Kwimozulu, kukho iikhonsepthi ezininzi ezibaluleke kakhulu. Imalunga nokudibana kunye ukwahluka. Ukuba sifuna ukwandisa umgangatho kunye nokuchaneka kwesimo sezulu, kufuneka sazi indlela yokuzihlalutya ezi zinto zenzekayo. Namhlanje siza kusebenza sazi inkcazo yezi zinto zinamandla kunye namandla asele enawo. Ukongeza, siza kubona ukuba lichaphazela njani ixesha kunye nendlela esinokuthi siziqonde ngayo.
Ngaba uyafuna ukwazi okungakumbi malunga nokwahluka kunye nokudibana? Siza kukucacisela yonke into ngokweenkcukacha.
Yintoni ukuhlangana kunye nokwahluka
Xa kusemoyeni kuthiwa kuyadibana, sibhekisa ekutyunyuzweni komoya kwindawo ethile njengesiphumo sokufuduka kwawo. Oku kutyumza kubangela ukuba ubunzima bomoya bufumbe kwindawo ethile. Kwelinye icala, ukwahluka kuchasene. Ngenxa yokuhamba kwomoya, iyasasazeka kwaye inike indawo ezinomoya omncinci kakhulu.
Njengoko kunokuqikelelwa, ezi zinto zichaphazela kakhulu uxinzelelo lweatmosferi, kuba, apho kukho ukuhlangana, kuyakubakho uxinzelelo oluphezulu lomoya kunye nolusezantsi ekwahlukaneni. Ukuqonda ukusebenza kwezi zinto Kuya kufuneka ubazi kakuhle ubume bomoya abunaye emoyeni.
Makhe sicinge indawo apho sifuna ukuhlalutya umoya kunye nemisinga. Siza kuzobe imigca yomoya oya kwicala kwimephu esekwe kuxinzelelo lomoya. Umgca ngamnye woxinzelelo ubizwa ngokuba yi-isohipsas. Oko kukuthi, imigca yoxinzelelo olulinganayo lomoya. Kwinqanaba eliphezulu lomoya, kufutshane ne ukuyeka, umoya ngulowo we geostrophic. Oku kuthetha ukuba ngumoya ojikeleza kwicala elihambelana nemigca yokuphakama kokulingana komhlaba ngokulinganayo.
Ukuba kwingingqi ephantsi kophononongo sibona ukuba imigca yokuhamba komoya iyadibana, kungenxa yokuba kukho ukudibana okanye ukudibana. Ngokuchaseneyo, ukuba le mizila yokuhamba iyavula kwaye ihambele kude, kuthiwa kukho ukungafani okanye ukusasazeka.
Inkqubo yokuhamba komoya
Siza kucinga ngohola wendlela ukufumana obu bushushu bungaphezulu. Ukuba uhola wendlela uneendlela ezi-4 okanye ezi-5 kwaye ngequbuliso iba yimizila emi-2 kuphela, siya kuba sonyusa ukugcwala kwabantu kule ndawo ngeendlela ezimbalwa. Okuchaseneyo kuyenzeka xa kukho iindlela ezimbini kwaye ngequbuliso kukho iindlela ezininzi. Ngoku, izithuthi ziqala ukohlukana kwaye kuya kuba lula ukunciphisa ukuxinana. Ewe, okufanayo kunokuchazwa ngokwahluka kunye nokudibana.
Enye yeemeko apho kunokwenzeka ukuba kubekho ukunyuka okuthe nkqo kunye nokuwa kwemikhosi yomoya kuqatshelwe xa kukho ubudlelwane nomoya wegradient. Izantya ezithwalwa kukunyuka nokuhla kwemimoya ziphakathi kwe-5 kunye ne-10 cm / s. Into esimele ukuyicinga kukuba, kwiindawo apho ukuhlangana komoya kuya kuba khona, siya kuba noxinzelelo oluphezulu lomoya kwaye, ke ngoko, ubukho bentsholongwane. Kule ndawo siza kuba nexesha elimnandi kwaye sonwabele amaqondo obushushu azinzileyo.
Ngokuchasene noko, kwindawo apho kukho ukwahluka komoya, siya kufumana ukuncipha koxinzelelo lomoya. Indawo ishiywe ngumoya omncinci. Umoya uhlala uthanda ukuya kwindawo apho unoxinzelelo oluncinci lokugcwalisa izikhewu. Ngesi sizathu, ezi ntshukumo zomoya zinokubangela inkanyamba okanye into efanayo nemozulu embi.
Impembelelo yokuxubana ekhoyo ekuhambeni komoya ojikeleze uxinzelelo oluphezulu okanye oluphantsi, kuthathelwa ingqalelo ukuba ukungqubana ngokwakho kubangela ukuphambuka kwicala lomoya, kukuvelisa ukwahluka okanye ukuhlangana. Oko kukuthi, icandelo elibonisa isantya esihamba ngokungafaniyo kwii-isobars lelo livela emoyeni elingena embindini woxinzelelo oluphantsi okanye likhutshwe ngaphandle xa kukho uxinzelelo oluphezulu.
Umahluko wobude
Ngokwahlukileyo, imimoya yomoya yahlulahlula ibe ziimpompo ezimbini eziqala ukushenxa kumacala ahlukeneyo. Inkqubo elawula oku kujikeleza ngokubanzi kweatmosfera iyachaphazeleka kwezi zinto. Xa singafani, umoya utshintshwa kumanqanaba amabini: ukuphakama kunye nomgangatho kunye nomhlaba. Ukuhamba komoya ukusuka kwenye indawo ukuya kwenye kwenziwa ngokuthe nkqo. Ezi ntshukumo zomoya zibangela ukwenziwa kwento eyaziwa ngokuba yiseli. Ukuba ubumbano lusezantsi, umoya womoya uqala ukuphakama kubude. Xa befika kumphakamo othile, bohlula-hluka zibe yimilambo emibini eya kwelinye icala.
Ukuba oku kuhamba komoya kuqala ukwehla, bafikelela kwindawo yokudibana kwaye, kufutshane nomhlaba, sifumana enye indawo eyahlukileyo yokuphambuka apho ibangela ukuba imisinga yomoya ihambele kwicala elahlukileyo kuleyo bayenze phezulu. Le yindlela ivaliwe ngayo isekethe okanye iseli.
Iiyantlukwano kwindawo ephakame zihlala zenzeka kwimimandla yeetropiki nakwimimandla ye-polar. Kwezi ndawo, ukuhamba komoya kuyachaphazeleka bubushushu obujikelezileyo kunye noxinano lwayo. Zonke ezi ntshukumo zenza inkqubo yeeseli ezi-3 ezinkulu ezikhutshiweyo ezivelisa inkqubo apho umoya uqala ukuhamba ngokuthe nkqo.
Amava nomoya
Ukuba amava aselulo naluphi na uncedo kuthi, kukuba xa sikufutshane nenqanaba lolwandle kuhlala kukho ukuhlangana okungakumbi okubangela uhlaziyo lweemitha ezingama-8.000 ukuphakama. Kuxa sikule ndawo iphakamileyo, kuxinzelelo lweemililitha ezingama-350, xa iyantlukwano ephawulayo iqala ukubakho.
Ukuba sibona uxinzelelo okanye isaqhwithi kwaye sikwinqanaba lolwandle, kungenxa yokuba ukudibana komoya. Oku kuncitshiswa kobunzima bomoya kuyayinyanzela ukuba inyuke ngokuthe nkqo, ngelixa iyapholisa kwaye iyancipha. Njengoko umoya okhulayo unyuka, zenza amafu emvula, ngakumbi ukuba ukunyuka kwenyambalala yomoya ime nkqo.
Ndiyathemba ukuba ngolu lwazi ungafunda banzi malunga nokuhlukahluka kunye nokudibana kunye nokubaluleka kwayo kwimeteorology.
Molo!
Xa kukho ukungafani komoya phezu komhlaba, uxinzelelo lomoya kwelo nqanaba liphezulu, kuba ngelo xesha kukho ukuxhaswa kwemimoya, oko kukuthi, imimoya iyehla ngokuthe nkqo. Xa le mimoya ifikelela ngaphezulu iya kukhangela amaziko oxinzelelo oluphantsi, apho i-Wind Convergence iyakwenzeka khona, kwaye kungenxa yolu xinzelelo luphantsi apho imimoya inokunyuka ngokuthe nkqo.
Nangona kunjalo, xa ubhala lo mhlathi (nakwimihlathi elandelayo):
“Njengoko unokuthekelela, ezi zinto zichaphazela kakhulu uxinzelelo lweatmosferi, kuba, apho kukho ukudibana, kuyakubakho uxinzelelo oluphezulu lomoya kunye nolusezantsi ekwahlukaneni. Ukuqonda indlela ezisebenza ngayo ezi zinto, kuya kufuneka uyazi kakuhle amandla omoya emoyeni. "
Ubhala inkqubo echaseneyo, echaza ukuba kukho uxinzelelo oluphezulu apho kukho ukuhlangana kwemimoya, kunye noxinzelelo olusezantsi ngokwahluka kwemimoya.
Ngaphandle kokuba uthetha ukuDibana kunye nokuDibana okwenzekayo hayi ngaphezulu kodwa phezulu emoyeni. Ukuba kunjalo, ndicinga ukuba kuya kufuneka uyicacisile loo nto, kuba iboleka ukungangqinelani!
Ngokufanayo, iposti ebalaseleyo!
Imibuliso evela eColombia!