{"id":1334,"date":"2019-08-09T10:24:42","date_gmt":"2019-08-09T06:24:42","guid":{"rendered":"http:\/\/journal.geonatres.az\/?p=1334"},"modified":"2019-08-09T10:36:38","modified_gmt":"2019-08-09T06:36:38","slug":"boyuk-qafqazin-c%c9%99nub-yamacinda-aqrometeoroloji-s%c9%99raitin-proqnozlasdirilmasi","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/boyuk-qafqazin-c%c9%99nub-yamacinda-aqrometeoroloji-s%c9%99raitin-proqnozlasdirilmasi\/","title":{"rendered":"FORECAST OF AGROMETEOROLOGICAL CONDITIONS ON THE SOUTHERN SLOPE OF THE GREATER CAUCASUS"},"content":{"rendered":"

M.K.Rahimov, R.S.Ismayilov <\/strong><\/p>\n

Abstract.\u00a0<\/strong>Agrometeorological conditions in the southern slope of the Greater Caucasus are predicted on the basis of long-term meteorological materials (1960-2010).\u00a0The predictive equations of heat supply and the duration of the growing season and their coefficient of correlation, as well as the curves of supply with sums of temperatures above 100<\/sup>C during the warm season are calculated.<\/p>\n

REFERENCES<\/strong><\/p>\n

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  1. H\u0259s\u0259nov M.S. Ki\u00e7ik Qafqazda pay\u0131zl\u0131q bu\u011fdan\u0131n m\u0259hsuldarl\u0131\u011f\u0131n\u0131n iqliml\u0259 \u0259laq\u0259si. Elm, Bak\u0131-1999, 128 s.<\/li>\n
  2. R\u0259himov M.K. G\u00f6zl\u0259nil\u0259n iqlim d\u0259yi\u015fm\u0259l\u0259rinin B.Qafqaz\u0131n c\u0259nub yamaclar\u0131n\u0131n aqroiqlim ehtiyatlar\u0131n\u0131n t\u0259sirinin qiym\u0259tl\u0259ndirilm\u0259si. C.\u00fc.f.d. dis.-n\u0131n avtorefe\u00adrat\u0131. Bak\u0131-2012, 22 s.<\/li>\n
  3. S\u0259f\u0259rov S.H., R\u0259himov M.K. Az\u0259rbaycanda m\u00fca\u00adsir aqroiqlim ehtiyatlar\u0131n\u0131n t\u0259dqiqinin b\u0259zi probleml\u0259ri. Hidrometeorologiya v\u0259 \u0259traf m\u00fchitin monitorinqi, 4. 2007, 66-73 s.<\/li>\n
  4. \u0410\u043d\u0438\u0441\u0438\u043c\u043e\u0432 \u041e.\u0410., \u0411\u0435\u043b\u043e\u043b\u0443\u0446\u043a\u0430\u044f \u041c.\u0410. \u041f\u0440\u0438\u043c\u0435\u043d\u0435\u043d\u0438\u0435 \u0433\u0435\u043e\u0438\u043d\u0444\u043e\u0440\u043c\u0430\u0446\u0438\u043e\u043d\u043d\u043e\u0439 \u0441\u0438\u0441\u0442\u0435\u043c\u044b \u0434\u043b\u044f \u043f\u0440\u043e\u0433\u043d\u043e\u0437\u0430 \u0430\u0433\u0440\u043e\u043a\u043b\u0438\u00ad\u043c\u0430\u0442\u0438\u0447\u0435\u0441\u043a\u0438\u0445 \u0445\u0430\u0440\u0430\u043a\u0442\u0435\u0440\u0438\u0441\u0442\u0438\u043a. \u041c\u0435\u0442\u0435\u043e\u0440\u043e\u043b\u043e\u0433\u0438\u044f \u0438 \u0433\u0438\u0434\u0440\u043e\u00ad\u043b\u043e\u0433\u0438\u044f, 2001, \u21169,\u0441.89-98.<\/li>\n
  5. \u0420\u0443\u043a\u043e\u0432\u043e\u0434\u0441\u0442\u0432\u043e \u043f\u043e \u0430\u0433\u0440\u043e\u043c\u0435\u0442\u0435\u043e\u0440\u043e\u043b\u043e\u0433\u0438\u0447\u0435\u0441\u043a\u0438\u043c \u043f\u0440\u043e\u0433\u00ad\u043d\u043e\u0437\u0430\u043c. \u0422\u043e\u043c 1. \u041b.: \u0413\u0438\u0434\u0440\u043e\u043c\u0435\u0442\u0435\u043e\u0438\u0437\u0434\u0430\u0442, 1984, 309\u0441.<\/li>\n<\/ol>\n

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    M.K.Rahimov, R.S.Ismayilov Abstract.\u00a0Agrometeorological conditions in the southern slope of the Greater Caucasus are predicted on the basis of long-term meteorological materials (1960-2010).\u00a0The predictive equations of heat supply and the duration of the growing season and their coefficient of correlation, as well as the curves of supply with sums of temperatures above 100C during the warm […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-1334","post","type-post","status-publish","format-standard","hentry","category-mqallr"],"blocksy_meta":[],"yoast_head":"\nFORECAST OF AGROMETEOROLOGICAL CONDITIONS ON THE SOUTHERN SLOPE OF THE GREATER CAUCASUS<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" 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