[{"@context":"https:\/\/schema.org\/","@type":"Article","@id":"https:\/\/www.archall.cz\/pocasi-nebo-klima\/#Article","mainEntityOfPage":"https:\/\/www.archall.cz\/pocasi-nebo-klima\/","headline":"Po\u010das\u00ed nebo klima?","name":"Po\u010das\u00ed nebo klima?","description":"Atmosf\u00e9ra, n\u00e1\u0161 plynn\u00fd obal Zem\u011b, je v\u00e1z\u00e1na gravitac\u00ed a chr\u00e1n\u00ed \u017eivot p\u0159ed slune\u010dn\u00ed radiac\u00ed. Skl\u00e1d\u00e1 se z dus\u00edku, kter\u00fd se vyskytuje a\u017e v 78 %. Pot\u00e9 to je kysl\u00edk 21% a ostatn\u00ed plyny jako CO2 nebo helium \u010di argon. Jedna z hlavn\u00edch funkc\u00ed atmosf\u00e9ry je zabra\u0148ov\u00e1n\u00ed pronik\u00e1n\u00ed UV … ","datePublished":"2019-11-03","dateModified":"2023-05-15","author":{"@type":"Person","@id":"https:\/\/www.archall.cz\/author\/#Person","name":"","url":"https:\/\/www.archall.cz\/author\/","identifier":1,"image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/0dc285cbe86eecc8073f119fcb2e2c7032b51533f5bb47611c7d4a598558b8b7?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/0dc285cbe86eecc8073f119fcb2e2c7032b51533f5bb47611c7d4a598558b8b7?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"archall.cz","logo":{"@type":"ImageObject","@id":"\/logo.png","url":"\/logo.png","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/www.archall.cz\/wp-content\/uploads\/img_a359222_w3916_t1573313134.jpg","url":"https:\/\/www.archall.cz\/wp-content\/uploads\/img_a359222_w3916_t1573313134.jpg","height":0,"width":0},"url":"https:\/\/www.archall.cz\/pocasi-nebo-klima\/","about":["V\u011bda"],"wordCount":531,"articleBody":"Atmosf\u00e9ra, n\u00e1\u0161 plynn\u00fd obal Zem\u011b, je v\u00e1z\u00e1na gravitac\u00ed a chr\u00e1n\u00ed \u017eivot p\u0159ed slune\u010dn\u00ed radiac\u00ed.Skl\u00e1d\u00e1 se z dus\u00edku, kter\u00fd se vyskytuje a\u017e v 78 %. Pot\u00e9 to je kysl\u00edk 21% a ostatn\u00ed plyny jako CO2 nebo helium \u010di argon.Jedna z hlavn\u00edch funkc\u00ed atmosf\u00e9ry je zabra\u0148ov\u00e1n\u00ed pronik\u00e1n\u00ed UV z\u00e1\u0159en\u00ed. Pom\u00e1h\u00e1 planet\u011b udr\u017eet teplotu a neochladit se a nakonec rostlin\u00e1m vytv\u00e1\u0159et fotosynt\u00e9zu. Ovzdu\u0161\u00ed se skl\u00e1d\u00e1 z p\u011bti vrstev:a)      V troposf\u00e9\u0159e se tvo\u0159\u00ed po\u010das\u00ed a teplota kles\u00e1 s nadmo\u0159skou v\u00fd\u0161kou.b)      Stratosf\u00e9ra – ozonosf\u00e9ra- d\u00edky n\u00ed pronik\u00e1 na zemsk\u00fd povrch mal\u00e9 % UV z\u00e1\u0159en\u00ed dopadaj\u00edc\u00edho na hranici atmosf\u00e9ryc)      Mezosf\u00e9ra sah\u00e1 do v\u00fd\u0161ky 80 – 85 kilometr\u016f a obsahuje oz\u00f3n, kter\u00fd zabra\u0148uje pronik\u00e1n\u00ed \u0161kodliv\u00e9ho z\u00e1\u0159en\u00ed na povrch.d)      Termosf\u00e9ra – ionosf\u00e9ru. Ta obsahuje elektricky nabit\u00e9 \u010d\u00e1stice a odr\u00e1\u017e\u00ed r\u00e1diov\u00e9 vlny.e)      Posledn\u00ed – exosf\u00e9ra – p\u0159ech\u00e1z\u00ed do meziplanet\u00e1rn\u00edho prostoru. Sklen\u00edkov\u00fd efekt je proces, p\u0159i kter\u00e9m se funkce atmosf\u00e9ry sni\u017euje. Planeta se oh\u0159\u00edv\u00e1 t\u00edm, \u017ee absorbuje dopadaj\u00edc\u00ed paprsky na povrch a br\u00e1n\u00ed zp\u011btn\u00e9mu vr\u00e1cen\u00ed. D\u00edky nadm\u011brn\u00e9 pot\u0159eb\u011b slu\u017eeb jako jsou letadla, tov\u00e1rny a dokonce i chov krav, zvy\u0161ujeme riziko vzniku oz\u00f3nov\u00fdch d\u011br, kter\u00e9 propou\u0161t\u011bj\u00ed v\u011bt\u0161\u00ed % nebezpe\u010dn\u00e9ho z\u00e1\u0159en\u00ed. Ale konec s hrozbami. Velk\u00fd probl\u00e9m d\u011bl\u00e1 lidem vysv\u011btlit pojem po\u010das\u00ed a klima.Po\u010das\u00ed je okam\u017eit\u00fd stav atmosf\u00e9ry na ur\u010dit\u00e9m m\u00edst\u011b a ur\u010duje se um\u011bl\u00fdmi dru\u017eicemi. Kde\u017eto klima (podneb\u00ed) je dlouhodob\u00fd charakter po\u010das\u00ed. Doprov\u00e1z\u00ed ho pravideln\u00e9 v\u011btry, do kter\u00fdch pat\u0159\u00ed pas\u00e1ty, antipas\u00e1ty a monzuny. D\u00edky podneb\u00ed se Zem\u011b rozd\u011bluje na podnebn\u00e9 p\u00e1sy, ka\u017ed\u00fd m\u00e1 sv\u00e9 specifick\u00e9 rysy, faunu i floru. Po\u010das\u00ed pot\u00e9 ur\u010duj\u00ed meteorologick\u00e9 prvky jako je teplota, vlhkost, obla\u010dnost. Tlak, kter\u00fd do skupiny pat\u0159\u00ed tak\u00e9, vytv\u00e1\u0159\u00ed cyklony a anticyklony. Jedn\u00e1 se o oblasti se zm\u011bnou tlaku, pokud se jedn\u00e1 o cyklonu– tlakovou n\u00ed\u017ei – je to oblast se sn\u00ed\u017een\u00fdm tlakem. Anticykl\u00f3na – tlakov\u00e1 v\u00fd\u0161e – s vysok\u00fdm tlakem vzduchu.Front\u00e1ln\u00ed syst\u00e9my hraj\u00ed velkou roli p\u0159i tvorb\u011b p\u0159eh\u00e1n\u011bk a bou\u0159ek. Tepl\u00e1 fronta vznik\u00e1, kdy\u017e tepl\u00fd vzduch tla\u010d\u00ed chladn\u011bj\u0161\u00ed. Studen\u00e1 fronta naopak a pokud chladn\u011bj\u0161\u00ed studen\u00e1 fronta do\u017eene teplou frontu vznikne okluzn\u00ed fronta, kter\u00e1 se vyskytuje p\u0159ev\u00e1\u017en\u011b v tropick\u00fdch oblastech. Proto syst\u00e9m p\u0159edpov\u011bdi po\u010das\u00ed je velk\u00fd o\u0159\u00ed\u0161ek pro laiky. Poslechnout si p\u0159edpov\u011b\u010f v televizi neznamen\u00e1, \u017ee mus\u00ed 100 % pr\u0161et, tak\u017ee si rad\u0161i vezm\u011bte jak t\u00edlko, tak de\u0161tn\u00edk.                                                                                                                                                                                                                                                                                                                                                                                        4.2\/5 - (12 votes)        "},{"@context":"https:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"name":"Po\u010das\u00ed nebo klima?","item":"https:\/\/www.archall.cz\/pocasi-nebo-klima\/#breadcrumbitem"}]}]