Esikhathini esedlule, bekufanele sifunde ngokuphehla amandla omoya ezincwadini zokufunda zesikole samabanga aphezulu.Abakhiqizi bamandla omoya basebenzisa amandla omoya ukuguqula ugesi ube ugesi.Uma kuqhathaniswa nokuphehlwa kukagesi ngamalahle, ukukhiqizwa kwamandla omoya kuphephe kakhudlwana futhi kunobungani nemvelo.Uma kuqhathaniswa nokwakhiwa kweziteshi zokuphehla ugesi ngamanzi, ukukhiqizwa kwamandla omoya kudinga ukutshalwa kwezimali okuncane futhi kunciphisa umonakalo endaweni yemvelo yendawo.Namuhla, umhleli uzokhuluma kafushane ngomthelela wamandla omoya esimweni sezulu.
Ngokucwaninga ngokusebenza kwamapulazi omoya asogwini kanye namapulazi omoya aphakathi nezwe, kungatholakala ukuthi uma umswakama uphezulu, ipayipi elikhulu lomsila womoya ohwamukayo lijwayele ukujiya ngemuva kwesondo lomoya, okungase kuthinte i-microclimate yendawo, njenge umswakama nothuli.Yebo, lo mthelela empeleni mncane kakhulu, futhi ungase ube mncane kunomthelela womsindo nokufuduka kwezinyoni ezifudukayo endaweni ezungezile.Kusukela esikalini esikhulu, ukuphakama kokuthuthukiswa komuntu kwamandla omoya kunomkhawulo, futhi kuqinisekile ukuthi umthelela emathafeni aphansi nolwandle awubalulekile.Isibonelo, ukuphakama kokuhamba komhwamuko wamanzi we-monsoon ikakhulukazi cishe ku-850 kuya ku-900 Pa ongqimbeni olungaphezulu, okulingana namamitha ayinkulungwane ngaphezu kwezinga lolwandle.Ngokombono wokukhethwa kwesizinda sepulazi lomoya ezweni lami, indawo kanye namandla okuthuthukisa amapulazi omoya asezingomeni ezisendleleni yemvula kulinganiselwe kakhulu.Ukwengeza, ukusebenza kahle kwangempela kwama-turbines omoya kunomkhawulo, ngakho umthelela unganakwa.Yebo, uma isikali samandla omoya esikhathini esizayo sikhula sibe ngaphezu kwengxenye ethile yamandla okuthutha okujikeleza komkhathi, singakwazi ukubona umthelela osobala kwezinye izindawo-kodwa lilonke izinga lamanje lokuthuthukiswa kwamandla omoya encane kakhulu.Isizathu esiqondile salokhu kuvuka ukuthi umfutho womoya ongemuva kwesondo lomoya uphansi kunangaphambili, okubangela ukufiphala komhwamuko osemoyeni oseduze nokugcwala kwamanzi.Ukwenzeka kwalesi simo kukhawulelwe izimo zezulu, futhi akunakwenzeka emapulazini omoya aphakathi nezwe enyakatho lapho kutholakala khona umoya owomile wasenyakatho.
Kusukela kulesi singeniso esingenhla, kungabonakala ukuthi ukukhiqizwa kwamandla omoya akugcini nje ngokuhlanzekile, kuphephile futhi kusebenza kahle, kodwa okubaluleke kakhulu ukuthi umthelela wamajeneretha aphehla amandla omoya endaweni ezungezile, isimo sezulu sonke sendawo, nesimo sezulu sincane kakhulu; kungashiwo ukuthi cishe akukho.
Isikhathi sokuthumela: Aug-13-2021
