[{"@context":"https:\/\/schema.org\/","@type":"Article","@id":"https:\/\/www.gtasa.cz\/podnebi-a-cinitele\/#Article","mainEntityOfPage":"https:\/\/www.gtasa.cz\/podnebi-a-cinitele\/","headline":"Podneb\u00ed a \u010dinitel\u00e9","name":"Podneb\u00ed a \u010dinitel\u00e9","description":"S podneb\u00edm a po\u010das\u00edm se setk\u00e1v\u00e1me\u00a0ka\u017ed\u00fd den, ka\u017edou sekundu. Tak si n\u011bco o tom podneb\u00ed a po\u010das\u00ed v troposf\u00e9\u0159e pov\u00edme.\u00a0V podneb\u00ed se objevuj\u00ed meteorologick\u00e9 prvky: a) tlak vzduchu, b) vlhkost vzduchu, c) teplota vzduchu, d) slune\u010dn\u00ed svit, e) sm\u011br a rychlost v\u011btru, f) obla\u010dnost a za g) sr\u00e1\u017eky. Soubor v\u0161ech t\u011bchto meteorologick\u00fdch prvk\u016f ur\u010duje charakteristiku","datePublished":"2022-01-06","dateModified":"2022-01-06","author":{"@type":"Person","@id":"https:\/\/www.gtasa.cz\/author\/#Person","name":"","url":"https:\/\/www.gtasa.cz\/author\/","identifier":1,"image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/91506ed60e31abe586276a3e1420719df081581a820344a28fa2034bb1a2fe22?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/91506ed60e31abe586276a3e1420719df081581a820344a28fa2034bb1a2fe22?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"gtasa.cz","logo":{"@type":"ImageObject","@id":"\/logo.png","url":"\/logo.png","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/www.gtasa.cz\/wp-content\/uploads\/pexels-james-wheeler-1561322.jpg","url":"https:\/\/www.gtasa.cz\/wp-content\/uploads\/pexels-james-wheeler-1561322.jpg","height":0,"width":0},"url":"https:\/\/www.gtasa.cz\/podnebi-a-cinitele\/","about":["V\u011bda"],"wordCount":471,"articleBody":"S podneb\u00edm a po\u010das\u00edm se setk\u00e1v\u00e1me\u00a0ka\u017ed\u00fd den, ka\u017edou sekundu. Tak si n\u011bco o tom podneb\u00ed a po\u010das\u00ed v troposf\u00e9\u0159e pov\u00edme.\u00a0V podneb\u00ed se objevuj\u00ed meteorologick\u00e9 prvky: a) tlak vzduchu, b) vlhkost vzduchu, c) teplota vzduchu, d) slune\u010dn\u00ed svit, e) sm\u011br a rychlost v\u011btru, f) obla\u010dnost a za g) sr\u00e1\u017eky. Soubor v\u0161ech t\u011bchto meteorologick\u00fdch prvk\u016f ur\u010duje charakteristiku po\u010das\u00ed.Atmosf\u00e9rick\u00fd tlak m\u011b\u0159\u00edme pomoc\u00ed barometru, kter\u00fd m\u011b\u0159\u00ed okam\u017eit\u00fd stav tlaku vzduchu nebo barografem, kde je zaznamen\u00e1n \u010dasov\u00fd pr\u016fb\u011bh tlaku. Na m\u011b\u0159en\u00ed teploty vzduchu pou\u017e\u00edv\u00e1me stani\u010dn\u00ed teplom\u011bry, maxim\u00e1ln\u00ed a minim\u00e1ln\u00ed teplom\u011bry a termografy. Vlhkost vzduchu je vlastn\u011b obsah vodn\u00edch par v ovzdu\u0161\u00ed. Stavem nasycen\u00ed vznik\u00e1 maxim\u00e1ln\u00ed hodnota vlhkosti. Slune\u010dn\u00ed svit m\u011b\u0159\u00edme heliografem (pro m\u011b\u0159en\u00ed d\u00e9lky denn\u00edho sv\u011btla). Sm\u011br a rychlost v\u011btru se m\u011b\u0159\u00ed v\u011btrometrem (anemometrem). P\u0159ev\u00e1\u017en\u011b se m\u011b\u0159\u00ed v 10 metrech nad zem\u00ed. Obla\u010dnost ud\u00e1v\u00e1 stupe\u0148 pokryt\u00ed oblohy mraky. A sr\u00e1\u017eky m\u011b\u0159\u00edme sr\u00e1\u017ekom\u011brem.Oblaka rozli\u0161ujeme podle v\u00fd\u0161ky: a) vysok\u00e9 – 5-12 kilometr\u016f nad povrchem Zem\u011b, b) st\u0159edn\u00ed – 2-7 kilometr\u016f nad povrchem Zem\u011b a za c) n\u00edzk\u00e9 – 0-2 kilometry nad povrchem Zem\u011b.Hlavn\u00edmi klimatick\u00fdmi \u010diniteli jsou: A) zem\u011bpisn\u00e1 \u0161\u00ed\u0159ka – to je \u00fahlov\u00e1 vzd\u00e1lenost od rovn\u00edku. Jde vlastn\u011b o to, pod jak\u00fdm \u00fahlem dopadaj\u00ed slune\u010dn\u00ed paprsky na zem. B) nadmo\u0159sk\u00e1 v\u00fd\u0161ka – s p\u0159ib\u00fdvaj\u00edc\u00ed teplotou kles\u00e1 pr\u016fm\u011brn\u00e1 teplota vzduchu. Co\u017e je vlastn\u011b ka\u017ed\u00e9mu jasn\u00e9 a zn\u00e1 to u\u017e ze z\u00e1kladn\u00ed \u0161koly. Rozd\u00edlnost klimatu se tak\u00e9 projev\u00ed v rozd\u00edlnosti fl\u00f3ry a fauny, tam mluv\u00edme o vegeta\u010dn\u00ed stup\u0148ovitosti. C) mo\u0159sk\u00e9 proudy – tyto proudy opravdu v\u00fdrazn\u011b ovliv\u0148uj\u00ed klima Zem\u011b. Hnac\u00edm motorem pro tyto proudy je cirkulace vzduchu v atmosf\u00e9\u0159e, ale i slune\u010dn\u00ed z\u00e1\u0159en\u00ed \u010di ot\u00e1\u010den\u00ed zem\u011b. Te\u010f n\u011bco o tepl\u00fdch a studen\u00fdch proudech. Tepl\u00e9 proudy jsou ty, kter\u00e9 si nashrom\u00e1\u017ed\u00ed teplo v povrchov\u00fdch vod\u00e1ch na rovn\u00edku a p\u0159en\u00e1\u0161\u00ed je do chladn\u011bj\u0161\u00edch oblast\u00ed (u n\u00e1s v Evrop\u011b je to nap\u0159\u00edklad Golfsk\u00fd proud). Studen\u00e9 proudy velice \u010dasto ovliv\u0148uj\u00ed z\u00e1padn\u00ed pob\u0159e\u017e\u00ed kontinent\u016f a jsou z\u00e1rove\u0148 takov\u00fdm klimatick\u00fdm blokem proti z\u00e1padn\u00edmu proud\u011bn\u00ed (Benguelsk\u00fd proud). D) vliv \u010dlov\u011bka – Vliv \u010dlov\u011bka hraje na Zemi obrovskou roli. Nap\u0159\u00edklad t\u00edm, \u017ee budeme nap\u0159\u00edklad v Amazonsk\u00e9m pralesech vytv\u00e1\u0159et nov\u00e9 cesty, tak podneb\u00ed moc nepom\u016f\u017eeme, ale naopak, pokud sn\u00ed\u017e\u00edme emise nebo zv\u00fd\u0161\u00edme s\u00e1zen\u00ed strom\u016f, tak podneb\u00ed velice pom\u016f\u017eeme.                                                                                                                                                                                                                                                                                                                                                                                        3.9\/5 - (8 votes)        "},{"@context":"https:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"name":"Podneb\u00ed a \u010dinitel\u00e9","item":"https:\/\/www.gtasa.cz\/podnebi-a-cinitele\/#breadcrumbitem"}]}]