Mene ne wani anticyclone? Cyclones da anticyclones - tebur

Yanayi mamaki a kan ƙarni sun kasance abu na binciken saboda muhimmanci da tasiri a kan duk duniyoyin rayuwa. Cyclones da anticyclones ba togiya. A ra'ayi na wadannan weather mamaki ba da baya a makaranta labarin kasa. Cyclones da anticyclones, bayan wannan taƙaitaccen nazari domin da yawa ya zauna a asiri. Air talakawa da kuma fronts ne key Concepts cewa zai taimake nuna jigon wadannan weather faru.

iska talakawa

Yana yakan faru ne cewa saboda mutane da yawa dubban kilomita a cikin kwance shugabanci na iska yana da matukar kama da kaddarorin. Wannan taro da aka kira iska.

Air talakawa kasu kashi sanyi, dumi, da kuma gida:

- sanyi taro kira idan ta zafin jiki ne m fiye da yawan zafin jiki na surface a kan wanda shi ne located.

- dumi - shi ne irin wannan iska taro wanda zafin jiki ne mafi girma fiye da yawan zafin jiki na surface, wanda aka located a ƙasa da shi;

- gida iska taro zafin jiki ba ya bambanta daga surface karkashin shi.

The iska talakawa suna kafa a kan sassa daban daban na Duniya, abu don siffofin a cikin dũkiyarsu. Idan taro da aka kafa a kan Arctic, cewa, daidai da, da shi za a kira da Arctic. Hakika, wannan iska ne sosai sanyi, zai iya kawo m hazo ko haske hazo. Iyakacin duniya iska su ajiya ĩmãni temperate latitudes. Da kaddarorin iya bambanta dangane da abin da lokaci na shekara da ya zo. A cikin hunturu, da iyakacin duniya talakawa ba su da yawa daban-daban daga Arctic, amma wannan lokacin rani iska iya kawo wani sosai matalauta Ganuwar.

Tropical taro, ya fito daga cikin tropics da subtropics, suna da wani babban zafin jiki da kuma ya karu ƙura. Su ne originators na hazo, abin da ya rufe batutuwa, a lokacin da kyan gani daga nesa. Tropical taro kafa a kan babban yankin na Arewacin, kai ga kura vortices, da kuma hadari tornadoes. Equatorial iska ne sosai kama da wurare masu zafi, amma wadannan kaddarorin ne mafi pronounced.

fronts

Idan biyu iska talakawa da ciwon daban-daban yanayin zafi, a can ne kafa wani sabon yanayin sabon abu - gaban surface ko sashe.

By yanayin motsi gefuna kasu kashi na kullum da kuma mobile.

Kowane data kasance gaban raba tsakanin wani iska taro. Alal misali, babban gaban ne hasashen iyakacin duniya tsakiya tsakanin iyakacin duniya da kuma wurare masu zafi da iska, da babban Arctic - tsakanin Arctic da iyakacin duniya, da sauransu.

Idan dumi iska taro rarrafe a kan wani sanyi, dumi gaban auku. Domin matafiya a gaban ƙofar iya presage ko torrential ruwan sama ko dusar ƙanƙara, wanda zai rage da ganuwa. Lokacin da sanyi iska ne wedged karkashin wani dumi, akwai samuwar wani sanyi gaban. Jirãge shiga yanki na wani sanyi gaban, sha daga squalls, ruwan sama da kuma saukar aradu.

Yana haka ya faru da cewa iska talakawa ba fuskanta, da kuma kamawa up tare da juna. A irin haka ne, occluded gaban da aka kafa. Idan rawar da kama-up aikin wani sanyi taro, shi ne ake kira sabon abu na sanyi gaban occlusion, idan, a akasin haka, da dumi gaban occlusion. Wadannan fronts ne hadari yanayin da karfi gusts na iska.

Cyclones

Don gane da abin da wani anticyclone, shi ya kamata a fahimci cewa irin wannan cyclone. Wannan shi ne wani yanki na rage matsa lamba a wani yanayi da kadan nuna alama a cikin cibiyar. Anfaninta biyu iska gudana da ciwon daban-daban yanayin zafi. Very sharadi gwargwado ga su samuwar su ne a gaban. The iska a cikin cyclone tafiya daga gefen inda matsa lamba ne mafi girma a wajen cibiyar to low matsa lamba. A tsakiyar iska kamar yadda idan aka jefa up, da sa samuwar wannan qarfin iskar ba.

Kan yadda za a motsa da iska a cikin cyclone, zaka iya sanin ko a abin da yammancin duniya da shi aka kafa. Idan ya dace da shugabanci na kewaye iri na agogo, to, wannan shi ne shakka kudancin yammancin duniya, idan - da wannan arewacin yammancin duniya.

Cyclones tsokane irin yanayin da suka faru, kamar yadda girgije taro jari, da karfi hazo, iska da zafin jiki da bambancin.

guguwa

By cyclones kafa a temperate latitudes, rabu da cyclones cewa su asalin suyi yammacin sahara. Suna da yawa sunayen. Wannan mahaukaciyar guguwa (West Indies) da kuma typhoons (East Asia), da kuma sauki cyclones (Indian Ocean), da kuma Arch (ta Kudu Indian Ocean). Girman wannan vortex kewayon daga 100 zuwa 300 miles, da diamita na cibiyar - daga 20 zuwa 30 mil.

Iska sai accelerates zuwa 100 km / h, kuma shi ne na hali na dukan yankin na vortex, wanda fundamentally bambanta su daga cyclones kafa a temperate latitudes.

A tabbata ãyã daga cikin kimantawa ne cyclone ripples a cikin ruwa. Kuma shi ke a gaban shugabanci iska ne hurawa da iska cewa busa jim kadan kafin.

anticyclone

Filin ya karu matsa lamba a wani yanayi da ciwon a kalla a cibiyar - cewa shi ne Maɗaukaki. Matsa lamba a da ƙananan gefuna, barin iska rush daga cibiyar ga periphery. The iska makale a cikin cibiyar ne kullum saukar da diverges wajen gefuna da anticyclone. Kamar wancan kafa downdrafts.

Anticyclone ne m na cyclone ne ma saboda a Arewa Hemisphere, ya bi wani kewaye iri na agogo shugabanci a Kudancin ke kan shi.

Bayan sake karanta duk a sama bayani, shi ne hadari a ce cewa irin wannan wani anticyclone.

An ban sha'awa alama na anticyclones a temperate latitudes shi ne cewa su ze bi cyclones. A wannan yanayin, jinkirin-dabba ba a kanta yanayin gaba daya characterizes anticyclone. Weather, kafa ta wannan guguwa, gizagizai kuma bushe. Iska ne kusan ba ya lura.

Asian anticyclone

Na biyu sunan wannan sabon abu - Siberian high. A tsawon rayuwarsa - game 5 watanni, da kuma shi ne marigayi kaka (Nuwamba) - farkon spring (Maris). Wannan ba daya anticyclone, da kuma 'yan cewa suna sosai da wuya ba da hanyar cyclones. A tsawo daga iskõki har zuwa 3 km.

Saboda Gwargwadon yanayi (Asia tsaunika), da sanyi iska ba zai iya fasa, sakamakon kara sanyaya shi, kusa da surface zazzabi saukad da zuwa 60 digiri kasa sifili.

Baya da cewa irin wannan anticyclone, za mu iya cewa da tabbaci ba da wannan yanayi vortex na babban size, kawo sarari weather ba tare da hazo.

Cyclones da anticyclones. Kamance da kuma bambance-bambance

Domin fahimtar mafi alhẽri abin da yake wani anticyclone da wani cyclone, shi wajibi ne don kwatanta su. Ma'anar da kuma babban al'amurran da wadannan mamaki, mun sami fita. Ya zauna wani bude tambaya ko da bambance-bambance tsakanin cyclones da anticyclones. Tebur nuna bambanci more fili.

Saboda haka, da muka gani da bambance-bambance tsakanin cyclones da anticyclones. Tebur ya nuna cewa shi ne ba kawai da m, da yanayin da asalin mabanbanta.