Yintoni na ubunzima umoya? Iintlobo khona umoya. Iimpawu kunye neempawu khona umoya

Ukuphendula lo mbuzo, yintoni na ubunzima umoya, sinokuthi oku indawo zokuhlala abantu. We uphefumle ngayo, sibona nokuva yonke imihla. Ngaphandle yabantu air kokugquma bekungayi kuba nako ukuqhuba nobomi babo.

Indima kwegazi flow yendalo

Yintoni na ubunzima umoya? Le komoya ezisa utshintsho kweemeko zemozulu. Ngenxa kwindalo medium yabangela imvula amawaka eekhilomitha ehlabathini lonke. Ikhephu nemvula, ukubanda nobushushu kulifikela imithetho emisiwe. Izazinzulu ulaziyo ukutshintsha kwemozulu sijule nzulu iipateni iintlekele zemvelo.

Siza kuzama ukuphendula umbuzo: yintoni na ubunzima umoya? Xa izibonelo zayo ziquka iinkanyamba, ihamba ngokuqhubekayo. Nabo iza uyafudumala okanye zokupholisa. Zihamba kunye njalo njalo, kodwa ke kwiimeko ezinqabileyo kukho ukutenxa trajectories yabo yesiqhelo. Ngenxa yoko komgomo ezinjalo kwindalo, iintlekele mboniso.

Ngenxa yoko, kwikhephu entlango iwela ekudalekeni amaqondo obushushu okanye iinkanyamba kwasekwa neenkanyamba, iinkanyamba. bonke edibana ngayo impendulo yalo mbuzo: yintoni na ubunzima umoya? Kwimo yazo kuxhomekeke koko imozulu, umoya Ukwanda ioksijini okanye ukufuma.

Ukutshintsha ubushushu nengqele: Oonobangela

khona umoya - yeyona inxaxheba ephambili kwimfundo imozulu emhlabeni. Amalahle esicwangciswe ojikeleze kungenxa amandla efunyenwe elangeni. Ngenxa yotshintsho lobushushu lutshintsha lexinene umoya. Imimandla rarefied ngakumbi azele imiqulu ashinyeneyo.

khona umoya - ingqokelela uthi ezahlukeneyo zomaleko sukube yeegesi, ngokuxhomekeke nokunikezelwa ubushushu emini nasebusuku. Ngobusuku-air time buyehla, kukho umoya ihamba evela maleko luthe in rarefied. amandla flow kuxhomekeke ekunciphiseni Velocity lobushushu imigodi ukufuma.

Kwi intshukumo okugqithileyo echaphazela ukuthambeka lobushushu tyaba, yaye nkqo. Earth Usuku ithatha ubushushu ukusuka uqale ilanga ukuba amnike zomaleko asezantsi yeegesi kwi ngokuhlwa. Le nkqubo yaqhubeka bumini kwaye ngentsasa elandelayo umphunga wamanzi kwi umoya bagxila. Oku kubangela imvula: umbethe, imvula, inkungu.

Yintoni na urhulumente sukube?

Iimpawu khona umoya - lixabiso oluninzi, enokusetyenziselwa ukuchaza ithi ezithile umaleko sukube nokuba ingaphononongwa kubo.

Kukho ezintathu isalathiso ezingundoqo ungqameko ye eziFihliweyo:

• Lobushushu inika ulwazi ngemvelaphi ukufuduka abaninzi.
• Ukufuma, ukwanda kwiindawo kufuphi kweelwandle, amachibi kunye nemilambo.
• Selubala kuchazwa ngaphandle. Esi sicwangciso kuchaphazela particulates emoyeni uthuli.

Kukho ezi ndidi zilandelayo khona umoya:

• Tropical - aye ezinezinga embindini.
• Arctic - ubunzima abandayo lisondela ezinezinga ezifudumeleyo inxalenye esemantla planethi.
• Antarctic - kuyabanda, yiya kwi-South Pole.
• Phakathi, icala, ezifudumeleyo mass umoya waza waya esibondeni ebandayo.
• Equatorial - kunayo yonke, diverge kummandla iqondo elisezantsi.

iintlobo zeHPV zingonobangela

Xa uhambisa khona umoya ukuguquka kwazo ukusuka uhlobo enye ukuya kwenye eengingqi. Kukho iintlobo zeHPV zingonobangela: elizwekazi zaselwandle. Ngako oko, owokuqala alawulwa elizweni, ngoxa olwesibini kuzisa ukufuma ngabeelwandle kunye neelwandle. Kukho umzekelo utshintsho obushushu kwezi inyambalala, kuxhomekeke kwixesha: ngumoya ehlotyeni ezweni ufudumele kakhulu kwaye ntolovelo ulwandle efudumeleyo.

Naphi na apho kukho ke khona umoya lubalaseleyo ezikhoyo rhoqo ngenxa imithetho emisiwe. Zimisela imozulu kule ndawo, yaye ngenxa yoko, oku kukhokelela umahluko enezityalo nezilwanyana. Kwiminyaka yakutshanje, inguqu khona umoya zatshintsha kakhulu ngenxa yezenzo zabantu.

Ukuguqulwa khona umoya ibonakalisiwe ngokucacileyo ngakumbi nemida yalo, apho ukungena nokuphuma kwimihlaba kunye nabo ulwandle. Kwezinye iindawo, umoya uyafa ngenxa owesibini. Amaninzi kuba njani na kowomileyo yaye akatshintshi indlela ixesha elide.

Njani na utshintsho kubunjani lokumpompoza?

mass Air kuzobonakala phantsi kweemeko ezithile. Imizekelo iziganeko ezinjalo amafu, amafu, fogs. Bangakwazi kuba zombini kwi ephakame amawaka eekhilomitha, yaye ngaphezu nje emhlabeni. Aba bamva akhekha ukuhla elibukhali kwamaqondo obushushu okukufutshane evela ukufuma ephakamileyo.

Sun ludlala indima ebalulekileyo kwinkqubo intshukumo engapheliyo khona umoya. Imini nobusuku kukhokelela kukuba kokungcola oxineneyo up, kunye nokunyuka amasuntswana yamanzi. Phezulu phaya esibhakabhakeni, bona nokuntlalutyisa nokuqalisa ukuba bawe. Ehlotyeni xa esifudumeleyo ngokwaneleyo ukuze zinyibilike icicles nexesha ngexesha esemoyeni, ngoko ubukele imvula isikakhulu ngohlobo imvula.

Kwaye ebusika, xa umhlaba kukho amanzi abandayo, uqala ikhephu okanye isichotho. Ngoko ke, kwiindawo Equatorial kunye ezinezinga tropical air efudumeleyo ivula kwakheka. Kule mimandla, imimandla yomntla ezi iidipozithi zenzeka phantse yonke imihla. flow Cold afudunyezwe kumphezulu shushu bomhlaba, lihlaleni imitha yelanga kwiiseli emoyeni. Kodwa ke ubushushu elinikiweyo ebusuku, ebangela ukuyilwa amafu, kusasa mbethe, inkungu.

Njengoko ngezizathu ezithile ingqalelo utshintsho kwimozulu?

Nkqu lokugqibela bafunda ukuqikelela kwemvula iimpawu ezicacileyo:

• Xa yebanga ngokulambisa ebonakalayo amafu kagesi okanye iindawo ezimhlophe ngohlobo semitha.
• Ukunyuka ngokukhawuleza umoya uthi indlela izihlwele ezibandayo. Isenokuba line, ikhephu.
• Clouds zisoloko ukuya kwiindawo xi eliphantsi. Kukho indlela esebenzayo ukuqinisekisa kule ndawo. Ukuze wenze oku, jikani yakho emfuleni khangela kancinane ukuya ekhohlo ikhoyo. noYaduwa Ukuba ukudumba, ingumqondiso ecacileyo yemozulu engentle. Musa ukuba bedidekile: ilifu kwicala lasekunene aba uphawu yempilo iimeko zemozulu.
• Ukubonakala isigqubuthelo ezimhlophe, xa ilanga liqala ukuba kweso.

Umoya kudambe, xa ummandla kubanda udlula. imilambo ezifudumeleyo bazalise zidle onesiphumo, kaninzi iba ukuvaleka emva kwemvula.