Iindaba zeNethiwekhi yaMandla omoya: Kwinqanaba lokuqala leeprojekthi zamandla omoya, indawo yenqaba yokulinganisa umoya inxulumene ngokusondeleyo nendawo yeinjini yomoya.Inqaba yomlinganiselo womoya sisikhululo sedatha yereferensi, kwaye indawo nganye yeinjini yomoya ethile luqikelelo.yima.Kuphela kuxa isikhululo soqikelelo kunye nesikhululo sereferensi sinokufana okuthile, apho kunokuthi kwenziwe uvavanyo olungcono lwemithombo yomoya kunye noqikelelo olungcono lokuveliswa kwamandla.Oku kulandelayo kukudityaniswa komhleli kwemiba efanayo phakathi kwezikhululo ezithatha inxaxheba kunye nezikhululo zokuxela kwangaphambili.
Ubume bendawo
Uburhabaxa obungasemva buyafana.Uburhabaxa bomphezulu buchaphazela ikakhulu umgca wecontour othe nkqo wesantya somoya esikufutshane nomphezulu kunye nobunzulu besaqhwithi.Uburhabaxa bomphezulu besikhululo sesalathiso kunye nesikhululo sokuqikelela abunakungqinelana ngokupheleleyo, kodwa imvelaphi enkulu yokufana noburhabaxa kunye neempawu zengingqi iyimfuneko.
Iqondo lokuntsokotha komhlaba liyafana.Ubume bomoya okhoyo buchatshazelwa kakhulu bubunzima bomhlaba.I-terrain eyinkimbinkimbi ngakumbi, incinci i-reference range ye-reference station, kuba imozulu ye-micro-wind ye-terrain eyinkimbinkimbi inzima kakhulu kwaye iyaguquka.Kungenxa yesi sizathu ukuba iifama zomoya ezinomhlaba ontsonkothileyo zihlala zifuna iinqaba ezininzi zomlinganiselo womoya.
Imiba emibini yemozulu yomoya
Umgama uyafana.Umgama phakathi kwesikhululo sereferensi kunye nesikhululo soqikelelo yinqobo ethe ngqo.Oku kuyinyani kwiimeko ezininzi, kodwa kukho ezinye iimeko, ezinjengomgama osuka kwisikhululo sokungqinisisa ngaselunxwemeni lweekhilomitha ezi-5 ukusuka kunxweme oluthe nkqo ukuya kwisikhululo sokungqinisisa xa kuthelekiswa nendawo yeekhilomitha ezi-3, imozulu yomoya inokuba kufutshane nolwandle. isikhululo sesalathiso.Ke ngoko, ukuba ubume bomhlaba kunye ne-morphology yomphezulu abutshintshanga kakhulu ngaphakathi kwendawo enkulu yentsimi yomoya, ukufana kunokugwetywa ngokubhekiselele kumgama.
Ukuphakama kuyafana.Njengoko umphakamo usanda, iqondo lobushushu kunye noxinzelelo lomoya nazo ziya kutshintsha, kwaye umahluko wokuphakama uya kuzisa umahluko emoyeni nakwimozulu.Ngokwamava amaninzi kwiingcali zobutyebi bomoya, umahluko wobude phakathi kwesikhululo sesalathiso kunye nesikhululo soqikelelo kufuneka ungadluli kwi-100m, kwaye kufuneka ungagqithi kwi-150m ubukhulu becala.Ukuba umahluko wobude mkhulu, kuyacetyiswa ukuba kongezwe iinqaba zomlinganiselo womoya zobude obahlukeneyo kumlinganiselo womoya.
Ukuzinza kwe-atmospheric kuyafana.Ukuzinza kwe-atmospheric ngokusisiseko kunqunywe ngubushushu bomhlaba.Okukhona iqondo lobushushu liphezulu, kokukhona i-convection yomelele ngokuthe nkqo kunye nokungazinzi kweatmosfera.Umahluko kumhlaba wamanzi kunye nokugquma kwezityalo kusenokukhokelela kumahluko kuzinzo lwe-atmospheri.
Ixesha lokuposa: Nov-02-2021
