Imimandla yemozulu kunye nenkcazo

Xa ufunda isicatshulwa semifuno yomhlaba, kunokuqatshelwa ukuba kukho ukwahlula kwiindawo apho abanye okanye abanye abameli beeflora kubakho. Isityholo esifanayo sisebenza kwihlabathi lezilwanyana. Oku kunqunywe yiimeko ezithile zemozulu ezikhoyo kwindawo nganye. Ngokusekelwe kulo mbono, ukwahlula kwimihlaba yezolimo. Makhe siwaqwalasele ngokubanzi.

Ummandla we-equatorial, okanye i-tropical interior, iquka inxalenye yomhlaba eqhubeka kunye ne-equator ngaphambi kokuqala kwe-10 ° S. W. No-10 ° sec. W. Lo mmandla ubonakaliswe ngumlinganiselo ophezulu weemvula kunye nokushisa okuphezulu. Ukunyuka kweqondo lokushisa akubalulekanga.

Emva koko kuza ummandla wezityalo ongaphandle. Kwakhona kubonakaliswe ukushisa okuphezulu, kodwa imvula ingaphantsi. Ixesha lezulu limile. Zonke iinkalo ze-climine zinempawu zabo zobume beemeko zemozulu.

Ukuqhubela phambili kukho indawo ye-subtropics okanye ummandla weemveliso zorhwebo. Lapha inani lemvula liyancitshiswa kakhulu. Umoya kulo mmandla ungaphantsi kancinci. Ngenxa yokukhuphuka kwemimoya yomoya, imozulu ayinasiphelo, kwaye ukuguqulwa kobushushu bomoya ngexesha lomsebenzi alibalulekanga. Iintlango ziyabonakala kule ndawo yezolimo.

Ummandla we-etheses ubonakaliswe utshintsho olubukhali kwihlobo lasebusika ehlobo ehlobo olomileyo.

Imozulu yemozulu epholileyo ibonakaliswa ngumlinganiselo ophezulu weemvula ngexesha lonyaka. Imozulu kwimeko enjalo inokufudumala, ikhululeke ngokukhululeka kwamaqabunga okanye kubanda, kodwa iholide emfutshane. Kuxhomekeke ekujongeni kolwandle.

Kodwa oku akuzona zonke iinkalo zeenkomfa ezimelelwe kwiplanethi yethu.

Oku kulandelelwano lwezityalo ezihamba ngokukhawuleza. Ubonakaliswe ngumlinganiselo omncinci wemphala, ukungcola kancinci komoya, ubusika obusika kunye nehlobo elifudumeleyo.

Imimandla yemozulu yomhlaba igqiba ukugqibela, indawo ye-polar okanye ye-arctic. Ubonakaliswe yimvula encinci kunye nobushushu obuphantsi kakhulu.

Imimandla yendalo kunye neyezulu kwiindawo ezahlukileyo azifani. Ziyakwazi ukubonakaliswa ngokukhawuleza okanye, ngokuchaseneyo, zibe nezixhobo ezinobuthakathaka. Oku kuxhomekeke kumlinganiselo womhlaba kunye nolwandle lwamanzi, kunye nemimoya yolwandle nolwandle.

Kodwa ke, iplanethi ijikelezwe yimihlaba yezulu efana neempawu ezifanayo kunye neemeko zemozulu.

Umzekelo wanikwa isahlulo esicacisiweyo seMhlaba kwiindawo ngokuhambelana nesimo sezulu esele sikhona. Kodwa ukuba sithetha kancinci, siyakwazi ukwahlula iindawo ezincinci ezihlanu.

Ekufuphi kweMzantsi kunye neNyakatho yePolisi yiindawo eziphambili. Emva koko, njengoko sisondela kwi-equator, kukho indawo yemozulu epholileyo. Kwaye ummandla wokugqibela ungamahlangothi omabini e-equator kwaye ubizwa ngokuba yi-tropical.

Amaninzi kumazwe aseYurophu akwindawo epholileyo.

Ngommandla ngamnye, abameli abathile beeflora kunye nezidalwa ziimpawu.

Ukuba sicinga ngemimandla yeenkcubeko zaseRashiya, ngoko kukho iintlobo ezahlukeneyo. Oku kungenxa yensima enkulu yelizwe, emele indawo epholileyo, i-subarctic, indawo ephantsi komhlaba kunye ne- arctic.

Izibonakaliso zemozulu zemihlaba elandelayo zichazwe ngokucacileyo: i-tundra, ihlathi, i-tundra, ihlathi, ihlathi kunye ne-arctic.

Iinkalo zezulu zichaphazela ubutyebi belizwe. Bayijonga ubuninzi bezilwanyana kunye nesityalo. Ngokomzekelo, iRashiya ngumlimi omkhulu kunye nomthengisi weefurs ezixabisekileyo.

Ngaloo ndlela, indawo yemozulu iyimpawu yomnye ummandla weplanethi. Iba ngumlinganiselo wokuba indawo yokuhlala yezilwanyana kunye nokukhula kweentlobo ezithile zezityalo. Ummandla ngamnye wemozulu uhambelana nesimo sezulu, esixhomekeke kwimimoya yomoya kunye nolwandle.