{"id":2157,"date":"2015-02-02T09:32:44","date_gmt":"2015-02-02T07:32:44","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2157"},"modified":"2016-06-07T11:45:31","modified_gmt":"2016-06-07T09:45:31","slug":"2157-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2157-2\/","title":{"rendered":"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76"},"content":{"rendered":"

Geoinformatika 2014; 3(51) : 67-76\u00a0 (in Russian)<\/p>\n

THE WIND FIELD STRUCTURE ABOVE THE WORLD OCEAN<\/strong><\/h4>\n
V.N. Eremeev<\/em>1<\/sup><\/em>, A.E. Bukatov<\/em>2<\/sup><\/em>, M.V. Babiy<\/em>2<\/sup><\/em>, A.A. Bukatov<\/em>2<\/sup><\/em><\/h5>\n

1<\/sup><\/em>Oceanological Center NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine
\n<\/em>2<\/sup><\/em>Marine Hydrophysical Institute NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine<\/em><\/p>\n

On the basis of the monthly average values of wind velocity components of the above-ground level an investigation of the intraannual variability of the wind climatic field structure above the World Ocean is carried out during 1948\u20132012. The intraannual motion of the centers location of the major cyclones and anticyclones is considered. The analysis of the wind field climatic maps shows that the centers location of the basic cyclones and anticyclones practically does not change. The probability of the second centers appearing\u00a0 into vortical structures and additional vortical formations occurring away from the main vortex is estimated. The analysis of the trend regional distribution of the above-ground level wind velocity is carried out. Areas of positive and negative trends are shown and estimations of their values are obtained. The correlation estimation of zonal and meridional wind velocity components of the above-ground level is given. In the regional distribution fields of a correlation coefficient and the hypothesis of no correlation, the areas of a positive and negative correlation coefficient and the areas with a high probability of no correlation between wind climatic velocity components are noted.<\/p>\n

Keywords:<\/strong> wind above-ground level, wind field structure, the vortical structures centers, wind velocity trend.<\/p>\n

\"pdf\"<\/a>
\n<\/strong><\/em><\/p>\n

References:<\/strong><\/a><\/p>\n

\n
    \n
  1. Garvej Dzh. Atmosfera i okean<\/em> [Atmosphere and ocean]. Moscow. Progres,<\/em> 1982, 184 p.<\/li>\n
  2. Eremeev V.N., Bukatov A.E., Babij M.V., Bukatov A.A. Projavlenie fazy Jel\u2019-Nin\u2019o – Juzhnoe kolebanie v geograficheskom polozhenii vnutritropicheskoj zony konvergencii<\/em> [The El Nino – Southern oscillation phase response in the geographical location of the convergence zone]. Dopovidi NAN Ukraini<\/em> [Reports of the National Academy of Sciences of Ukraine (Ukraine)], 2011, no. 10, pp. 93-98.<\/li>\n
  3. Martazinova V.F., Timofeev V.\u0415. Sovremennoe sostojanie atmosfernoj cirkuljacii vozduha v Severnom i Juzhnom polusharii i regional\u2019nye klimaticheskie osobennosti v atlantiko-evropejskom sektore i rajone Antarkticheskogo poluostrova<\/em> [\u0421urrent state of atmospheric circulation in the Northern and Southern hemispheres and regional climate in the Atlantic-European sector and the region of the Antarctic peninsula]. Problemy Arktiki i Antarktiki<\/em> [Problems of Arctic and Antarctic (Russia)], 2008, no. 3(80), pp. 17-37.<\/li>\n
  4. Mokhov I.I., Hon V.Ch. Mezhgodovaja izmenchivost\u2019 i dolgoperiodnye tendencii izmenenij centrov dejstvija atmosfery v Severnom polusharii: analiz dannyh nabljudenij<\/em> [Interannual variability and long-term tendencies of change in atmospheric centers of action in the Northern hemisphere: analyses of observational data] Izvestija RAN. Fizika Atmosfery i Okeana<\/em> [Izvestiya, Atmospheric and Oceanic Physics (Russia)], 2005, vol. 41, no. 6, pp. 723-732.<\/li>\n
  5. Smirnov N.P., Saruhanyan E.I., Rozanova I.V. Ciklonicheskie centry dejstvija atmosfery Juzhnogo polusharija i izmenenija klimata<\/em> [Cyclonic action centres in the atmosphere of the Southern Hemisphere and climatic variations]. St. Peterburg. RSHU Publishers<\/em>, 2004, 209 pp.<\/li>\n
  6. Sorkina A.I. Utochnennye dannye ob intensivnosti i polozhenijah centrov dejstvija atmosfery v Severnom polusharii<\/em> [The specified data about intensity and positions of atmosphere centers of action in Northern hemisphere]. Voprosy gidrologii i meteorologii okeanov. Trudy Gosudarstvennogo Ocean. Inst.<\/em> Leningrad. Gidrometeoizdat<\/em>, 1972, vol. 114, pp. 71-79.<\/li>\n
  7. Sorkina A.I. Tipy atmosfernoj cirkuljacii i svjazannyh s nej vetrovyh polej nad Severnoj chast\u2019ju Tihogo okeana<\/em> [Types of atmospheric circulation and connected with it the wind fields over Northern part of Pacific ocean]. Moscow. Gidrometeoizdat <\/em>(branch), 1963, 248 p.<\/li>\n
  8. http:\/\/www.esrl.noaa.gov.<\/li>\n<\/ol>\n<\/div>\n

    \u00a0<\/strong><\/p>","protected":false},"excerpt":{"rendered":"

    Geoinformatika 2014; 3(51) : 67-76\u00a0 (in Russian) THE WIND FIELD STRUCTURE ABOVE THE WORLD OCEAN V.N. Eremeev1, A.E. Bukatov2, M.V. Babiy2, A.A. Bukatov2 1Oceanological Center NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine 2Marine Hydrophysical Institute NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine On the basis of the monthly average values of wind velocity components of the above-ground level an investigation of the intraannual variability of the wind climatic field structure above the World Ocean is carried out during 1948\u20132012. The intraannual motion of the centers location of the major cyclones and anticyclones is considered. The analysis of the wind field climatic maps shows that the centers location of the basic cyclones and anticyclones practically does not change. The probability of the second centers appearing\u00a0 into vortical structures and additional vortical formations occurring away from the main vortex is estimated. The analysis of the trend regional distribution of the above-ground level wind velocity is carried out. Areas of positive and negative trends are shown and estimations of their values are obtained. The correlation estimation of zonal and meridional wind velocity components of the above-ground level is given. In the regional distribution fields of a correlation coefficient and the hypothesis of no correlation, the areas of a positive and negative correlation coefficient and the areas with a high probability of no correlation between wind climatic velocity components are noted. Keywords: wind above-ground level, wind field structure, the vortical structures centers, wind velocity trend. References: Garvej Dzh. Atmosfera i okean [Atmosphere and ocean]. Moscow. Progres, 1982, 184 p. Eremeev V.N., Bukatov A.E., Babij M.V., Bukatov A.A. Projavlenie fazy Jel\u2019-Nin\u2019o – Juzhnoe kolebanie v geograficheskom polozhenii vnutritropicheskoj zony konvergencii [The El Nino – Southern oscillation phase response in the geographical location of the convergence zone]. Dopovidi NAN Ukraini [Reports of the National Academy of Sciences of Ukraine (Ukraine)], 2011, no. 10, pp. 93-98. Martazinova V.F., Timofeev V.\u0415. Sovremennoe sostojanie atmosfernoj cirkuljacii vozduha v Severnom i Juzhnom polusharii i regional\u2019nye klimaticheskie osobennosti v atlantiko-evropejskom sektore i rajone Antarkticheskogo poluostrova [\u0421urrent state of atmospheric circulation in the Northern and Southern hemispheres and regional climate in the Atlantic-European sector and the region of the Antarctic peninsula]. Problemy Arktiki i Antarktiki [Problems of Arctic and Antarctic (Russia)], 2008, no. 3(80), pp. 17-37. Mokhov I.I., Hon V.Ch. Mezhgodovaja izmenchivost\u2019 i dolgoperiodnye tendencii izmenenij centrov dejstvija atmosfery v Severnom polusharii: analiz dannyh nabljudenij [Interannual variability and long-term tendencies of change in atmospheric centers of action in the Northern hemisphere: analyses of observational data] Izvestija RAN. Fizika Atmosfery i Okeana [Izvestiya, Atmospheric and Oceanic Physics (Russia)], 2005, vol. 41, no. 6, pp. 723-732. Smirnov N.P., Saruhanyan E.I., Rozanova I.V. Ciklonicheskie centry dejstvija atmosfery Juzhnogo polusharija i izmenenija klimata [Cyclonic action centres in the atmosphere of the Southern Hemisphere and climatic variations]. St. Peterburg. RSHU Publishers, 2004, 209 pp. Sorkina A.I. Utochnennye dannye ob intensivnosti i polozhenijah centrov dejstvija atmosfery v Severnom polusharii [The specified data about intensity and positions of atmosphere centers of action in Northern hemisphere]. Voprosy gidrologii i meteorologii okeanov. Trudy Gosudarstvennogo Ocean. Inst. Leningrad. Gidrometeoizdat, 1972, vol. 114, pp. 71-79. Sorkina A.I. Tipy atmosfernoj cirkuljacii i svjazannyh s nej vetrovyh polej nad Severnoj chast\u2019ju Tihogo okeana [Types of atmospheric circulation and connected with it the wind fields over Northern part of Pacific ocean]. Moscow. Gidrometeoizdat (branch), 1963, 248 p. http:\/\/www.esrl.noaa.gov. \u00a0<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-2157","page","type-page","status-publish","hentry"],"yoast_head":"\n(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"http:\/\/www.geology.com.ua\/en\/2157-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"og:description\" content=\"Geoinformatika 2014; 3(51) : 67-76\u00a0 (in Russian) THE WIND FIELD STRUCTURE ABOVE THE WORLD OCEAN V.N. Eremeev1, A.E. Bukatov2, M.V. Babiy2, A.A. Bukatov2 1Oceanological Center NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine 2Marine Hydrophysical Institute NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine On the basis of the monthly average values of wind velocity components of the above-ground level an investigation of the intraannual variability of the wind climatic field structure above the World Ocean is carried out during 1948\u20132012. The intraannual motion of the centers location of the major cyclones and anticyclones is considered. The analysis of the wind field climatic maps shows that the centers location of the basic cyclones and anticyclones practically does not change. The probability of the second centers appearing\u00a0 into vortical structures and additional vortical formations occurring away from the main vortex is estimated. The analysis of the trend regional distribution of the above-ground level wind velocity is carried out. Areas of positive and negative trends are shown and estimations of their values are obtained. The correlation estimation of zonal and meridional wind velocity components of the above-ground level is given. In the regional distribution fields of a correlation coefficient and the hypothesis of no correlation, the areas of a positive and negative correlation coefficient and the areas with a high probability of no correlation between wind climatic velocity components are noted. Keywords: wind above-ground level, wind field structure, the vortical structures centers, wind velocity trend. References: Garvej Dzh. Atmosfera i okean [Atmosphere and ocean]. Moscow. Progres, 1982, 184 p. Eremeev V.N., Bukatov A.E., Babij M.V., Bukatov A.A. Projavlenie fazy Jel\u2019-Nin\u2019o – Juzhnoe kolebanie v geograficheskom polozhenii vnutritropicheskoj zony konvergencii [The El Nino – Southern oscillation phase response in the geographical location of the convergence zone]. Dopovidi NAN Ukraini [Reports of the National Academy of Sciences of Ukraine (Ukraine)], 2011, no. 10, pp. 93-98. Martazinova V.F., Timofeev V.\u0415. Sovremennoe sostojanie atmosfernoj cirkuljacii vozduha v Severnom i Juzhnom polusharii i regional\u2019nye klimaticheskie osobennosti v atlantiko-evropejskom sektore i rajone Antarkticheskogo poluostrova [\u0421urrent state of atmospheric circulation in the Northern and Southern hemispheres and regional climate in the Atlantic-European sector and the region of the Antarctic peninsula]. Problemy Arktiki i Antarktiki [Problems of Arctic and Antarctic (Russia)], 2008, no. 3(80), pp. 17-37. Mokhov I.I., Hon V.Ch. Mezhgodovaja izmenchivost\u2019 i dolgoperiodnye tendencii izmenenij centrov dejstvija atmosfery v Severnom polusharii: analiz dannyh nabljudenij [Interannual variability and long-term tendencies of change in atmospheric centers of action in the Northern hemisphere: analyses of observational data] Izvestija RAN. Fizika Atmosfery i Okeana [Izvestiya, Atmospheric and Oceanic Physics (Russia)], 2005, vol. 41, no. 6, pp. 723-732. Smirnov N.P., Saruhanyan E.I., Rozanova I.V. Ciklonicheskie centry dejstvija atmosfery Juzhnogo polusharija i izmenenija klimata [Cyclonic action centres in the atmosphere of the Southern Hemisphere and climatic variations]. St. Peterburg. RSHU Publishers, 2004, 209 pp. Sorkina A.I. Utochnennye dannye ob intensivnosti i polozhenijah centrov dejstvija atmosfery v Severnom polusharii [The specified data about intensity and positions of atmosphere centers of action in Northern hemisphere]. Voprosy gidrologii i meteorologii okeanov. Trudy Gosudarstvennogo Ocean. Inst. Leningrad. Gidrometeoizdat, 1972, vol. 114, pp. 71-79. Sorkina A.I. Tipy atmosfernoj cirkuljacii i svjazannyh s nej vetrovyh polej nad Severnoj chast\u2019ju Tihogo okeana [Types of atmospheric circulation and connected with it the wind fields over Northern part of Pacific ocean]. Moscow. Gidrometeoizdat (branch), 1963, 248 p. http:\/\/www.esrl.noaa.gov. \u00a0\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2157-2\/\" \/>\n<meta property=\"og:site_name\" content=\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"article:modified_time\" content=\"2016-06-07T09:45:31+00:00\" \/>\n<meta property=\"og:image\" content=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"3 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/\",\"name\":\"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-02-02T07:32:44+00:00\",\"dateModified\":\"2016-06-07T09:45:31+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/#primaryimage\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"contentUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2157-2\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76\"}]},{\"@type\":\"WebSite\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\",\"name\":\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"description\":\"\u0426\u0435\u043d\u0442\u0440 \u043c\u0435\u043d\u0435\u0434\u0436\u043c\u0435\u043d\u0442\u0443 \u0442\u0430 \u043c\u0430\u0440\u043a\u0435\u0442\u0438\u043d\u0433\u0443 \u0432 \u0433\u0430\u043b\u0443\u0437\u0456 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"http:\/\/www.geology.com.ua\/en\/2157-2\/","og_locale":"en_US","og_type":"article","og_title":"(\u0423\u043a\u0440\u0430\u0457\u043d\u0441\u044c\u043a\u0430) Geoinformatika 2014; 3(51) : 67-76 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","og_description":"Geoinformatika 2014; 3(51) : 67-76\u00a0 (in Russian) THE WIND FIELD STRUCTURE ABOVE THE WORLD OCEAN V.N. Eremeev1, A.E. Bukatov2, M.V. Babiy2, A.A. Bukatov2 1Oceanological Center NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine 2Marine Hydrophysical Institute NASU, Kapitanskaya St., 2, Sevastopol 99011, Ukraine On the basis of the monthly average values of wind velocity components of the above-ground level an investigation of the intraannual variability of the wind climatic field structure above the World Ocean is carried out during 1948\u20132012. The intraannual motion of the centers location of the major cyclones and anticyclones is considered. The analysis of the wind field climatic maps shows that the centers location of the basic cyclones and anticyclones practically does not change. The probability of the second centers appearing\u00a0 into vortical structures and additional vortical formations occurring away from the main vortex is estimated. The analysis of the trend regional distribution of the above-ground level wind velocity is carried out. Areas of positive and negative trends are shown and estimations of their values are obtained. The correlation estimation of zonal and meridional wind velocity components of the above-ground level is given. In the regional distribution fields of a correlation coefficient and the hypothesis of no correlation, the areas of a positive and negative correlation coefficient and the areas with a high probability of no correlation between wind climatic velocity components are noted. Keywords: wind above-ground level, wind field structure, the vortical structures centers, wind velocity trend. References: Garvej Dzh. Atmosfera i okean [Atmosphere and ocean]. Moscow. Progres, 1982, 184 p. Eremeev V.N., Bukatov A.E., Babij M.V., Bukatov A.A. Projavlenie fazy Jel\u2019-Nin\u2019o – Juzhnoe kolebanie v geograficheskom polozhenii vnutritropicheskoj zony konvergencii [The El Nino – Southern oscillation phase response in the geographical location of the convergence zone]. Dopovidi NAN Ukraini [Reports of the National Academy of Sciences of Ukraine (Ukraine)], 2011, no. 10, pp. 93-98. Martazinova V.F., Timofeev V.\u0415. Sovremennoe sostojanie atmosfernoj cirkuljacii vozduha v Severnom i Juzhnom polusharii i regional\u2019nye klimaticheskie osobennosti v atlantiko-evropejskom sektore i rajone Antarkticheskogo poluostrova [\u0421urrent state of atmospheric circulation in the Northern and Southern hemispheres and regional climate in the Atlantic-European sector and the region of the Antarctic peninsula]. Problemy Arktiki i Antarktiki [Problems of Arctic and Antarctic (Russia)], 2008, no. 3(80), pp. 17-37. Mokhov I.I., Hon V.Ch. Mezhgodovaja izmenchivost\u2019 i dolgoperiodnye tendencii izmenenij centrov dejstvija atmosfery v Severnom polusharii: analiz dannyh nabljudenij [Interannual variability and long-term tendencies of change in atmospheric centers of action in the Northern hemisphere: analyses of observational data] Izvestija RAN. Fizika Atmosfery i Okeana [Izvestiya, Atmospheric and Oceanic Physics (Russia)], 2005, vol. 41, no. 6, pp. 723-732. Smirnov N.P., Saruhanyan E.I., Rozanova I.V. Ciklonicheskie centry dejstvija atmosfery Juzhnogo polusharija i izmenenija klimata [Cyclonic action centres in the atmosphere of the Southern Hemisphere and climatic variations]. St. Peterburg. RSHU Publishers, 2004, 209 pp. Sorkina A.I. Utochnennye dannye ob intensivnosti i polozhenijah centrov dejstvija atmosfery v Severnom polusharii [The specified data about intensity and positions of atmosphere centers of action in Northern hemisphere]. Voprosy gidrologii i meteorologii okeanov. Trudy Gosudarstvennogo Ocean. Inst. Leningrad. Gidrometeoizdat, 1972, vol. 114, pp. 71-79. Sorkina A.I. Tipy atmosfernoj cirkuljacii i svjazannyh s nej vetrovyh polej nad Severnoj chast\u2019ju Tihogo okeana [Types of atmospheric circulation and connected with it the wind fields over Northern part of Pacific ocean]. Moscow. 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