Kwinqaku elandulela eli besikuhlalutya ukuba liyintoni kwaye linaziphi iziphumo ukubanda. Sibonile njengesiphelo sokuba ingqibelelo yelahleko ebandayo isetyenziswe gwenxa siseti yeengxelo eziphosakeleyo ezihamba nayo. Kwaye umbono wokuba ukwehla okubandayo bubuchwephesha kwezobuchwephesha obuzimeleyo kumanqanaba aphezulu. Yaziwa ngcono njenge Dana. Esi sisiganeko semozulu esenzeka rhoqo ngonyaka kwaye sibonakaliswa ziimozulu zemozulu ezigwenxa ezenza umonakalo omkhulu.
Kweli nqaku uza kufunda yonke into malunga neDANA. Ngaba uyafuna ukwazi ngakumbi ngayo? Kufuneka uqhubeke ufunda.
Yintoni iDANA
Njengoko kuchaziwe kwinqaku lokwehla kobandayo, yinto ehlasela ngokupheleleyo icala laseMeditera leIberia. Kwenzeka njengoko igama layo libonisa ukuba kukudakumba okukumanqanaba aphezulu. Umoya uphantsi kotshintsho olukhulu kumanqanaba oxinzelelo lomoya kwaye yenza imvula enkulu ebonakala ngala maxesha. Umxholo wokwehla okubandayo ubhekisa kuphela kwiziphumo ezibangelwe lolu xinzelelo lodwa kubude kwaye isetyenziswa ngokudibeneyo ukubhengeza ukuba siza kuba neziganeko zemvula eziyingozi.
Nangona kunjalo, iingcali kwicandelo, kwaye ke abo bayaziyo ukuba isebenza njani le nto, bakhethe igama elithi DANA ukuchaza inkqubo evela kuyo.
Iveliswa njani
Ukuze i-DANA iqulunqwe kufuneka kubekho iintlobo ezahlukeneyo zeemeko ezinokwenzeka ngeli xesha lonyaka. Ngesi sizathu, kuqhelekile ukuba, kwiintsuku ezikufutshane Ihlobo laseSan Martín Kukho iintsuku apho kubakho imvula eyintlekele, edala umonakalo omkhulu.
Into yokuqala efunekayo ukuyilwa kwale meko yemozulu kukuba umoya we umlambo wejet uyajikeleza ukuze yenze amanani angasemva. Emva kwexesha, ukolulwa kwemisinga yomoya emazantsi kwenziwa ngenxa yokwehla koxinzelelo lomoya. Inxalenye ethe qelele yoxinzelelo olusezantsi ibonakala njengesiphumo sokuhamba komoya usiya emazantsi.
Njengoko besesitshilo kwamanye amanqaku afana nala Uxinzelelo lomoya, indawo yoxinzelelo oluphantsi ibonisa icala apho umoya uhamba khona. Imisinga yomoya ihamba ngokujikeleza kwintshona ye-hemisphere esemazantsi kunye nokuphambana newashi kumantla e-hemisphere. Kukujikeleza komoya oku kukhokelela ekubunjweni kwamafu e Uhlobo lweqela le-nimbus ukuvelisa izaqhwithi ezinamandla.
I-DANA yahlukaniswe ngokupheleleyo kummango owawukuwo kwaye iqala ukuya emazantsi. Kwelinye icala, kumaxesha amaninzi kwenzeka oko uxinzelelo oluphezulu kumantla eDANA. Ezi meko zezulu ezifanelekileyo zibonakaliswa luxinzelelo oluphezulu lomoya. Kulabo abangaziyo, umqolo uyindawo yomoya apho uxinzelelo luphezulu kunakwimimandla engqongileyo.
Iphi kwaye iveliswa nini iDANA
Eyona nto iqhelekileyo, iDANA yenzeka ngexesha lokuwa. Oku kungenxa yokuba umoya usajikeleza kwiindawo zaselwandle kubushushu behlobo. Ummandla othambekele ekubandezelekeni kolu hlobo lwesiganeko yiMeditera. KukwiPeninsula yethu apho kwenzeka khona ukothuka komoya okuhamba phambili kuyo yonke iNtshona Yurophu kunye nomoya ofudumeleyo nofumileyo ovela kuLwandle lweMeditera.
Ukusuka kwimijelo yejeti, kuba ezi zizihlwele zomoya obandayo oza ngamandla kwi-stratosphere (apho amaqondo obushushu asezantsi kakhulu), zisasazeka ngaphezulu kwamawaka eekhilomitha ukuba zibe nobubanzi obukhulu bekhulu leekhilomitha. Olu kuvulwa kukhulu luchaphazela yonke iPeninsuka egcina ineemvula ezinkulu ngamandla amakhulu phantse kuzo zonke iindawo ngaxeshanye.
Eyona ntshukumo iqhelekileyo iDANA inayo Kukujikeleza kwe-ntshona-mpuma, nangona ngamanye amaxesha inokuthatha icala elisemantla-mzantsi, ibangele ubunzima bomoya ukuba buguquke bade baphule. Xa oku kufuduswa kwesihlwele somoya kusenzeka, enye yazo ihlala izimele kodwa ibanda kakhulu kwaye iyodwa. Obu bubunzima bomoya obuya kubangela le mvula inamandla yimimoya neenkqwithela, esizibiza ngokuba yi-cold drop.
Iziphumo zale meko yemozulu zinamandla ngakumbi ngakumbi Umahluko kumaqondo obushushu phakathi kobunzima obubandayo bomoya obuhlala bodwa kunye nobushushu bomoya ovela elwandle. Ukuba ulwandle lufudumele, ubunzima bomoya buya kukhawuleza bube ngumphunga kwaye buza kuphinda bufike kubunzima obubandayo, kudala amafu amakhulu kunye nemvula enkulu.
Iziphumo zeDANA
Ingxaki eveliswa lolu hlobo lwemvula kukuba izixeko eziwela kuzo azilungelanga loo manzi ngexesha elifutshane. Kwaye kukuba umjelo ohambisa amanzi amdaka kunye nenethiwekhi yokuhambisa amanzi ifikelela kumda wayo kunye nezikhukula ezaziwayo zenzeka.
Iziphumo zale mvula kwisixeko esithile zibangelwe ukucwangciswa nokucwangciswa komhlaba. Isixeko ngasinye sine-PGOU (uCwangciso lweeDolophu noCwangciso loLawulo) oluqulathe yonke imiba eyimfuneko ukukhusela umonakalo kweyona mvula inamandla. Yimo YEZULU kunye neempawu zayo zibandakanyiwe kwi-PGOU yendawo. Ukuba, umzekelo, isixeko sijamelana neziphumo ezibi ezivela kwi-DANA minyaka le, eyona nto iqhelekileyo kukuzama ukwenza okanye ukuququzelela izibonelelo eziyimfuneko ukunciphisa umonakalo.
Izikhukula zidala umonakalo omkhulu wezinto kunye abanye abantu bayabulawa minyaka le kwilizwe lethu. Uninzi lwabantu abanjiswe zizithuthi, barhaxwa okanye bathathwa yimisinga kunye / okanye imilambo iyaphuphuma.
Njengoko ubona, ukubanda okubandayo akukho nto ngaphandle kwesiphumo okanye igama eliqhelekileyo elinikezelwa kolo xinzelelo lodwa olwenzeka kwindawo ebizwa ngokuba yi-DANA.