Instituti Hidrometeorologjik i Kosov\u00ebs ka b\u00ebr\u00eb t\u00eb ditur se n\u00eb vend v\u00ebrshimet\/p\u00ebrmbytjet, po b\u00ebhen gjithnj\u00eb e m\u00eb t\u00eb shpeshta, si pasoj\u00eb e kushteve meteorologjike (intensitet i lart\u00eb i reshjeve p\u00ebr periudh\u00eb t\u00eb shkurt\u00eb kohore, shkrirja e shpejt\u00eb e bor\u00ebs), pastaj faktor\u00ebt gjeomorfologjik \u2013 relievi, pjesa m\u00eb e madhe e uj\u00ebrrjedhave, burimin e tyre ose formohen n\u00eb viset m\u00eb t\u00eb larta t\u00eb cilat rrjedhin rr\u00ebmbyeshum n\u00eb form\u00eb t\u00eb rr\u00ebkeve.<\/p>\n
Sipas nj\u00eb raporti t\u00eb IHMK-s\u00eb thuhet se vet\u00ebm disa lumenj, ose pjes\u00eb t\u00eb tyre si p.sh lumi Sitnica, Ibri, rrjedha e mesme dhe e poshtme e Drinit t\u00eb Bardh\u00eb, p\u00ebr shkak t\u00eb karakterit fushor\u00eb, p\u00ebrmbysin m\u00eb ngadal\u00eb, shkaku i sip\u00ebrfaqes, pozit\u00ebs, konfiguracionit t\u00eb terrenit.<\/p>\n
\u201cN\u00eb Kosov\u00eb brenda nj\u00eb periudhe 5 vje\u00e7are, kemi pasur paraqitje t\u00eb p\u00ebrmbytjeve me shkall\u00eb m\u00eb t\u00eb lart\u00eb gjat\u00eb vitit 2021, 2023 dhe tani nga 5 \u2013 8 janar 2026. K\u00ebto t\u00eb fundit, ishin n\u00eb p\u00ebrmasa me nj\u00eb periudh\u00eb kthyese hidrologjike prej 50 viteve (sidomos pjesa per\u00ebndimore apo pellgu i Drinit t\u00eb Bardh\u00eb). Si pasoj\u00eb e reshjeve t\u00eb shumta t\u00eb shiut e pastaj edhe t\u00eb shkrirjes s\u00eb bor\u00ebs (sidomos n\u00eb zonat m\u00eb t\u00eb lara malore), fillimisht n\u00eb pjes\u00ebn per\u00ebndimore (Rrafshi i Dukagjinit), qendrore (disa pjes\u00eb t\u00eb Rrafshit t\u00eb Kosov\u00ebs dhe Drenic\u00ebs), e m\u00eb pas edhe n\u00eb pjes\u00ebn m\u00eb t\u00eb madhe t\u00eb vendit, lumenjt\u00eb kryesor\u00eb t\u00eb Kosov\u00ebs, si Drini i Bardh\u00eb (kryesisht rrjedha e mesme dhe e poshtme), pastaj, Ereniku, Mirusha, Toplluha, Bistrica e De\u00e7anit, Lumi Klina, Sitnica, Drenica, Ibri etj me deg\u00ebt e tyre, duke filluar nga dat\u00eb 05-08\/01\/2026, kan\u00eb pasur ngritje t\u00eb shpejta dhe t\u00eb larta t\u00eb niveleve dhe prurjeve t\u00eb ujit\u201d.<\/p>\n
IHMK b\u00ebn t\u00eb ditur se nga 08\/01\/2026 e deri m\u00eb dat\u00eb 10\/01\/2026, mesatarisht n\u00eb territorin e s\u00eb Kosov\u00ebs kan\u00eb r\u00ebn\u00eb 41.3 mm (l\/m2) reshje, nd\u00ebrsa nga dat\u00eb: 01-10\/01\/2026, mesatarisht n\u00eb Kosov\u00eb kan\u00eb r\u00ebn\u00eb 124.1 mm, apo \u2264 64.9 mm ose 50.6% m\u00eb shum\u00eb se sasia mesatare e janarit 1961 \u2013 2024.<\/p>\n
Po ashtu, n\u00eb njoftim thuhet se sasia m\u00eb e lart\u00eb e reshjeve prej 400.4 mm (l\/m2), gjat\u00eb k\u00ebsaj periudha \u00ebsht\u00eb regjistruar n\u00eb Junik, pastaj n\u00eb Gllogjan 331.2 mm, Radoniq 280.8 mm, Kuqisht\u00eb 256.8 mm, Kramovik 245.5 mm, Gjakov\u00eb 217.3 mm, Restelic\u00eb 201.8 mm, Klin\u00eb 199 mm etj.<\/p>\n
Si\u00e7 v\u00ebrehet nga t\u00eb dh\u00ebnat, sasia m\u00eb e madhe e reshjeve \u00ebsht\u00eb regjistruar n\u00eb pjes\u00ebn per\u00ebndimore t\u00eb Kosov\u00ebs n\u00eb Pellgu i Drinit t\u00eb Bardh\u00eb 192.8 mm, ku si pasoj\u00eb jan\u00eb shkaktuar edhe v\u00ebrshimet\/p\u00ebrmbytjet m\u00eb t\u00eb m\u00ebdha.<\/p>\n
Pastaj, ato kan\u00eb qen\u00eb m\u00eb t\u00eb theksuara n\u00eb pellgun e Lepencit me mesatare 104.3 mm, me maksimumin e tyre prej 116.6 mm n\u00eb Ferizaj.<\/p>\n
Nd\u00ebrsa, n\u00eb pellgun e Ibrit, mesatarisht kan\u00eb r\u00ebn\u00eb 89 mm, me maksimumin e tyre prej 164.8 n\u00eb Komoran, pastaj n\u00eb Drenas 154.2 etj. (Si\u00e7 v\u00ebrehet nga t\u00eb dh\u00ebnat sidomos t\u00eb n\u00ebn pellgut t\u00eb Drenic\u00ebs, jan\u00eb regjistruar sasi m\u00eb t\u00eb larta t\u00eb reshjeve, prandaj jan\u00eb shkaktuar p\u00ebrmbytje, kryesisht n\u00eb rrjedh\u00ebn e tij t\u00eb mesme dhe t\u00eb poshtme).<\/p>\n
N\u00eb pellgun e Morav\u00ebs s\u00eb Bin\u00e7\u00ebs mesatarisht kan\u00eb r\u00ebn\u00eb 68.7mm, me maksimum n\u00eb V\u00ebrbic\u00eb t\u00eb Zhegocit ku jan\u00eb regjistruar 89.9 mm.<\/p>\n
Tutje n\u00eb njoftim thuhet se Instituti Hidrometeorologjik i Kosov\u00ebs (sektori i hidrologjis\u00eb), deri para situat\u00ebs me p\u00ebrmbytje, ka operuar me nj\u00eb num\u00ebr prej 34 stacionesh automatike Hidrometrike (GPRS), t\u00eb cilat jan\u00eb t\u00eb vendosura n\u00eb t\u00eb gjitha pellgjet, duke p\u00ebrfshi lumenjt\u00eb kryesor\u00eb si p.sh: N\u00eb pellgun e Drinit t\u00eb bardh\u00eb 12 stacione, Ibri 11, Morava e Bin\u00e7\u00ebs me 6, Lepenci 3 dhe lumi plav\u00ebs me 2 stacione hidrometrike.<\/p>\n
\u201cN\u00eb 7 profile hidrometrike jan\u00eb t\u00eb instaluara sisteme t\u00eb kamerave p\u00ebr fotogrametri, t\u00eb cilat i regjistrojn\u00eb k\u00ebta parametra: nivelin e ujit (h), shpejt\u00ebsin\u00eb e rrjedh\u00ebs (v) dhe prurjen (q). N\u00eb profilet tjera, jan\u00eb t\u00eb vendosur\/instaluar censor\u00ebt, t\u00eb cil\u00ebt e b\u00ebjn\u00eb regjistrimin e nivelit t\u00eb ujit n\u00eb intervale \u00e7do 15, 30 dhe 1h. T\u00eb dh\u00ebnat rruhen n\u00eb data Logerin e tyre t\u00eb cilat p\u00ebrmes sistemit GPRS, transferohen n\u00eb serverin qendror\u00eb t\u00eb IHMK-s n\u00eb Prishtin\u00eb. Aty b\u00ebhet, ruajtja, p\u00ebrpunimi, analizimi dhe pastaj publikimi i t\u00eb dh\u00ebnave pas nj\u00eb analize dhe kontrolli. Gjat\u00eb periudh\u00ebs 5\u201310 janar 2026, Republika e Kosov\u00ebs ka p\u00ebrjetuar reshje intensive t\u00eb shiut dhe shkrirje t\u00eb bor\u00ebs, \u00e7ka ka ndikuar ndjesh\u00ebm n\u00eb gjendjen dhe sjelljen e lumenjve kryesor\u00eb dhe ka shkaktuar p\u00ebrmbytje n\u00eb shum\u00eb zona. Situata hidrologjike p\u00ebr k\u00ebt\u00eb periudh\u00eb u monitorua Instituti Hidrometeorologjik i Kosov\u00ebs (IHMK)\u201d.<\/p>\n","protected":false},"excerpt":{"rendered":"
Instituti Hidrometeorologjik i Kosov\u00ebs ka b\u00ebr\u00eb t\u00eb ditur se n\u00eb vend v\u00ebrshimet\/p\u00ebrmbytjet, po b\u00ebhen gjithnj\u00eb e m\u00eb t\u00eb shpeshta, si pasoj\u00eb e kushteve meteorologjike (intensitet i lart\u00eb i reshjeve p\u00ebr periudh\u00eb t\u00eb shkurt\u00eb kohore, shkrirja e shpejt\u00eb e bor\u00ebs), pastaj faktor\u00ebt gjeomorfologjik \u2013 relievi, pjesa m\u00eb e madhe e uj\u00ebrrjedhave, burimin e tyre ose formohen […]<\/p>\n","protected":false},"author":1,"featured_media":225231,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[],"class_list":{"0":"post-226501","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-lajme"},"_links":{"self":[{"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/posts\/226501","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/comments?post=226501"}],"version-history":[{"count":1,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/posts\/226501\/revisions"}],"predecessor-version":[{"id":226502,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/posts\/226501\/revisions\/226502"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/media\/225231"}],"wp:attachment":[{"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/media?parent=226501"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/categories?post=226501"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/radiostargjilan.com\/web\/wp-json\/wp\/v2\/tags?post=226501"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}