Izindaba Zenethiwekhi Yamandla Omoya: Esigabeni sokuqala samaphrojekthi wamandla omoya, indawo yombhoshongo wokulinganisa umoya ihlobene eduze nendawo yenjini yomoya.Umbhoshongo wokulinganisa umoya uyisiteshi sereferensi yedatha, futhi indawo ngayinye ethile yenjini yomoya iyisibikezelo.yima.Kuphela uma isiteshi sokubikezela kanye nesiteshi sereferensi sinokufana okuthile, lapho kungase kuhlolwe kangcono imithombo yomoya kanye nesibikezelo esingcono sokukhiqizwa kukagesi.Okulandelayo ukuhlanganisa komhleli izici ezifanayo phakathi kweziteshi ezibamba iqhaza neziteshi zokubikezela.
I-Topography
Ingemuva elimangelengele liyafana.Ubukhulu obungaphezulu buthinta kakhulu ulayini wekhonta ome mpo wesivinini somoya esiseduze nendawo kanye namandla okunyakaza.Ubulukhuni besiteshi sereferensi kanye nesiteshi sokubikezela abukwazi ukuhambisana ngokuphelele, kodwa ukufana okungemuva okukhulu okunezici zesifunda kuyadingeka.
Izinga lobunkimbinkimbi bendawo liyafana.Ukuma komsinga womoya kuthintwa kakhulu ubunkimbinkimbi bendawo.Indawo eyinkimbinkimbi kakhulu, incane ububanzi obumele isiteshi sokubhekisela, ngoba isimo sezulu somoya omncane wendawo eyinkimbinkimbi siyinkimbinkimbi kakhulu futhi siyashintsha.Kungalesi sizathu ukuthi amapulazi omoya anezindawo eziyinkimbinkimbi ngokuvamile adinga imibhoshongo eminingi yokulinganisa umoya.
Izici zesimo sezulu somoya ezimbili
Ibanga liyafana.Ibanga eliphakathi kwesiteshi sereferensi nesiteshi sokubikezela liwumbandela oqondile ngokuqhathaniswa.Lokhu kuyiqiniso ezimweni eziningi, kodwa kunezimo ezithile, njengebanga ukusuka esiteshini sokubhekisela ngasogwini amakhilomitha angu-5 ukusuka ogwini oluqondile ukuya esiteshini sereferensi Uma kuqhathaniswa nendawo engamakhilomitha angu-3, isimo sezulu somoya singase sisondele isiteshi sokubhekisela.Ngakho-ke, uma ukuma komhlaba kanye ne-surface morphology kungashintshanga kakhulu endaweni enkulu yenkundla yomoya, ukufana kungahlulelwa ngokubhekisela ebangeni.
Ukuphakama kuyafana.Njengoba ukuphakama kukhula, izinga lokushisa nokucindezela komoya nakho kuzoshintsha, futhi umehluko wokuphakama uzoletha umehluko emoyeni nesimo sezulu.Ngokusho kokuhlangenwe nakho kwabasebenzi abaningi bezinsiza zomoya, umehluko wokuphakama phakathi kwesiteshi sereferensi nesiteshi sokubikezela akufanele udlule u-100m, futhi akufanele udlule u-150m kakhulu.Uma umehluko we-altitude umkhulu, kuyanconywa ukuthi wengeze imibhoshongo yokulinganisa umoya yokuphakama okuhlukile ukuze kukale umoya.
Ukuzinza komkhathi kuyafana.Ukuzinza komkhathi kunqunywa izinga lokushisa elingaphezulu.Uma izinga lokushisa liphezulu, kulapho i-convection eqondile iqina khona kanye nesimo sezulu esingazinzi kakhulu.Umehluko ezindaweni ezinamanzi kanye nokusabalala kwezitshalo kungase futhi kubangele umehluko ekuzinzeni komkhathi.
Isikhathi sokuthumela: Nov-02-2021
