Izindaba UmphakathiSezulu

Uyini phambili aspirated? Atmosphere izimpi, izishingishane futhi anticyclones

Imvula ... iqhwa ... Ukubhoboza umoya ... ohangulayo ilanga ... Lezi kubonakaliswa sedlule ijwayelekile ngamunye wethu ebuntwaneni ezijulile. Kodwa ukukhuthalele cwaningo geography esikolweni, asifuni namanje ngezinye izikhathi kusimangaze ngokuphazima kweso lapho izinga lokushisa nezinhlekelele zemvelo engavamile. Nge uthuthumele zezulu njalo ezihambisana izimpi ozungeze umhlaba wethu. Bakha sezulu nsuku zonke kanye nokuchaza imingcele zonyaka.

sezulu phambi

Igama elithi "phambi" (kusukela Latin "frontis" - esiphongweni sakhe, ohlangothini front) kusho umugqa omncane phakathi okuthile. Kungathatha indawo, isibonelo, phakathi kwezindawo ezehlukene zemisebenzi: izindawo lokuhlushwa amabutho esitha nebutho enobungane. Uma sisebenzisa inkulumo ethi "phambili aspirated", sisuke ebhekisela emngceleni emoyeni, ingqophamlando emkhathini. Ukuthi wabelane, futhi kusithinta kanjani?

Umama imvelo ubumbe sezulu evumayo lapho abantu bengaphila khona, sakhe kabusha futhi ziphenduke. Siphila iThrojani efaka isimeli seseva, emkhathini ephansi, okuyinto hhayi kuphela usinika umoya-mpilo, kodwa siyahamba njalo. Ezinye volumetric emoyeni mass therein ngezikhathi basebenzisane. Phakathi naleyo lala mafu microclimate yayo emaphaketheni ezincane, okuyinto zingafani izakhiwo zabo, kodwa ngokuvamile iyunifomu, ngenkathi sigcina lokushisa esitebeleni kanye nomswakama. Izinkumbi ehamba phezu Zomhlaba, kanti kukhona ngisho babhekana. Kodwa musa mix. Umngcele phakathi kwazo kubizwa ngokuthi ngaphambili ozungeze umhlaba wethu.

Izinhlobo ezinkulu

I-bandwidth phakathi ezifanayo zokuhlola emoyeni uquqaba ifinyelela amashumi noma ngezinye izikhathi namakhulu amakhilomitha. Lokhu phambi asemkhathini, lapho kukhona njalo ingcindezi emoyeni okhuphuka zenzeka, cloudiness kanye ushintsho lokushisa. ncamashi lezi zindawo ungabona kanjani esikhundleni elangeni elishisayo Lokho kuza imvula ebandayo futhi okuphambene nalokho. Uma oxhumana naye liseduze kakhulu, eqinisweni mass homogeneous, phambi asemkhathini asivelanga. Ngenxa yalokho, isimo sezulu akashintshi.

Kunezinhlobo eziningana izimpi ozungeze umhlaba wethu. Bona kwamiswa ngesisekelo sezulu esihlukahlukene, izinkomba main okusalayo njalo.

  1. Arctic. Kuhlukanisa emoyeni abandayo kusukela ngokulinganisela arctic.
  2. Polar. Kutholwe phakathi esipholile futhi ezishisayo emoyeni uquqaba.
  3. Tropical. Lona umngcele phakathi esishintshashintshayo ezishisayo enkabazwe.

Endabeni ka baxhashazwe egcwele umoya uquqaba phambi wayethatha evundlile. Kulokhu, amakhaza emoyeni ungqimba elaliyoba kuwo njalo ezansi, futhi efudumele - phezulu. Kodwa ngenxa Ukuphinda njalo, yena engela phansi.

phambi abandayo

Kungakhathaliseki sezulu zizoshintsha esifundeni ukuthi kuyoba - konke lokhu kuzobonisa ibalazwe izimpi ozungeze umhlaba wethu. Kubonisa ngokucacile ukuthi ngaphambili efudumele njalo esitshekile bebheke lapho ezihambayo, abandayo - kolunye uhlangothi. Lapho mithandazo ngalapho okusezingeni eliphezulu lokushisa zone, nalo ingena phakathi nesigaxa yokuqala, ukusunduza phezulu, Ukupholisa kwenzeka endaweni. uquqaba Warm kancane kancane kuphole, baye bakhipha umswakama - amafu ngakho-kwakhiwa futhi ngamafu.

Uphawu lokuqala front abandayo esondela emvula zokwakheka Cumulus evelayo emkhathizwe. Ngesikhathi esifanayo lo Umoya ushaya e ipheshulwa, elishintsha isiqondiso. Wall sinda mvula ngokuzumayo. Dark esibhakabhakeni, ke besika umbani, ukuduma, nesichotho ngezinye izikhathi uya. sezulu esibi ihlala akukho amahora angaphezu kwamabili, ngemva kwalokho isikhathi kwezulu sithule. Amazinga air lehliselwa, ngezinye izikhathi ngokushesha 5-10 degrees, njengoba umkhathi isikhala ithatha ngokuphelele phambi abandayo, displacing emoyeni wotha ilanga.

phambi efudumele

Kumiswa It is uma okusezingeni eliphezulu omuhle lokushisa zone "aqoqana" isisindo abandayo. Wayebonakala ukundiza nezinye izingcweti phezu kwalo, kancane kancane liphuma. Isimo sezulu siyashintsha ngokushelela, ngaphandle yokwanda kwama esingalindelekile kanye spikes. Cirrus - lesibonakaliso sokuqala ukuthi ngaphambili esondela asemkhathini, maphakathi okuyinto okushisa kunalokho okusezingeni eliphezulu. Lomoya ningagcini. Uma kuyiyo, khona-ke ashaye ngaso sonke isikhathi futhi kulula.

Kancane kancane kufiphaza ancibilike, futhi isibhakabhaka akha umgubuzelo white zokwakheka okuqinile encane egqinsiwe ukuthi ihlukene nabantu ethandana nabo a blue sky ecacile. Ngemva kwesikhathi esithile, isigejane bona up: ungqimba obukhulu lize liba ngaphansi kwe, umoya ucosha, a Ukukhemezela imvula noma iqhwa ukukhanya uwela. Inzika waqinisa, hamba amahora ambalwa, ngezinye izikhathi izinsuku, kulandelwa ukufudumala. Isimo sezulu esihle ihlala isikhathi eside. Front asemkhathini, lapho ongaphakeme lokushisa ukushisa indawo Ubamba kusukela ihamba ngokushesha futhi steeper.

isishingishane

Air ezindaweni ebusweni emhlabathini engalingani. Ngenxa yalokho, ukwakheka esishintshashintshayo of umfutho ophakeme futhi ongaphakeme. Inkambu yokuqala emoyeni okwedlula, okwesibili - kule negative. Kusukela indawo ephezulu ingcindezi ngulona logeleta nibonakala njengoba bekungalindeleka kuthululwe ngokusebenzisa onqenqemeni ingilazi futhi igcwalise okuholela "umgodi" engxenyeni lapho a ingcindezi ongaphakeme. Lesi simo esiyingqayizivele sibangelwa zemvelo sikubiza emoyeni.

ephansi kwengcindezi ingxenye futhi kukhona isishingishane. It has simise vortex. Bona ukuthi amanzi ageleza aphume echibini - it yakha uphondo. Isimiso esifanayo usikhombisa sezulu. Cyclone - wentaba ofanayo lapho zigezwa khona, nabokhulumile sibheke phansi kuphela. Ngo isigxobo yayo maphakathi ingcindezi ongaphakeme, eveza nhlangothi zonke umoya futhi odlula phezulu, nge esonta ke clockwise e Nenkabazwe eningizimu nangokumelene - enyakatho. Ngaphakathi esinamafu isikhwishikhwishi, ngoba umoya waba "sucks" futhi ifu. Ubathola efana amagquma Roll kulo ezivela ezindaweni lapho yokucindezeleka okwandayo.

anticyclone

Isebenza abasebenzela. Maphakathi - high blood pressure, kukhona omningi, ngakho-ke kuhlakazeka kuzo zonke izinhlangothi, njengoba uma isibambo kusuka iphakethe khekhe ukhilimu. Ukusakaza okokusonteka ngokwewashi e Nenkabazwe, ngokumelene - eningizimu. Asiphumele esinye isibonelo: uma bayengelwa ekwenzeni ngamapayipi carbonated isiphuzo, bese uyayekela, wayehlale stechot e ingilazi. Isenzakalo esifanayo yilesi sifo anticyclone. Kuphela ngendiza kanye embulungeni yonke.

Isimo sezulu anticyclone ngokuvamile ecacile ngoba umfutho ophakeme displaces ingxenye efwini. Ngesikhathi esifanayo ehlobo kuhlale kushisa kakhulu: izithiyo kwifomu Tuček, ekuvimbeleni ilanga zishise emoyeni, kungekho. Ebusika, kwenzeka okuphambene. Ilanga uphansi ngokwanele, kodwa emoyeni efudumele, ngeke: azikho amafu, futhi ngakho akukho okubambe ukushisa. Ngenxa yalokho, ebusika, uma kuziwa i anticyclone, isimo sezulu zicacile kodwa nesithwathwa. By the way, ukutadisha asemkhathini izimpi, izishingishane futhi anticyclones, ukunyakaza kwabo, izinguquko kanye nenguquko bezulu ukwenza sezulu for endaweni ethize.

Liphetheni ikusasa liphetheni?

Into enzima kakhulu kunazo zonke, uthi bezulu, kuyinto sikulindele sezulu ezinsukwini ezintathu ezizayo. Okungukuthi, ngemva kubutsela lonke ulwazi oludingekayo ukuze bayisebenze ngokushesha, ikhumbula zonke vagaries of izimpi sezulu, izinguquko zasezindaweni futhi anticyclones. Kuphela ngokuqhathanisa idatha, singaqondile, singafinyelela eziphethweni.

Ukubikezela izulu zimi kanje:

  1. Esifushane - izinsuku ezintathu.
  2. I medium-term - kuze kube izinsuku eziyishumi.
  3. Isibikezelo sezulu - i ngenyanga noma sonyaka.

Okokuqala okubili - isinqumo bezulu zibalo wokushintsha kwamandla nokwakheka kwezinto kanye namandla okubakhona echaza isimo emkhathini. Ngenxa yalesi ochwepheshe sihlaziye kungenzeka zishintsheke umoya isiqondiso, kwezulu, kulindeleke ingcindezi yokwanda kwama kanye nomswakama. Isimo sezulu ngeke ngempela kuyiqiniso. Ngisho ne imishini entsha, bezulu abakwazi ukubikezela zonke lezimanga okulungiselelwe ngokwemvelo. Kodwa kungaba noma kunjalo kubalulekile, njengoba kule umhlahlo libhekisela olulindelekile nyangazonke noma ngezikhathi ezithile zonyaka sezulu anomalies.

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