Umphezulu bha kunye nempembelelo yayo phezu kwemozulu

Sidla phawula ubuhle bendalo, kodwa abafane bacinge malunga ezihlelwe ngayo, nendlela ebalulekileyo kukuba phantsi kweenyawo zethu. Kubonakala, nekhephu abengezelayo, siya ukudlala ebusika, kwaye umhlaba apho kukhula ingca, kunye emahlathini, ibe njengentlabathi eselunxwemeni lolwandle ovuthuzayo (yaye ulwandle) babizwa esinye - "ubuso emhlabeni".

Yintoni ehlanganiswa iplanethi yethu

Umsebenzi okanye elo naphantsi - lo umaleko phezulu kolu qweqwe lomhlaba, eliquka zonke iintlobo amadama, umkhenkce nomhlaba, aqukiweyo kwiinkqubo ezahlukeneyo zendalo.

Njani oko phantsi kweenyawo zethu, oko kuchaphazela imozulu? Okokuqala, ngenxa ukufunxeka okanye ku vangama ka kwelanga. Ngaphezu koko, impembelelo elo naphantsi kwimozulu ngokusebenzisa amanzi kunye negesi exchange kwakunye neenkqubo nemvelo. Umzekelo, amanzi ingacota kunendlela kumo umhlaba phezulu kwaye lwentaba-, ngenxa yoko iindawo zonxweme kufuneka lwemozulu zamva abo bakude ngabeelwandle kunye neelwandle.

zibone ukukhanya

Iqondo lobushushu emhlabeni yethu ixhomekeke elangeni. Kodwa njengokuba usazi, imiphezulu eyahlukileyo ngeendlela ezahlukeneyo ukufunxa kwaye zibonisa imitha yelanga, lisekelwe kule nefuthe elo naphantsi kwimozulu. Into yokuba umoya ngokwawo unalo conductivity thermal ephantsi kakhulu, ngenxa yokuba emoyeni kuyabanda ngaphezu imiphezulu: ezantsi zezulu wotha bubushushu ifunxwe ngamanzi okanye emhlabeni.

Snow ibonisa ukuya kwi-80% ye-radiation, ngoko ngoSeptemba xa ezi neetyuwa akukho kunomzimba ngoMatshi, nangona umlinganiselo radiation elanga kwiinyanga ngokulinganayo. A Indian ihlobo ezaziwayo-kakuhle, nathi kufuneka ukuba elo naphantsi: shushu ehlotyeni umhlaba ekwindla ngcembe onika amandla elanga, esongeza kulo ubushushu ezibolayo mass eluhlaza.

sezulu Insular

Wonke umntu othanda sezulu onomoya ngaphandle utshintsho obushushu zasebusika nezasehlotyeni. Uyasinika iilwandle kunye neelwandle. Ubunzima zolwelo itshiswe kancinci, kodwa unako ukusindisa ukuya ku-4 phinda ubushushu ngaphezu komhlaba. Ngaloo ndlela, amanzi elo naphantsi ngexesha lasehlotyeni oluhlala isixa esikhulu wamandla, kwaye ebusika linikeza, amalahle kwimimandla yonxweme.

Wobisi edumileyo elwandle - it kwakhona ngokwemfanelo emanzini. Beach kwemini ukufudumala ngakumbi, yandisa umoya oshushu "yadika 'icala zasebusika eli dama ukwenza impepho ukukhanya emanzini. Ebusuku, phezu koko, umhlaba ayaphola ngokukhawuleza, ingqele umoya ubunzima ihamba kwicala yolwandle, ngoko ke mpepho utshintsha ulwalathiso kabini ngemini.

ukukhululeka

kubaluleke kakhulu ukuba imozulu kunye selwnziwe. Ukuba elo naphantsi uthe tyaba, oko akuthethi kuphazamisana nokuhamba komoya. Kodwa kwiindawo apho kukho intaba okanye, icala, nelezihlambo, iimeko ezizodwa zidalwe. Umzekelo, ukuba ichibi ibekwe elitywinwe ngezantsi yoncedo engundoqo kunye nobushushu komphunga yamanzi saa, kwaye iqokelelwe kulo mmandla, ukudala microclimate.

Abaninzi baye beva ngalo ilizwe Sannikov kwi-Arctic Ocean. Kukho ingcamango yokuba ngokwenene akungekhe isiqithi kunye sezulu, ukuba indawo yomhlaba engqongwe ngokupheleleyo ezinemithi ezihambayo, kuye kwasasazwa umoya lifinyele, ubushushu akayi kuba "enokubangela", yaye glacier, ebonisa imitha yelanga liya kuqalisa ukuba nomzi kuzo kwesi siqithi.

Nanamhlanje sikwazi ukubona ezinye kwiziqithi elisemntla kohlaza, engaqhelekanga ezo ezinezinga. Oku kuchazwe liSebe awohluke ze kumphezulu zokuziswa emaweni amahlathi yokukhusela umoya, nolwandle ezingqonge smooths amathontsi lobushushu.

ukhuseleko kwivayirasi

Sisoloko sisiva ukuba ngenxa yokukhula kwenani mveliso greenhouse gases, kwaye hlathi eninzi ioksijini. Enyanisweni akunjalo; kuyimfuneko ukuba siqwalasele izinto elo naphantsi. izityalo ezifileyo kunye namagqabi ewile zikukutya inani elikhulu micro-eziphilayo, izinambuzane kunye ntshulube. Zonke ezi nkqubo ebaluleke kwenzeka nge kwakhululwa isixa esikhulu greenhouse gases kwaye oksijini ukufunxeka. Ngoko ke, inxalenye carbon dioxide, nto leyo izityalo ezivela emoyeni ubuyela emoyeni.

Ngokubanzi, izinto intsalela igcinwa malunga rhoqo ngenxa ekukhuleni mass eluhlaza, ukuba kuphosakele ukuzicingela ukuba hlathi - lo mveliso enjalo ekuveliseni ioksijini kweso sixeko. Kumahlathi ashinyeneyo ukuphefumla nzima ngakumbi kwiindawo zenqila, ngenxa ukufuma ephakamileyo ebangela umphezulu ubomi asebenzayo kuyo. Kakade ke, lo icandelo kube nefuthe kwimozulu, kodwa hayi ngqo kuphela, kodwa ngenxa ekutshatyalalisweni eziphilayo. Kwamahlathi kunye nomhlaba kunye nongcoliseko amanzi ikhokelela ekubeni ubunzima eluhlaza omtsha olukhulayo ezincinane, yaye lo, uhageleyo liba ekukhutshelwe emoyeni esinxilisayo lunezinto ngaphambili ukuba izityalo ezinxulumene. Ngoko ke, elo naphantsi yehlathi kwenza i "nemiphunga emhlabeni" kwi umthombo kunene greenhouse gases.