{"id":3103,"date":"2015-03-23T12:51:38","date_gmt":"2015-03-23T10:51:38","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3103"},"modified":"2015-03-23T12:51:38","modified_gmt":"2015-03-23T10:51:38","slug":"2014-452-54-60","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2014-452-54-60\/","title":{"rendered":"2014; 4(52) : 54-60"},"content":{"rendered":"<p>Geoinformatika 2014; 4(52) :\u00a054-60<\/p>\n<h4>DYNAMICS OF THE AZOV SEA IN ICE CONDITIONS<\/h4>\n<h5><em>Bukatov A.E., Zav&#8217;yalov D.D., Solomakha T.A.<\/em><\/h5>\n<p style=\"text-align: justify;\">On the basis of constructed two-dimensional mathematical model the evolution of fields of drift speed, thickness, mass and area of ice in the Azov Sea is considered. The estimation is made to the influence of hydrometeorological factors on spatio-temporal distribution of ice cover characteristics.<\/p>\n<p><strong>Keywords:<\/strong> ice cover dynamic, ice drift.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/07_Bukatov.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-790 alignleft\" src=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" alt=\"pdf\" width=\"48\" height=\"48\" srcset=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg 128w, http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf-150x150.jpg 150w\" sizes=\"auto, (max-width: 48px) 100vw, 48px\" \/><\/a><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2014; 4(52) :\u00a054-60 DYNAMICS OF THE AZOV SEA IN ICE CONDITIONS Bukatov A.E., Zav&#8217;yalov D.D., Solomakha T.A. On the basis of constructed two-dimensional mathematical model the evolution of fields of drift speed, thickness, mass and area of ice in the Azov Sea is considered. The estimation is made to the influence of hydrometeorological factors on spatio-temporal distribution of ice cover characteristics. Keywords: ice cover dynamic, ice drift.<\/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-3103","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2014; 4(52) : 54-60 - \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\/2014-452-54-60\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2014; 4(52) : 54-60 - \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; 4(52) :\u00a054-60 DYNAMICS OF THE AZOV SEA IN ICE CONDITIONS Bukatov A.E., Zav&#8217;yalov D.D., Solomakha T.A. On the basis of constructed two-dimensional mathematical model the evolution of fields of drift speed, thickness, mass and area of ice in the Azov Sea is considered. The estimation is made to the influence of hydrometeorological factors on spatio-temporal distribution of ice cover characteristics. 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On the basis of constructed two-dimensional mathematical model the evolution of fields of drift speed, thickness, mass and area of ice in the Azov Sea is considered. The estimation is made to the influence of hydrometeorological factors on spatio-temporal distribution of ice cover characteristics. 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