Assessment and forecast of the teleconnection between the Antarctic ozone and water vapor and the circulation and temperature of the lower thermosphere over the regions of Russia
The teleconnection between the Antarctic ozone anomaly (AOA) and the structure of semidiurnal tidal wind in the mid latitude and polar lower thermosphere (altitude interval between 80 and 110 km) of the Northern Hemisphere caused by the absorption of solar radiation by ozone and water vapor was foun...
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description | The teleconnection between the Antarctic ozone anomaly (AOA) and the structure of semidiurnal tidal wind in the mid latitude and polar lower thermosphere (altitude interval between 80 and 110 km) of the Northern Hemisphere caused by the absorption of solar radiation by ozone and water vapor was found and later explained in our previous works using the developed model of the atmospheric thermal tides (ATT). We clearly demonstrated in numerical experiments using the developed model that the semidiurnal tidal perturbations (TPs) (unlike diurnal ones) generated by the AOA propagate in the vertical and horizontal directions from the AOA and reach the mid latitude and polar lower thermosphere of the Northern Hemisphere in 710 days, where they strongly influence the formation of the spatiotemporal structure of the semidiurnal tidal wind in this region of the middle atmosphere. |
doi_str_mv | 10.1134/S1028334X10090126 |
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We clearly demonstrated in numerical experiments using the developed model that the semidiurnal tidal perturbations (TPs) (unlike diurnal ones) generated by the AOA propagate in the vertical and horizontal directions from the AOA and reach the mid latitude and polar lower thermosphere of the Northern Hemisphere in 710 days, where they strongly influence the formation of the spatiotemporal structure of the semidiurnal tidal wind in this region of the middle atmosphere.</description><identifier>ISSN: 1028-334X</identifier><identifier>EISSN: 1531-8354</identifier><identifier>DOI: 10.1134/S1028334X10090126</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Air pollution ; Atmospheric models ; Atmospheric sciences ; Diurnal variations ; Earth and Environmental Science ; Earth Sciences ; Geophysics ; Latitude ; Mathematical models ; Nuclear radiation ; Ozone ; Solar radiation ; Teleconnections ; Water vapor ; Wind</subject><ispartof>Doklady earth sciences, 2010-09, Vol.434 (1), p.1200-1204</ispartof><rights>Pleiades Publishing, Ltd. 2010</rights><rights>COPYRIGHT 2010 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c386t-d85ebcbf2fc61a1f965d4f756c0f7fb6f6af31a8163d7e689b605f21446f35663</citedby><cites>FETCH-LOGICAL-c386t-d85ebcbf2fc61a1f965d4f756c0f7fb6f6af31a8163d7e689b605f21446f35663</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1028334X10090126$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1028334X10090126$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Kapitsa, A. 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We clearly demonstrated in numerical experiments using the developed model that the semidiurnal tidal perturbations (TPs) (unlike diurnal ones) generated by the AOA propagate in the vertical and horizontal directions from the AOA and reach the mid latitude and polar lower thermosphere of the Northern Hemisphere in 710 days, where they strongly influence the formation of the spatiotemporal structure of the semidiurnal tidal wind in this region of the middle atmosphere.</description><subject>Air pollution</subject><subject>Atmospheric models</subject><subject>Atmospheric sciences</subject><subject>Diurnal variations</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geophysics</subject><subject>Latitude</subject><subject>Mathematical models</subject><subject>Nuclear radiation</subject><subject>Ozone</subject><subject>Solar radiation</subject><subject>Teleconnections</subject><subject>Water vapor</subject><subject>Wind</subject><issn>1028-334X</issn><issn>1531-8354</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kV2L1TAQhosouK7-AO-CN151TZqPtpeHxS9YEPwA70qaTo5d2qRm0j3oz_IXOqdVBEVyMZN33mcyZIriqeBXQkj14oPgVSOl-iw4b7mozL3iQmgpykZqdZ9yKpfn-sPiEeIt50op3V4UPw6IgDhDyMyGgfmYwFnMLHqWvwDLMIGLIYDLYwysh3wCCFvpELJNJDsWv8cAG36yGRK7s0tM2_3sc2Ny62Q3ftNgXiDZvCb4_coUT4RRluaICwWq3O0KS3AkEs_W9yviaB8XD7ydEJ78ipfFp1cvP16_KW_evX57fbgpnWxMLodGQ-96X3lnhBW-NXpQvtbGcV_73nhjvRS2EUYONZim7Q3XvhJKGS-1MfKyeL73XVL8ugLmbh7RwTTZAHHFrhFay9pwTs5nfzlv45oCDdfVWremom5kutpNRztBNwYfc7KOzgDzSF8MfiT9IA2vuKplS4DYAZciYgLfLWmcbfrWCd6dl979s3Riqp1B8oYjpD-T_B_6CftgsiM</recordid><startdate>20100901</startdate><enddate>20100901</enddate><creator>Kapitsa, A. 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We clearly demonstrated in numerical experiments using the developed model that the semidiurnal tidal perturbations (TPs) (unlike diurnal ones) generated by the AOA propagate in the vertical and horizontal directions from the AOA and reach the mid latitude and polar lower thermosphere of the Northern Hemisphere in 710 days, where they strongly influence the formation of the spatiotemporal structure of the semidiurnal tidal wind in this region of the middle atmosphere.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1028334X10090126</doi><tpages>5</tpages></addata></record> |
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subjects | Air pollution Atmospheric models Atmospheric sciences Diurnal variations Earth and Environmental Science Earth Sciences Geophysics Latitude Mathematical models Nuclear radiation Ozone Solar radiation Teleconnections Water vapor Wind |
title | Assessment and forecast of the teleconnection between the Antarctic ozone and water vapor and the circulation and temperature of the lower thermosphere over the regions of Russia |
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