{"id":103,"date":"2020-04-23T10:33:28","date_gmt":"2020-04-23T10:33:28","guid":{"rendered":"http:\/\/localhost\/pelister\/?post_type=climates&#038;p=103"},"modified":"2020-09-09T06:19:12","modified_gmt":"2020-09-09T06:19:12","slug":"test-1","status":"publish","type":"climates","link":"https:\/\/park-pelister.com\/sq\/climates\/test-1\/","title":{"rendered":"Kushte klimatike dhe temperatura"},"content":{"rendered":"<p>Ndikimi i klim\u00ebs kontinentale dhe malore ndihet n\u00eb malin Baba, ku ndodhet Parku Komb\u00ebtar i Pelisterit. Ndikimi i klim\u00ebs malore \u00ebsht\u00eb rritur sepse \u00ebsht\u00eb nj\u00eb mal i lart\u00eb mbi 2000 m.<\/p>\n<p>Kushtet klimatike t\u00eb malit Baba ndikohen nga disa faktor\u00eb, si\u00e7 jan\u00eb gjer\u00ebsia, lart\u00ebsia, drejtimi i kreshtave malore, bim\u00ebt dhe t\u00eb ngjashme. Pjes\u00ebt per\u00ebndimore t\u00eb malit, ve\u00e7an\u00ebrisht ato n\u00eb lart\u00ebsi m\u00eb t\u00eb ul\u00ebta, jan\u00eb t\u00eb ndikuara fuqimisht nga pellgjet ujore t\u00eb Liqenit t\u00eb Ohrit dhe Liqenit t\u00eb Presp\u00ebs.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-413\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/67876317_10206141963505972_7364288253005922304_o-300x199.jpg\" alt=\"\" width=\"300\" height=\"199\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/67876317_10206141963505972_7364288253005922304_o-300x199.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/67876317_10206141963505972_7364288253005922304_o-768x509.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/67876317_10206141963505972_7364288253005922304_o.jpg 960w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/>\u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 \u00a0 <img loading=\"lazy\" class=\"alignnone size-medium wp-image-414\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/404-300x200.jpg\" alt=\"\" width=\"300\" height=\"200\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/404-300x200.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/404.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n<p><strong>Temperatura e ajrit<\/strong><\/p>\n<p>N\u00eb PK &#8220;Pelister&#8221;, nuk ka stacion mat\u00ebs p\u00ebr t\u00eb monitoruar temperaturat e ajrit. T\u00eb dh\u00ebnat nga stacioni mat\u00ebs n\u00eb Manastir u p\u00ebrdor\u00ebn n\u00eb analiza.<\/p>\n<p>Sipas t\u00eb dh\u00ebnave t\u00eb temperatura mesatare vjetore \u00ebsht\u00eb nga 11.2 \u00b0 C deri n\u00eb 11.9 \u00b0 C. Amplituda e temperatur\u00ebs p\u00ebr periudh\u00ebn 1951-1990 \u00ebsht\u00eb 22.3 \u00b0 C (-0.4 \u00b0 C deri 21.9 \u00b0 C), n\u00eb periudh\u00ebn 1991-2000 \u00ebsht\u00eb 23.5 \u00b0 (-1 \u00b0 C deri 22.5 \u00b0 C), dhe p\u00ebr periudh\u00ebn 2001-2010 \u00ebsht\u00eb 22.7 \u00b0 C (0.6 \u00b0 C deri 23.3 \u00b0 C). P\u00ebr t\u00eb p\u00ebrcaktuar temperatur\u00ebn mesatare sipas zonave, u p\u00ebrdor metoda isohypsy dhe metoda e korrelacionit. Vlerat e dh\u00ebna n\u00eb Tabel\u00ebn 11 jan\u00eb marr\u00eb nga llogaritjet.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-394\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_049-2-1-300x75.jpg\" alt=\"\" width=\"496\" height=\"124\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-2-1-300x75.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-2-1-1024x257.jpg 1024w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-2-1-768x193.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-2-1.jpg 1404w\" sizes=\"(max-width: 496px) 100vw, 496px\" \/><\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-393\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_049-1-2-300x152.jpg\" alt=\"\" width=\"490\" height=\"248\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-1-2-300x152.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-1-2-1024x520.jpg 1024w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-1-2-768x390.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_049-1-2.jpg 1404w\" sizes=\"(max-width: 490px) 100vw, 490px\" \/><\/p>\n<p>Tabela 10. Temperatura mesatare mujore dhe vjetore e llogaritur n\u00eb grad\u00eb Celsius p\u00ebr periudh\u00ebn 2001\/2010.<\/p>\n<p><strong>Zonat Tok\u00eb-Klim\u00eb- Vegjetacion<\/strong><\/p>\n<p>Parku Komb\u00ebtar Pelister shtrihet n\u00eb nj\u00eb lart\u00ebsi prej 880 &#8211; 2601 m. Sipas metodologjis\u00eb s\u00eb Filipovskit, Rizovskit dhe Risteskit, (1996) n\u00eb Parkun ka disa zona t\u00eb tok\u00ebs-klim\u00ebs-vegjetacionit:<\/p>\n<ul>\n<li>kontinentale e ftoht\u00eb (880-1100 m mbi nivelin e detit), mesatare 1010 m.<\/li>\n<li>kontinentale Podgorike (1100-1300 m mbi nivelin e detit), mesatare 1200 m mbi nivelin e detit;<\/li>\n<li>kontinentale malore por K eG (1300-1650 m. C.), Mesatarja 1475 m. mbi nivelin e detit<\/li>\n<li>subalpine malore (1650-2250 m. Asl.), Mesatarja 1950 t m. mbi nivelin e detit<\/li>\n<li>alpine malore (2250-2601 m asl), mesatarja 2425 m. mbi nivelin e detit<\/li>\n<\/ul>\n<p>N\u00eb zon\u00ebn subalpine, temperatura mesatare negative ndodh n\u00eb mars, dhe n\u00eb zon\u00ebn alpine, n\u00eb mars dhe n\u00ebntor.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-463\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_059-1-246x300.jpg\" alt=\"\" width=\"246\" height=\"300\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_059-1-246x300.jpg 246w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_059-1.jpg 595w\" sizes=\"(max-width: 246px) 100vw, 246px\" \/><\/p>\n<p><strong>Reshjet <\/strong><\/p>\n<p>Gjat\u00eb analiz\u00ebs s\u00eb reshjeve n\u00eb nj\u00eb periudh\u00eb m\u00eb t\u00eb gjat\u00eb, jan\u00eb marr\u00eb t\u00eb dh\u00ebna nga disa stacione. Bazuar n\u00eb t\u00eb dh\u00ebnat nga Tabela 12, u b\u00eb nj\u00eb marr\u00ebdh\u00ebnie matematikore midis reshjeve dhe lart\u00ebsis\u00eb.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-395\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_050-1-1-300x68.jpg\" alt=\"\" width=\"388\" height=\"88\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-1-1-300x68.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-1-1-1024x233.jpg 1024w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-1-1-768x175.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-1-1.jpg 1408w\" sizes=\"(max-width: 388px) 100vw, 388px\" \/><\/p>\n<p>Tabela 12. Reshjet mesatare n\u00eb disa mat\u00ebs shiu sipas muajve<\/p>\n<p>Kur p\u00ebrafrohen reshjet p\u00ebr zona t\u00eb ndryshme n\u00eb Malin Baba, vlerat e marra matematikisht mund t\u00eb merren si nj\u00eb lidhje me lart\u00ebsin\u00eb. N\u00eb k\u00ebt\u00eb m\u00ebnyr\u00eb, p\u00ebr zonat subalpine dhe alpine, reshjet p\u00ebrcaktohen n\u00eb baz\u00eb t\u00eb analogjis\u00eb me stacionet e reshjeve n\u00eb zona t\u00eb ngjashme n\u00eb vend (Tabela 13).<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-396\" src=\"http:\/\/pelister.development.ivote.mk\/wp-content\/uploads\/2020\/04\/1-150_Page_050-2-1-300x90.jpg\" alt=\"\" width=\"427\" height=\"128\" srcset=\"https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-2-1-300x90.jpg 300w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-2-1-1024x308.jpg 1024w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-2-1-768x231.jpg 768w, https:\/\/park-pelister.com\/wp-content\/uploads\/2020\/04\/1-150_Page_050-2-1.jpg 1356w\" sizes=\"(max-width: 427px) 100vw, 427px\" \/><\/p>\n<p>Megjith\u00ebse nuk ka t\u00eb dh\u00ebna mat\u00ebse, mesatarja maksimale e reshjeve vjetore t\u00eb pritshme n\u00eb k\u00ebt\u00eb zon\u00eb nuk duhet t\u00eb kaloj\u00eb 1200 tt, n\u00eb nj\u00eb lart\u00ebsi prej rreth 1650 m. n.v.<\/p>\n<p>\u00cbsht\u00eb p\u00ebrcaktuar nj\u00eb var\u00ebsi logaritmike midis lart\u00ebsis\u00eb dhe reshjeve me nj\u00eb koeficient p\u00ebrcaktues t\u00eb P2 = 0.996, q\u00eb do t\u00eb thot\u00eb se marr\u00ebdh\u00ebnia \u00ebsht\u00eb pothuajse funksionale. T\u00eb dh\u00ebna t\u00eb p\u00ebrshtatshme nga stacionet Manastir dhe Kazhani jan\u00eb p\u00ebrdorur p\u00ebr t\u00eb p\u00ebrcaktuar reshjet n\u00eb PK Pelister p\u00ebr periudh\u00ebn 1991 &#8211; 2000.<\/p>\n<p>Sipas t\u00eb dh\u00ebnave, reshjet mesatare n\u00eb k\u00ebt\u00eb dekad\u00eb n\u00eb stacionin Manastir (590 tt&gt; 607 tt) dhe n\u00eb stacionin Kazhani (805 tt&gt; 800 tt) jan\u00eb shum\u00eb af\u00ebr shiut mesatar p\u00ebr disa vite (1951-1990), me at\u00eb n\u00eb Manastir jan\u00eb m\u00eb t\u00eb vogla, dhe n\u00eb Kazhani me vlera m\u00eb t\u00eb larta. Ve\u00e7an\u00ebrisht vitet e thata jan\u00eb 1993 dhe 2000.<\/p>\n<p>1996 ve\u00e7ohet si nj\u00eb vit i lag\u00ebsht.<\/p>\n<p>Vitet jan\u00eb af\u00ebr vlerave mesatare.<\/p>","protected":false},"featured_media":531,"template":"","_links":{"self":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/climates\/103"}],"collection":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/climates"}],"about":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/types\/climates"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media\/531"}],"wp:attachment":[{"href":"https:\/\/park-pelister.com\/sq\/wp-json\/wp\/v2\/media?parent=103"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}