Uninzi lwezinto eziguqukayo zemozulu zichaphazela imozulu. Amaxabiso ezi zinto zixabisekileyo zezo zibangela ukungazinzi komoya, uzinzo, umoya ovuthuzayo, imvula, njl. Mhlawumbi umvile umntu ohlola imozulu amaxesha amaninzi esithi a ukubanda ngaphambili. Iyintoni le ndawo ibandayo?
Kweli nqaku siza kuchaza ukuba yintoni umphambili obandayo, ukuba wenziwe njani kunye neziphumo zemozulu.
Yintoni umphambili obandayo
Xa sithetha ngaphambili, sithetha ngentambo yokuqhagamshela phakathi kwomoya emibini eneempawu ezahlukeneyo. Ubunzima bomoya bujikeleza kwaye baneempawu ezahlukeneyo ngokuxhomekeke kwizinto eziguquguqukayo zemozulu esele sizichazile ngasentla. Enye yezinto eziqwalaselwe kakhulu kwiimpawu zomoya ukuze wazi iimpawu zangaphambili bubushushu.
Ngokwahluka, ikakhulu, sinokwazi uhlobo lwangaphambili oluza kwindawo. Ukuba kubanda ngaphambili, kushushu ngaphambili, njl. Enye yezinto eziguquguqukayo zomoya oxhomekeke kwimida ngu-lukufuma, isantya somoya kunye nendlela kunye noxinzelelo lomoya.
Umphambili obandayo ngulo ubonisa umda ophakathi ubunzima obuhambayo obubandayo, xa kuthelekiswa nobunzima bomoya oshushu. Ngokwesiqhelo, kolu hlobo lweefonti bubunzima obubandayo obususa ubushushu bomoya oshushu. Kubalulekile ukuba wazi ukuba umoya womoya awuxubeki ngaphambili. Ngaphandle koko, akukho ngaphambili kuya kwenziwa. Kufuneka sithathele ingqalelo umahluko phakathi koxinano xa sithetha ngendawo yomoya.
Khumbula ukuba i Umoya oshushu ungqindilili kunomoya obandayo, ke uya kuhlala unyuka. Xa ubunzima bomoya obandayo kunye nobunzima bomoya oshushu badibana, bubunzima bomoya obubandayo obuhamba ngokukhawuleza apha ebusweni kuba buxinene. Oku kubangela ukuba umoya oshushu uhambe endaweni ephezulu kuba uxinene. Ukuba sinendawo ebandayo ngaphambili, ngokubanzi, amaqondo obushushu aya kwehla kuba owona moya ubandayo uphezulu.
Yenziwa njani
Umfanekiso - Wikimedia / HERMENEGILDO SANTISTEBAN
Siza kuhlalutya inyathelo ngenyathelo ukuba lwenziwa njani olu hlobo lwangaphambili. Xa sinomoya ofumileyo kwaye ongazinzanga, xa uhlala unyuka ngenxa yobuninzi obuphantsi, uyakuhla uye kumaqondo obushushu aqhelekileyo troposphere. Njengoko sonyusa ukuphakama, amaqondo obushushu ayancipha kwithambeka lobushushu. Oku kuyakwenza ukuba umoya oshushu udibane ube ngamafu.
Kuxhomekeka kwimeko yokusingqongileyo kunye nobungakanani bomoya oshushu ojiyayo, ohlukileyo iintlobo zamafu. Ukuba umoya obandayo ususa indawo enkulu yomoya ofudumeleyo kwinqanaba eliphezulu lokunyuka, tSiza kuphetha ngokufumana ngakumbi lo moya oya kuba uncipha kwindawo ephezulu. Oku kuyakubangela ukukhula nkqo kwamafu e-cumulonimbus.
Olu hlobo lwelifu lubangela isiphithiphithi esikhulu somoya esibangela iimvula ezinkulu kwaye ezinkulu. Phakathi kweziganeko esinokuba nazo sinesichotho, izaqhwithi zombane, imimoya enamandla kakhulu, izaqhwithi zekhephu, imvukelo embi, imimoya ebhudlayo kunye neenkanyamba ukuba zinokubakho.
Kuya kufuneka kwakhona kuthiwe ayizizo zonke iindawo ezibandayo ezinogonyamelo olunje. Inqanaba lobundlobongela okanye ubungozi ngaphambili komlambo kuxhomekeke kubumanzi bomoya oshushu, ukongeza kwisixa somoya oshushu ojiweyo. Kungenzeka ukuba ukunyuka komoya ofudumeleyo akukho nkqo njengokuma ngokuthe nkqo kwamafu, kodwa ezinye i-nimbostratus ziya kuthi zenze imvula ethe chu. Elinye lawona maxabiso amiselweyo sisantya somoya. Kuxhomekeke kweli xabiso, ubunzima bomoya obandayo buza kuhamba ngesantya esiphezulu esiya kuthi, kwakhona, sihambise ngakumbi umoya oshushu ngobude. Ukuba umoya ufumile kwaye intshukumo ime nkqo, siya kuba nemozulu eyintlekele.
Iimpawu eziphambili
Imida ebandayo ihlala ihamba ngokukhawuleza, ngesantya esiphakathi kwama-40 nama-60 km / h. Oku kwenza ukuba ixesha lihlale phakathi kweentsuku ezi-3 ukuya kwezi-7. Ubude bommandla wonke oqhelekileyo ochaphazeleka buhlala phakathi kwama-500 nama-5.000 eekhilomitha. Ngokubanzi, inokuba phakathi kwe-5 km kunye ne-50 km.
Xa umphambili obandayo kusithiwa uyasondela, emoyeni oshushu uxinzelelo lomoya luzinzile. Kusenokwenzeka ukuba iyehla kumthamo omncinci yiyo le nto ibangela ukuba umoya uthambekele ekuhambeni kwindawo enoxinzelelo oluncinci lomoya. Into yokuqala esihlala siyijonga ukuchonga umphambili obandayo kukwenziwa kwamafu amhlophe aphezulu kakhulu. La mafu ngohlobo cirrostratus. Emva kwexesha, sBenza amafu aphakathi anjengeAltocumulus okanye iAltostratus. Ngeli xesha, umoya ulula kodwa awunasalathiso.
Njengokuba umphambili obandayo usiya usondela, amafu aya esanda nangakumbi kwaye imvula iya isiba namandla. Ngaphezulu kwayo yonke into, eyona nto ibonisa ukuba kufutshane nendawo ebandayo kukunyuka kobungakanani bamathontsi amanzi. Umoya uqala ukukhazimla kwaye ungabinaso isikhombisi esizinzileyo.
Xa sele sidibene nomphambili obandayo, siya kuqaphela ukwehla kwamaqondo obushushu, omelele Iishawa ezihlala zikhatshwa sisaqhwithi, umoya onamandla, ukungabonakali kakuhle nolwandle olulwayo.
Nje ukuba idlule ngaphambili
Xa umphambili obandayo udlulile, siya kuba nakho ukubona ukucocwa okukhulu emantla ntshona kwaye iya kuphucula ukubonakala ngakumbi. Iqondo lobushushu liza kwehla kwaye kuya kubakho ubumanzi obuncinci. Uxinzelelo lomoya lonyuka ngokukhawuleza, kuba umoya ongaphezulu kwethu uyabanda kwaye ngenxa yoko unzima.
Ngokuphathelele amafu, amanye amafu eecumulus akwanti anokuvela kodwa ngaphandle kwemvula engakumbi. Emantla, indima yomoya iya ngasekunene nakwindawo esemazantsi ye-hemisphere ngasekhohlo ngenxa yefuthe le-coriolis.
Ndiyathemba ukuba ngolu lwazi ungafunda ngakumbi malunga nokubanda ngaphambili nayo yonke into enxulumene nayo.
Ndiyabulela kakhulu ngolwazi ndinombuzo ndihlala eTegucigalpa, eHonduras, kodwa apha xa kusithiwa kukho indawo ebandayo, amafu abomvu ngombala kwaye akana mvula kwaphela.
Inkcazo elungileyo kakhulu