Iilwandle, iilwandle, kunye neziqhamo ziileyibhile eziqhelekileyo kuwo onke amazwe eziqithi ezitshisayo.ESri Lanka, ekuLwandlekazi lwaseIndiya, iti emnyama ngokungathandabuzekiyo yenye yeempawu zayo ezikhethekileyo.Oomatshini bokukha itizifunwa kakhulu ekuhlaleni.Njengemvelaphi yeti emnyama yaseCeylon, enye yeeti ezine ezinkulu ezimnyama emhlabeni, kutheni iSri Lanka yeyona mvelaphi yeti emnyama kakhulu ngenxa yendawo yayo ekhethekileyo kunye neempawu zemozulu.

Isiseko sokutyala iti yaseCeylon silinganiselwe kwiindawo eziphakamileyo ezisembindini nakwimimandla esezantsi yelizwe lesiqithi.Yahlulwe yaziindawo ezisixhenxe eziphambili zemveliso ngokwejografi yezolimo, imozulu kunye nomhlaba.Ngokutsho kokuphakama okuhlukeneyo, yahlulwe yangamacandelo amathathu: iti ye-highland, iti ephakathi kunye ne-lowland tea.Nangona zonke iintlobo zeti zineempawu ezahlukeneyo, ngokomgangatho, iti ye-highland iseyeyona ilungileyo.

Iti ye-highland yaseSri Lanka iveliswa ikakhulu kwimimandla emithathu ye-Uva, Dimbula kunye neNuwara Eliya.Ngokuphathelele indawo yejografi, i-Uwo ifumaneka kwi-slope esempuma ye-Central Highlands, kunye nokuphakama kwe-900 ukuya kwi-1,600 yeemitha;IDimbula ikwithambeka elingasentshona loMbindi Weentaba, kwaye izitiya zeti kwindawo yemveliso zisasazwa kwi-1,100 ukuya kwi-1,600 yeemitha ngaphezu komphakamo wolwandle;kunye ne-Nuwara Eli Ifumaneka kwiintaba ezisembindini weSri Lanka, kunye nobude obuphakathi kweemitha ze-1868.

Uninzi lweendawo zokutyala iti zaseSri Lanka zikwindawo eziphakamileyo, kwayeisivuni setiisombulula ubunzima bendawo bokukha amagqabi eti ngexesha.Kungenxa ngokuchanekileyo ngenxa ye-alpine microclimate ekhethekileyo kule mimandla i-tea emnyama yaseLanka iveliswa.Iintaba zinamafu kwaye zinenkungu, kwaye umoya kunye nokufuma komhlaba kuyenyuka, nto leyo eyenza kube nzima kwiikhompawundi zeswekile ezenziwe yi-photosynthesis ye-tea buds kunye namagqabi ukuba ajike, i-cellulose ayenziwa lula, kwaye ihlumela lomthi weti linokuhlala litsha kwaye lithambile. ixesha elide ngaphandle kokuba kube lula ukuguga;ukongeza, iintaba eziphakamileyo Ihlathi liluhlaza, kwaye imithi yeti ifumana ukukhanya ixesha elifutshane, ukuqina okuphantsi, kunye nokukhanya okusasazekayo.Oku kuluncedo ekwandeni kweekhompawundi ezinenitrogen kwiti, ezifana neklorofili, initrogen epheleleyo, kunye nomxholo we-amino acid, kwaye ezi zinempembelelo kumbala, ivumba, incasa, kunye nokuthantamisa kweti.Kuyinzuzo kakhulu ukwandisa ubushushu;iqondo lokushisa malunga ne-20 degrees Celsius kwiindawo eziphakamileyo zaseSri Lanka yiqondo lokushisa elifanelekileyo lokukhula kweti;uhlaza lweAlpine luyachulumancisa kwaye kukho amasebe amaninzi namagqabi afileyo, enza umaleko oshinyeneyo wokugquma emhlabeni.Ngale ndlela, umhlaba awukho nje ukhululekile kwaye ulungelelaniswe kakuhle, kodwa kwakhona Umhlaba ucebile kwizinto eziphilayo, ukubonelela ngezondlo ezityebileyo zokukhula kwemithi yeti.Kakade ke, ingenelo yomhlaba yomhlaba othambekileyo olungele imijelo yamanzi ayinakubethwa ngoyaba.

Ukongeza, iimpawu zemozulu yaseLanka zemonsoon zidlala indima eqinisekileyo ekusebenziseni kamvaoomatshini bokuqhotsa itiukuqhotsa iti elungileyo.Kuba nakwiindawo ezivelisa iti eziphakamileyo, ayizizo zonke iti ezikumgangatho ofanayo kuwo onke amaxesha onyaka.Nangona imithi yeti ifuna imvula eninzi ukuze ikhule, kakhulu akwanelanga.Ngoko ke, xa imonsoon ekumzantsi-ntshona ehlotyeni izisa umphunga wamanzi osuka kuLwandlekazi lwaseIndiya ukuya kwimimandla ekwintshona yemimandla ephakamileyo, lixesha apho i-Uwa, ekwithambeka elingasempuma leentaba, ivelisa iti yodidi oluphezulu (Julayi-Septemba);ngokuchaseneyo, xa kufika ubusika, amanzi afudumeleyo namanzi e-Bay of Bengal Xa ukuhamba komoya kutyelela rhoqo kwiindawo ezisempuma yeendawo eziphakamileyo ngoncedo lwe-monsoon esenyakatho-mpuma, kwenzeka ukuba ixesha lokuvelisa i-Dimbula kunye ne-Nuwara Eliya. iti ekumgangatho ophezulu (ngoJanuwari ukuya kuMatshi).