Khona umoya kunye nefuthe lazo lwemozulu-langa,

Imvulophu sukube le planethi, ngokuba umoya, idlala indima ephambili ebangela ukuba kusekwe iinkqubo zendalo kunye nokudalwa iimeko zemozulu. Kwakhona wenza umsebenzi ebalulekileyo yokhuselo, ekhusela Umhlaba kwimiphumo kwimitha ezahlukeneyo solar kwaye ekuhlaseleni ezincinane imizimba yasezulwini, leyo aqhumisele yinqakrzaze kwiingcamba ezishinyeneyo phambi kokuba afikelele komhlaba. I-atmosfera Isakhiwo igesi inamandla kakhulu kwaye owahlukeneyo. Eqalisiweyo enzulwini nobunzina yayo enkulu zezulu nefuthe ngqo kunye tsotsololo kolawulo lwemozulu kwiingingqi ngamnye zomhlaba, yaye yonke loo mhlaba.

imiqulu emikhulu komoya iveliswe kwiingcamba eziFihliweyo (umoya osezantsi) ubukhulu abasakwazi ifana elwandle okanye amazwekazi. Ngokuseka axela nelaye lasisiseko kakhulu ezinamandla iinkanyamba, neenkanyamba, amandla kakhulu otshabalalisayo neenkanyamba. Ukuhanjiswa komoya ukusuka kummandla omnye lonke kwezinye imisela iimeko zemozulu kunye neemeko zemozulu kwezi nkalo. Kwaye kaninzi babethwele iintlekele zemvelo.

Ngasinye giant air mass ukuba twatse iimpawu (degree of elubala, ubushushu, amanqanaba ukufuma uthuli kunye nezinye inclusions amazwe) yokufumana umgangatho kunye neempawu kwendawo lenzeka apho. Lisondela neminye imimandla, izihlwele umoya awuyitshintshi kuphela indlela yabo yezulu; kodwa utshintshwe ngokwabo nokuzuzwa iimpawu zemozulu ukuba uphawu kwezi ndawo.

A mfanekiso ocacile kwale meko olutshintshayo ukuze umoya ubunzima Russia, phakathi kwegazi yalo babeziindleko enkulu kweli lizwe ngenxa imozulu eziliqela, ngokuphindaphindiweyo nokulawula ukutshintsha ngokupheleleyo iipropati zabo. Ngaphezu kwesiqingatha mmandla Russian kuphenjelelwe yi khona umoya kuyilwa phezu Atlantic. Balizisa ke isambuku kwemvula kwi inxalenye yaseYurophu kweli lizwe, kwaye kwimimandla zaseSiberia le iinkanyamba efudumeleyo Mediterranean kakhulu ukunciphisa ingqele ebusika.

Ngokubanzi inkqubo entsonkothileyo khona umoya lohlobo ukubolekisa esesibhakabhakeni abe nolwalamano ecacileyo n'wina. Ngenxa yoko, ubunzima umoya phezu amacandelo kwakhiwa abandayo kumphezulu womhlaba, ejongene Iimbumba ezifudumeleyo zixubene nabo yaye ngaloo ndlela zenze ngaphambili omtsha umoya ezineempawu ngendlela ezahlukeneyo. Le isiphumo ngokukodwa ngendlela ngamandla ziingcathu zone zemozulu xa ehlaselayo kuyo umoya arctic kubanda.

Ukuxubana efudumeleyo Atlantic fronts esesibhakabhakeni, zakha ubunzima umoya omtsha, leyo, ngaphandle sokwehlisa, amafu Cumulus kunye Ukuvutha izandyondyo zemvula. Ngamanye amaxesha ezi Iimbumba ezibandayo esesibhakabhakeni, edlula kummandla Russia ndidibana khona umoya efudumeleyo ukufikelela imimandla esemazantsi eYurophu. Kodwa kwiimeko ezininzi bakhumbule sigcina loza Alps.

Kodwa e Asia kukho intshukumo simahla komoya arctic kwiindawo ezinkulu phantsi kwiintaba olusemazantsi eSiberia. Yaye le nto yabenza kwemozulu kubanda kakhulu kule mimandla.