_EvhnELqk5JZS4HcvhBDKARSRKYgUR2hGhRCZZOr9GM0mOZv0U3QWwjYRjJN8hsxqaLrRDrXFrsEab9qPDdbWu-A6XLs0H6LXsXUDThk3dirf6w6H6Mc6jv774STo2LuwS2pb48qNg9F-jzu9t_4cnTS6C_bip8_R2_LhdfGUrZ8fV4v7dVYDiJgZVpkGOOc5MAqyMLqxjGglgCsDqhKVFgCEMCatSm4tlRqk4WC0UgwkzNHN4d-dd5-jDbHs21DbrtODdWMoC8KAM8pJIq__JRmhOaGFSODVL3DrRj8kF2UuKYgiB0gQPUB12lvwtil3vu2T_ZKScjpP-ec88AVm0IFt</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>761359733</pqid></control><display><type>article</type><title>Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer</title><source>SpringerLink Journals</source><creator>Khaikin, M N ; Kuznetsova, IN ; Kadygrov, EN</creator><creatorcontrib>Khaikin, M N ; Kuznetsova, IN ; Kadygrov, EN</creatorcontrib><description>The influence of increased concentrations of submicron aerosol produced by forest fires on thermal characteristics of the atmospheric boundary layer (ABL) in Moscow and its remote vicinity (the town of Zvenigorod) are analyzed on the basis of regular remote measurements of the ABL temperature profile with the use of MTP-5 profilers. In the air basin of a large city, additional aerosol and accompanying pollutants in early morning hours (at small heights of the Sun) most frequently did not cause substantial changes in the ABL thermal structure. In the locality remote from the megalopolis (Zvenigorod), the atmospheric pollution by aerosol led to noticeable changes in the ABL thermal characteristics. Especially strong changes were observed in the daytime, during the maximum supply of solar radiation. In morning hours, the heating rate of the lower 100-m layer of the polluted air exceeded the heating rate of a relatively pure air by more than one degree. In higher layers, the differences between the rates of temperature changes in a relatively clean atmosphere and in an atmosphere polluted by aerosol (in the suburb) were insignificant.</description><identifier>ISSN: 0001-4338</identifier><identifier>EISSN: 1555-628X</identifier><identifier>DOI: 10.1134/S0001433806060065</identifier><language>eng</language><publisher>Washington: Springer Nature B.V</publisher><subject>Aerosol concentration ; Aerosols ; Air pollution ; Atmosphere ; Atmospheric boundary layer ; Atmospheric pollution ; Boundary layer structure ; Boundary layers ; Forest fires ; Heating ; Solar radiation ; Temperature changes ; Temperature profiles ; Urban atmospheric pollution</subject><ispartof>Izvestiya. Atmospheric and oceanic physics, 2006-12, Vol.42 (6), p.715-721</ispartof><rights>Nauka/Interperiodica 2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c335t-d2bdf34447321369dafe20a85348d38b5ba53300226e8014e16a36d43da882363</citedby><cites>FETCH-LOGICAL-c335t-d2bdf34447321369dafe20a85348d38b5ba53300226e8014e16a36d43da882363</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Khaikin, M N</creatorcontrib><creatorcontrib>Kuznetsova, IN</creatorcontrib><creatorcontrib>Kadygrov, EN</creatorcontrib><title>Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer</title><title>Izvestiya. Atmospheric and oceanic physics</title><description>The influence of increased concentrations of submicron aerosol produced by forest fires on thermal characteristics of the atmospheric boundary layer (ABL) in Moscow and its remote vicinity (the town of Zvenigorod) are analyzed on the basis of regular remote measurements of the ABL temperature profile with the use of MTP-5 profilers. In the air basin of a large city, additional aerosol and accompanying pollutants in early morning hours (at small heights of the Sun) most frequently did not cause substantial changes in the ABL thermal structure. In the locality remote from the megalopolis (Zvenigorod), the atmospheric pollution by aerosol led to noticeable changes in the ABL thermal characteristics. Especially strong changes were observed in the daytime, during the maximum supply of solar radiation. In morning hours, the heating rate of the lower 100-m layer of the polluted air exceeded the heating rate of a relatively pure air by more than one degree. In higher layers, the differences between the rates of temperature changes in a relatively clean atmosphere and in an atmosphere polluted by aerosol (in the suburb) were insignificant.</description><subject>Aerosol concentration</subject><subject>Aerosols</subject><subject>Air pollution</subject><subject>Atmosphere</subject><subject>Atmospheric boundary layer</subject><subject>Atmospheric pollution</subject><subject>Boundary layer structure</subject><subject>Boundary layers</subject><subject>Forest fires</subject><subject>Heating</subject><subject>Solar radiation</subject><subject>Temperature changes</subject><subject>Temperature profiles</subject><subject>Urban atmospheric pollution</subject><issn>0001-4338</issn><issn>1555-628X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kcFKxDAQhoMouK4-gLfgQU_VJJOk6VEWVxcWPKjgraRN6nZpmzVJD_v2pq4nBZkZBub_EvhnELqk5JZS4HcvhBDKARSRKYgUR2hGhRCZZOr9GM0mOZv0U3QWwjYRjJN8hsxqaLrRDrXFrsEab9qPDdbWu-A6XLs0H6LXsXUDThk3dirf6w6H6Mc6jv774STo2LuwS2pb48qNg9F-jzu9t_4cnTS6C_bip8_R2_LhdfGUrZ8fV4v7dVYDiJgZVpkGOOc5MAqyMLqxjGglgCsDqhKVFgCEMCatSm4tlRqk4WC0UgwkzNHN4d-dd5-jDbHs21DbrtODdWMoC8KAM8pJIq__JRmhOaGFSODVL3DrRj8kF2UuKYgiB0gQPUB12lvwtil3vu2T_ZKScjpP-ec88AVm0IFt</recordid><startdate>20061201</startdate><enddate>20061201</enddate><creator>Khaikin, M N</creator><creator>Kuznetsova, IN</creator><creator>Kadygrov, EN</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M1Q</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7TV</scope><scope>C1K</scope></search><sort><creationdate>20061201</creationdate><title>Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer</title><author>Khaikin, M N ; Kuznetsova, IN ; Kadygrov, EN</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c335t-d2bdf34447321369dafe20a85348d38b5ba53300226e8014e16a36d43da882363</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Aerosol concentration</topic><topic>Aerosols</topic><topic>Air pollution</topic><topic>Atmosphere</topic><topic>Atmospheric boundary layer</topic><topic>Atmospheric pollution</topic><topic>Boundary layer structure</topic><topic>Boundary layers</topic><topic>Forest fires</topic><topic>Heating</topic><topic>Solar radiation</topic><topic>Temperature changes</topic><topic>Temperature profiles</topic><topic>Urban atmospheric pollution</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Khaikin, M N</creatorcontrib><creatorcontrib>Kuznetsova, IN</creatorcontrib><creatorcontrib>Kadygrov, EN</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Military Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Military Database</collection><collection>Science Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Pollution Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Khaikin, M N</au><au>Kuznetsova, IN</au><au>Kadygrov, EN</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer</atitle><jtitle>Izvestiya. Atmospheric and oceanic physics</jtitle><date>2006-12-01</date><risdate>2006</risdate><volume>42</volume><issue>6</issue><spage>715</spage><epage>721</epage><pages>715-721</pages><issn>0001-4338</issn><eissn>1555-628X</eissn><abstract>The influence of increased concentrations of submicron aerosol produced by forest fires on thermal characteristics of the atmospheric boundary layer (ABL) in Moscow and its remote vicinity (the town of Zvenigorod) are analyzed on the basis of regular remote measurements of the ABL temperature profile with the use of MTP-5 profilers. In the air basin of a large city, additional aerosol and accompanying pollutants in early morning hours (at small heights of the Sun) most frequently did not cause substantial changes in the ABL thermal structure. In the locality remote from the megalopolis (Zvenigorod), the atmospheric pollution by aerosol led to noticeable changes in the ABL thermal characteristics. Especially strong changes were observed in the daytime, during the maximum supply of solar radiation. In morning hours, the heating rate of the lower 100-m layer of the polluted air exceeded the heating rate of a relatively pure air by more than one degree. In higher layers, the differences between the rates of temperature changes in a relatively clean atmosphere and in an atmosphere polluted by aerosol (in the suburb) were insignificant.</abstract><cop>Washington</cop><pub>Springer Nature B.V</pub><doi>10.1134/S0001433806060065</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0001-4338 |
| ispartof | Izvestiya. Atmospheric and oceanic physics, 2006-12, Vol.42 (6), p.715-721 |
| issn | 0001-4338 1555-628X |
| language | eng |
| recordid | cdi_proquest_miscellaneous_902342140 |
| source | SpringerLink Journals |
| subjects | Aerosol concentration Aerosols Air pollution Atmosphere Atmospheric boundary layer Atmospheric pollution Boundary layer structure Boundary layers Forest fires Heating Solar radiation Temperature changes Temperature profiles Urban atmospheric pollution |
| title | Influence of a high aerosol concentration on the thermal structure of the atmospheric boundary layer |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-16T07%3A29%3A43IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Influence%20of%20a%20high%20aerosol%20concentration%20on%20the%20thermal%20structure%20of%20the%20atmospheric%20boundary%20layer&rft.jtitle=Izvestiya.%20Atmospheric%20and%20oceanic%20physics&rft.au=Khaikin,%20M%20N&rft.date=2006-12-01&rft.volume=42&rft.issue=6&rft.spage=715&rft.epage=721&rft.pages=715-721&rft.issn=0001-4338&rft.eissn=1555-628X&rft_id=info:doi/10.1134/S0001433806060065&rft_dat=%3Cproquest_cross%3E2177304841%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=761359733&rft_id=info:pmid/&rfr_iscdi=true |