Nangona kusekude ukutsho ngokuqinisekileyo ukuba isivunguvungu siya kubetha unxweme lweGulf ngaphambi kokuphela kuka-Agasti, kunokubakho isongelo kwiziqithi zase-United States kunye neCaribbean ukusuka eAtlantiki kwiintsuku ezizayo.
Njengoko indawo yemozulu ephazamisekileyo evela e-Afrika ekuqaleni kwale nyanga isiya ngasentshona kwiCaribbean kule mpelaveki, uphuhliso oluthe ngcembe lwetropikhi lunokwenzeka.
Ngokutsho kwe-AccuWeather Senior Meteorologist uBob Smerbeck, "Le mozulu iphazamisekile iya kuhamba kwindawo yomoya omanzi, imimoya elula phezulu kunye namanzi ashushu phezu kweCaribbean."
Ukuphazamiseka okucothayo kungekudala kuya kuqalisa ukuchaphazela ezinye zeziqithi zeCaribbean.
“Ii-Antilles eziNcinane ziya kuba nemimoya ebhudla ngamandla kunye neemvula ezinkulu ngoLwesine ebusuku ukuya ngolwesiHlanu ngelixa kunokwenzeka ukuba iZiqithi zaseVirgin kunye nePuerto Rico zifumana iimpembelelo ezifanayo ngempelaveki,” utshilo uSmerbeck.
Kweli nqanaba lokuqala, umkhondo kwiGulf of Mexico unokwenzeka kwiveki ezayo. Nangona kunjalo, kukho ifestile ebanzi yeendlela ezinokwenzeka kunye nemiqobo yokuba inkqubo yoyiswe ukuze uphuhliso luqhubeke.
Ukusebenzisana neziqithi ezikhulu zeCaribbean, ezifana nePuerto Rico, i-Hispaniola neCuba, kunokunciphisa ukomeleza kunye/okanye ukuphambukisa inkqubo ukuya emantla okanye emazantsi.
"Isakhiwo soxinzelelo oluphezulu ngaphaya kweMisissippi Valley esezantsi sinokunceda ukuhambisa eli nqaku ukuya nangaphaya kweGulf of Mexico ekupheleni kweveki, kodwa kunokwenzeka ukuba indawo yoxinzelelo oluphantsi oluphuhlayo empuma kunxweme oluphakathi kwe-Atlantiki itsalela inkqubo ukuya emantla ngaphaya kolwandle. Bahamas kunye neBermuda, ”utshilo uSmerbeck.
Imidla esuka kwiCaribbean ukuya kunxweme lweGulf, iAtlantiki esemazantsi eSeaboard nangaphakathi kumazwe aseMpuma kufuneka ibeke iliso elibukhali le meko.
Imvula enkulu kule mpelaveki kwiindawo ze-Ohio Valley kunye neAppalachian inokuba yinkxalabo eqhubekayo yezikhukula ukuba inkqubo yetropikhi egcwele izantyalantyala zemvula ibinokuzulazula ngaphakathi kwimpelaveki yoSuku lomSebenzi. Imijelo kunye nemilambo kwezinye iindawo ihamba ngaphezu komndilili ukuya ekupheleni kwehlobo.
INkanyamba yoNyaka iNcopho phakathi kuSeptemba
Nangona abanye abantu banokunxulumanisa ihlobo kunye nentliziyo yexesha lenkanyamba, izivunguvungu ezitshisayo kunye nezivunguvungu zase-Atlantiki ziphela ngasekupheleni kwehlobo kunye nesiganeko sokuqala sasekwindla.
Ngaphandle kwamanani abonakala ephantsi, isantya seenkqubo ezibizwa ngegama kwiAtlantiki singaphantsi komndilili ukuza kuthi ga ngoku.
Ngokutsho kwesazi ngemozulu seAccuWeather esiPhezulu uKristina Pydnynowski, “Ukulibaziseka kwamaxesha anento yokwenza nokulibaziseka kwenani leenkqubo zetropikhi.”
Amaqondo obushushu olwandle kuMntla weIkhweyitha adla ngokufika encotsheni ekupheleni kwehlobo. Ukongeza, iinkqubo zesaqhwithi ezingezizo ezetropikhi zilawula iimephu zemozulu kunye nemimoya yazo kwaye ngokubanzi zenza iindawo ezitshisayo zibe nobutshaba kakhulu ekuphuhliseni kwinxalenye yokuqala yehlobo.
Ipatheni yemozulu ezayo kwimpuma yoMntla Melika iya kuthandeka ngakumbi ukuba inkqubo yetropikhi isondele njengezowuni yomoya oshushu, ofumileyo onomoya olula kwaye usanda.
Ukuphazamiseka kweTropiki okulandelwayo kuya kuqhubeka nokulwa nomoya owomileyo, imimoya ephazamisayo kunye namaqondo obushushu amanzi asezantsi kwinxalenye yokuqala yempelaveki.
