{"id":15296,"date":"2016-12-08T11:11:58","date_gmt":"2016-12-08T10:11:58","guid":{"rendered":"https:\/\/elspeedo.cz\/4-8-oblacnost\/"},"modified":"2016-12-09T23:02:58","modified_gmt":"2016-12-09T22:02:58","slug":"4-8-oblacnost","status":"publish","type":"post","link":"https:\/\/elspeedo.cz\/pl\/4-8-oblacnost\/","title":{"rendered":"4.8. Zachmurzenie"},"content":{"rendered":"
[vc_row][vc_column][vc_single_image image=”14786″ img_size=”full” alignment=”center” style=”vc_box_rounded”][vc_column_text]\n
\n
Rodzaje chmur<\/strong><\/div>\n
Chmury pi\u0119tra wysokiego<\/strong>
\nC – cirrus, Cc – cirocumulus, Cs – cirostratus.<\/strong> Chmury zbudowane s\u0105 z kryszta\u0142k\u00f3w lodu, bowiem si\u0119 znajduj\u0105 na wysoko\u015bciach na kt\u00f3rych temperatura jest g\u0142\u0119boko poni\u017cej zera.<\/div>\n<\/div>\n

Chmury pi\u0119tra \u015bredniego<\/strong>
\nAs – altostratus, Ac – altocumulus.<\/strong>Altostratusy zwyk\u0142e pojawiaj\u0105 si\u0119 w pobli\u017cu front\u00f3w atmosferycznych. Altocumulusy mog\u0105 mie\u0107 kszta\u0142t soczewkowy, ostrzegaj\u0105c tak przed mocnym wiatrem na wysoko\u015bci, ich kszta\u0142t mo\u017ce te\u017c ostrzega\u0107 przed silnym, porywistym wiatrem na mniejszych wysoko\u015bciach.<\/p>\n

Chmury pi\u0119tra niskiego<\/strong>
\nCu – cumulus<\/strong>Chmura budowy pionowej, kt\u00f3ra buduje si\u0119 dzieki kominom termicznym. Chmury te pokazuj\u0105, \u017ce termika \u201eruszy\u0142a\u201d.
\nSt \u2013 stratus,<\/strong>. Nisko le\u017c\u0105ca chmura, z kt\u00f3rej mo\u017ce padawa\u0107 m\u017cawka. St le\u017c\u0105cy swoj\u0105 podstaw\u0105 na powierzchni Ziemi nazywamy mg\u0142\u0105. Taki stratus mo\u017ce powsta\u0107 nad ranem z powodu nocnego och\u0142adzania si\u0119 powierzchni Ziemi i przez to ozi\u0119bienia powietrza przy jej powierzchni. Ow\u0105 chmur\u0119 nazywamy mg\u0142\u0105 radiacyjn\u0105.<\/p>\n

Chmury, si\u0119gaj\u0105ce wi\u0119cej pi\u0119ter
\nNs – nimbostratus<\/strong>Ciemna chmura deszczowa, znajduj\u0105ca si\u0119 zwyk\u0142e we frontach atmosferycznych.<\/p>\n

Cb \u2013 cumulonimbus<\/strong>Chmura burzowa, mocno rozbudowana pionowo. Powstaje ona w warunkach wyra\u017anej niestabilno\u015bci, tzn. r\u00f3wnowagi chwiejnej. Jej szczyt znajduje si\u0119 wysoko, nawet w stratosferze, w warunkach \u015brodkowoeuropejskich nawet na wysoko\u015bci oko\u0142o 15 km. Wyst\u0119puj\u0105ce opady s\u0105 bardzo intensywne, cz\u0119sto z gradem, lecz zwykle maj\u0105 charakter przelotny.<\/p>\n[\/vc_column_text][\/vc_column][\/vc_row][vc_row][vc_column css=”.vc_custom_1481191342295{padding-top: 40px !important;}”][vc_separator el_width=”80″ el_class=”basic-separator” css=”.vc_custom_1481191316039{padding-top: 40px !important;padding-bottom: 40px !important;}”][\/vc_column][vc_column width=”1\/2″][vc_single_image image=”14785″ img_size=”full” alignment=”center” style=”vc_box_rounded”][\/vc_column][vc_column width=”1\/2″][vc_column_text]Zachmurzenie w troposferze buduje si\u0119 przez kondensacj\u0119 pary wodnej.<\/strong><\/p>\n

Podstawow\u0105 przyczyn\u0105 powstania chmur jest osi\u0105gn\u0119cie stanu nasycenia powietrza par\u0105 wodn\u0105<\/strong>. Temperatur\u0119 powietrza w momencie osi\u0105gn\u0119cia stanu kondensacji nazywamy temperatur\u0105 punktu rosy<\/strong>.<\/p>\n

J\u0105dra kondensacyjne<\/strong><\/p>\n

s\u0105 niezb\u0119dne do kondensacji pary wodnej w powietrzu kt\u00f3re osi\u0105gne\u0142o stan nasycenia. S\u0105 to drobne cz\u0105steczki py\u0142u lub innego zanieczyszczenia powietrza, jak np. kurz, rozproszone w powietrzu. Najwi\u0119cej j\u0105der kondensacyjnych znajduje si\u0119 w powietrzu w okolicy du\u017cych aglomeracji miejskich lub przemys\u0142owych.[\/vc_column_text][\/vc_column][\/vc_row]\n<\/div>","protected":false},"excerpt":{"rendered":"

[vc_row][vc_column][vc_single_image image=”14786″ img_size=”full” alignment=”center” style=”vc_box_rounded”][vc_column_text] Rodzaje chmur Chmury pi\u0119tra wysokiego C – cirrus, Cc – cirocumulus, Cs – cirostratus. Chmury zbudowane s\u0105 z kryszta\u0142k\u00f3w lodu, bowiem si\u0119 znajduj\u0105 na wysoko\u015bciach na kt\u00f3rych temperatura jest g\u0142\u0119boko poni\u017cej zera. Chmury pi\u0119tra \u015bredniego As – altostratus, Ac – altocumulus.Altostratusy zwyk\u0142e pojawiaj\u0105 si\u0119 w pobli\u017cu front\u00f3w atmosferycznych. Altocumulusy mog\u0105 […]<\/p>\n","protected":false},"author":7,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_tribe_blocks_recurrence_rules":"","_tribe_blocks_recurrence_exclusions":"","_tribe_blocks_recurrence_description":"","footnotes":""},"categories":[329],"tags":[],"class_list":["post-15296","post","type-post","status-publish","format-standard","hentry","category-bez-kategorie-pl"],"yoast_head":"\n4.8. Zachmurzenie — El Speedo<\/title>\n<meta name=\"description\" content=\"El Speedo je nejv\u011bt\u0161\u00ed paraglidingov\u00e1 komunita a \u0161kola v \u010cR. 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