I-PVGIS 5.3 IMANIWALI YOSEBENZISAYO

1. Isingeniso

Leli khasi lichaza indlela yokusebenzisa i- I-PVGIS 5.3 isixhumi esibonakalayo sewebhu ukukhiqiza izibalo ze ilanga
ukukhiqizwa kwamandla e-radiation kanye ne-photovoltaic (PV). Sizozama ukukhombisa indlela yokusebenzisa
I-PVGIS 5.3 ngokwenza. Ungabheka futhi izindlela esetshenzisiwe ukwenza izibalo
noma ngamafuphi "ukuqala" umhlahlandlela .

Leli bhukwana liyachaza I-PVGIS inguqulo 5.3

1.1 Yini I-PVGIS

I-PVGIS 5.3 uhlelo lokusebenza lwewebhu oluvumela umsebenzisi ukuthi athole idatha emisebeni yelanga futhi
photovoltaic (PV) uhlelo lokukhiqiza amandla, kunoma iyiphi indawo ezindaweni eziningi zomhlaba. Ikona
kumahhala ngokuphelele ukusebenzisa, ngaphandle kwemikhawulo yokuthi imiphumela ingasetshenziselwa ini, futhi ngaphandle kwe-cha
ukubhaliswa okudingekayo.

I-PVGIS 5.3 ingasetshenziswa ukwenza izibalo eziningi ezahlukene. Le manuwali izokwenza chaza
ngamunye wabo. Ukusebenzisa I-PVGIS 5.3 kufanele udlule ku-a izinyathelo ezilula ezimbalwa. Okuningi kwe
ulwazi olunikezwe kule manuwali lungatholakala futhi emibhalweni yosizo ye I-PVGIS 5.3.

1.2 Okokufaka nokukhiphayo I-PVGIS 5.3

I I-PVGIS ukusebenzelana komsebenzisi kuboniswe ngezansi.

Iningi lamathuluzi ku I-PVGIS 5.3 zidinga okokufaka okuvela kumsebenzisi - lokhu iphathwa njengamafomu ewebhu ajwayelekile, lapho umsebenzisi achofoza izinketho noma efaka ulwazi, njengalokhu usayizi wesistimu ye-PV.

Ngaphambi kokufaka idatha yesibalo umsebenzisi kufanele akhethe indawo yendawo
okumele enze ukubala.

Lokhu kwenziwa ngu:

Ngokuchofoza kumephu, mhlawumbe nokusebenzisa inketho yokusondeza.

Ngokufaka ikheli ku- "ikheli" inkambu engezansi kwemephu.

Ngokufaka i-latitude ne-longitude ezindaweni ezingezansi kwemephu.
I-latitude nobude kungafakwa ngefomethi ethi DD:MM:SSA lapho u-DD engamadigri,
MM the arc-minute, SS the arc- seconds kanye no-A the hemisphere (N, S, E, W).
I-latitude nobude nakho kungafakwa njengamavelu edesimali, ngakho-ke isibonelo 45°15'N kufanele
kube okokufaka njengo-45.25. I-latitudes eningizimu yenkabazwe ingokufakwayo njengamavelu anegethivu, enyakatho ayiwo
positive.
Ubude obusentshonalanga kokungu-0° i-meridian kufanele inikezwe njengamavelu angalungile, amanani asempumalanga
zinhle.

I-PVGIS 5.3 ivumela i umsebenzisi ukuze uthole imiphumela ngenani elihlukene izindlela:

Njengenombolo namagrafu kukhonjiswe kusiphequluli sewebhu.

Wonke amagrafu angagcinwa futhi kufayela.

Njengolwazi olukufomethi yombhalo (CSV).
Amafomethi okukhiphayo achazwa ngokwehlukana ku- "Amathuluzi" ingxenye.

Njengombhalo we-PDF, otholakala ngemuva kokuthi umsebenzisi achofoze ukukhombisa imiphumela kufayela le- isiphequluli.

Ukusebenzisa okungahlangani I-PVGIS 5.3 amasevisi ewebhu (amasevisi e-API).
Lezi zichazwe ngokuqhubekayo ku "Amathuluzi" ingxenye.

2. Ukusebenzisa ulwazi lwama-horizon

Isibalo semisebe yelanga kanye/noma ukusebenza kwe-PV ku I-PVGIS 5.3 angasebenzisa ulwazi mayelana
umkhathizwe wendawo ukulinganisa imiphumela yezithunzi ezivela emagqumeni aseduze noma izintaba.
Umsebenzisi unezinketho eziningi zale nketho, eziboniswa kwesokudla se- imephu ku
I-PVGIS 5.3 ithuluzi.

Umsebenzisi unezinketho ezintathu zolwazi lomkhathizwe:

1.

Ungasebenzisi ulwazi lomkhathizwe ekubaleni.
Lokhu ukukhetha lapho umsebenzisi uyeka ukukhetha kokubili i "umkhathizwe obaliwe" kanye ne
"layisha ifayela le-horizon" ongakhetha kukho.

2.

Sebenzisa i- I-PVGIS 5.3 ulwazi lomkhathizwe olwakhelwe ngaphakathi.
Ukuze ukhethe lokhu, khetha "Umkhathizwe obaliwe" kwe I-PVGIS 5.3 ithuluzi.
Lena yi- okuzenzakalelayo inketho.

3.

Layisha ulwazi lwakho mayelana nobude be-horizon.
Ifayela le-horizon elizolayishwa kuwebhusayithi yethu kufanele libe
ifayela lombhalo elilula, njengalo ongalidala usebenzisa isihleli sombhalo (njenge-Notepad ye
Windows), noma ngokukhipha isipredishithi njengamavelu ahlukaniswe ngokhefana (.csv).
Igama lefayela kufanele libe nezandiso '.txt' noma '.csv'.
Efayelini kufanele kube nenombolo eyodwa emugqeni ngamunye, inombolo ngayinye imele i- umkhathizwe
ukuphakama ngamadigri endaweni ethile yekhampasi eduze nendawo yentshisekelo.
Ukuphakama komkhathizwe efayelini kufanele kunikezwe ngendlela yewashi kuqalwa kuyo Enyakatho;
okungukuthi, ukusuka eNyakatho, ukuya eMpumalanga, eNingizimu, eNtshonalanga, nokubuyela eNyakatho.
Amanani acatshangwa ukuthi amele ibanga elilinganayo le-angular eduze komkhathizwe.
Isibonelo, uma unamanani angama-36 efayelini,I-PVGIS 5.3 ucabanga ukuthi i iphuzu lokuqala kufanele
enyakatho, elandelayo yi-10 degrees empumalanga yenyakatho, njalo njalo, kuze kube iphuzu lokugcina, 10 degrees entshonalanga
yasenyakatho.
Ifayela eliyisibonelo lingatholakala lapha. Kulokhu, kunezinombolo eziyi-12 kuphela efayeleni,
okuhambisana nokuphakama komkhathizwe kuwo wonke ama-degree angu-30 azungeze umkhathizwe.

Iningi le I-PVGIS 5.3 amathuluzi (ngaphandle kochungechunge lwesikhathi semisebe yehora) azokwenza bonisa a igrafu ye
umkhathizwe kanye nemiphumela yokubala. Igrafu iboniswa njenge-polar icebo ne
ukuphakama komkhathizwe kuyindilinga. Umfanekiso olandelayo ubonisa isibonelo sesakhiwo se-horizon. Iso lenhlanzi
isithombe sekhamera yendawo efanayo siyakhonjiswa ukuze siqhathaniswe.

3. Ukukhetha imisebe yelanga database

Isizindalwazi se-solar radiation (DBs) esitholakala ku I-PVGIS 5.3 yilezi:

Zonke izingosi zolwazi zinikeza izilinganiso zehora ngemisebe yelanga.

Iningi le Idatha ye-Solar Power Estimation esetshenziswa ngu I-PVGIS 5.3 zibalwe ngezithombe zesathelayithi. Kukhona inombolo izindlela ezahlukene zokwenza lokhu, ngokusekelwe ekutheni kusetshenziswa amaphi amasathelayithi.

Izinketho ezitholakala ku- I-PVGIS 5.3 kwe ezikhona yilezi:

I-PVGIS-SARAH2 Le sethi yedatha kade kubalwe yi-CM SAF kuya esikhundleni sika-SARAH-1.
Le datha ihlanganisa i-Europe, i-Afrika, iningi le-Asia, nezingxenye zaseNingizimu Melika.

I-PVGIS- I-NSRDB Le sethi yedatha kade okuhlinzekwa yiNational I-Renewable Energy Laboratory (NREL) futhi iyingxenye ye I-National Solar Imisebe Isizindalwazi.

I-PVGIS-SARAH Le sethi yedatha beyi kubaliwe by CM SAF kanye I-PVGIS iqembu.
Le datha inokufakwa okufanayo kune I-PVGIS-SARAH2.

Ezinye izindawo azimboziwe idatha yesathelayithi, lokhu ikakhulukazi ku-latitude ephezulu
izindawo. Ngakho-ke sethule isizindalwazi esengeziwe semisebe yelanga eYurophu, okuyinto
ihlanganisa i-latitudes esenyakatho:

I-PVGIS-ERA5 Lokhu ukuhlaziya kabusha umkhiqizo kusuka ku-ECMWF.
Ukusabalala kusemhlabeni wonke ngesikhathi sokulungiswa kwehora kanye nokulungiswa kwendawo 0.28°i-lat/lon.

Ulwazi olwengeziwe mayelana idatha esekelwe ekuhlaziyweni kabusha kwemisebe yelanga kuyinto etholakalayo.
Ngenketho ngayinye yokubala kusixhumi esibonakalayo sewebhu, I-PVGIS 5.3 izokwethula i umsebenzisi ngokukhethwa kolwazi olugciniwe olumboza indawo ekhethwe umsebenzisi. Isibalo esingezansi sibonisa izindawo ezimbozwe yisizindalwazi ngasinye semisebe yelanga.

Lezi zingosi zolwazi yizo ezisetshenziswa ngokuzenzakalelayo lapho ipharamitha ye-raddatabase inganikezwanga
kumathuluzi angasebenzisi. Lezi futhi ziyisizindalwazi esisetshenziswa ethuluzini le-TMY.

4. Ibala uhlelo lwe-PV oluxhunywe kugridi ukusebenza

Amasistimu we-Photovoltaic guqula amandla we ukukhanya kwelanga kube amandla kagesi. Nakuba amamojula e-PV ekhiqiza ugesi oqondile wamanje (DC), ngokuvamile amamojula axhunywe ku-Inverter eguqula ugesi we-DC ube yi-AC, okuyinto ingasetshenziswa endaweni noma ithunyelwe kugridi kagesi. Lolu hlobo lwe Isistimu ye-PV ibizwa nge-grid-connected PV. I ukubalwa kokukhiqizwa kwamandla kucabanga ukuthi wonke amandla angasetshenziswa endaweni angaba ithunyelwe kugridi.

4.1 Okokufaka kwezibalo zesistimu ye-PV

I-PVGIS idinga ulwazi oluthile kumsebenzisi ukwenza izibalo zamandla e-PV ukukhiqizwa. Lokhu okokufaka kuchazwe kulokhu okulandelayo:

Ubuchwepheshe be-PV

Ukusebenza kwamamojula we-PV kuncike ekushiseni nasekushiseni i-solar irradiance, kodwa
ukuncika okuqondile kuyahlukahluka phakathi kwezinhlobo ezahlukene zamamojula we-PV. Okwamanje singakwazi
linganisela ukulahlekelwa ngenxa izinga lokushisa kanye ne-irradiance imiphumela yezinhlobo ezilandelayo ze
amamojula: crystalline silicon amaseli; amamojula wefilimu amancane enziwe nge-CIS noma i-CIGS nefilimu encane
amamojula enziwe ngeCadmium Telluride (CdTe).

Kobunye ubuchwepheshe (ikakhulukazi ubuchwepheshe obuhlukahlukene be-amorphous), lokhu kulungiswa akukwazi
kubalwe lapha. Uma ukhetha okukodwa kokukhethwa kukho kokuthathu kokuqala lapha ukubala kwe ukusebenza
izocabangela ukuncika kwezinga lokushisa kokusebenza kwabakhethiwe
ubuchwepheshe. Uma ukhetha enye inketho (enye/engaziwa), ukubala kuzothatha ukulahlekelwa kwe
Amandla angu-8% ngenxa yemiphumela yezinga lokushisa (inani elijwayelekile elitholwe linengqondo
izimo zezulu ezipholile).

Ukukhishwa kwamandla we-PV nakho kuncike kububanzi bemisebe yelanga. I-PVGIS 5.3 kungaba bala
ukuthi ukushintshashintsha kwe-spectrum yokukhanya kwelanga kuthinta kanjani ukukhiqizwa kwamandla jikelele kusuka ku-PV
uhlelo. Okwamanje lokhu kubala kungenziwa nge-crystalline silicon ne-CdTe amamojula.
Qaphela ukuthi lesi sibalo asikatholakali uma usebenzisa imisebe yelanga ye-NSRDB database.

Ipeak efakiwe amandla

Lawa amandla umkhiqizi athi i-PV array ingakhiqiza ngaphansi kokujwayelekile
izimo zokuhlola (STC), okuyi-1000W engaguquki yokukhanya kwelanga ngemitha yesikwele
indiza ye-array, ekushiseni kwe-array engu-25°C. Amandla aphezulu kufanele afakwe
i-kilowatt-peak (kWp). Uma ungawazi amandla aphezulu ashiwo amamojula akho kodwa kunalokho
yazi indawo yamamojula kanye nokusebenza kahle kokuguqulwa okumenyezelwe (ngamaphesenti), ungakwazi
bala amandla aphezulu njengamandla = indawo * ukusebenza kahle / 100. Bona incazelo eyengeziwe ku-FAQ.

Amamojula we-Bifacial: I-PVGIS 5.3 akunjalo't yenza izibalo ezithile ze-bifacial amamojula okwamanje.
Abasebenzisi abafisa ukuhlola izinzuzo ezingaba khona zalobu buchwepheshe bangakwazi okokufaka inani lamandla we
I-Bifacial Nameplate Irradiance. Lokhu kungase futhi kungalinganiselwa kusuka isiqongo sohlangothi lwangaphambili
amandla P_STC inani kanye ne-bifaciality factor, φ (uma kubikwe ku ishidi ledatha lemojuli) njenge: P_BNPI
= P_STC * (1 + φ * 0.135). NB le ndlela yokusebenzelana kwezinhlangothi zombili ayiyona efanele i-BAPV noma i-BIPV
ukufakwa noma amamojula akhwezwa ku-axis ye-NS okungukuthi ebheke EW.

Ukulahlekelwa kwesistimu

Isilinganiso sokulahlekelwa kwesistimu konke ukulahlekelwa ohlelweni, okubangela amandla empeleni
ilethwe kugridi kagesi ukuze ibe ngaphansi kwamandla akhiqizwa amamojula e-PV. Lapho
yizimbangela eziningana zalokhu kulahlekelwa, njengokulahlekelwa kwezintambo, iziguquli zamandla, ukungcola (ngezinye izikhathi
iqhwa) kumamojula nokunye. Ngokuhamba kweminyaka amamojula nawo avame ukulahlekelwa kancane kwawo
amandla, ngakho isilinganiso saminyaka yonke esiphumayo phakathi nesikhathi sokuphila sohlelo sizokwehla ngamaphesenti ambalwa
kunomphumela weminyaka yokuqala.

Sinikeze inani elizenzakalelayo elingu-14% kukho konke ukulahlekelwa. Uma unomqondo omuhle ukuthi wakho
inani lizohluka (mhlawumbe ngenxa ye-inverter esebenza kahle kakhulu) unganciphisa lokhu inani
kancane.

Ukukhweza isikhundla

Kuzinhlelo ezigxilile (ezingalandeleli), indlela amamojula akhwezwa ngayo izoba nomthelela kuwo
izinga lokushisa le-module, elibuye lithinte ukusebenza kahle. Ukuhlola kubonisiwe
ukuthi uma ukunyakaza komoya ngemuva kwamamojula kuvinjelwe, amamojula angathola kakhulu
ukushisa (kufika ku-15°C ngo-1000W/m2 wokukhanya kwelanga).

Ku I-PVGIS 5.3 kukhona okubili okunokwenzeka: ukuma mahhala, okusho ukuthi amamojula anjalo kugitsheziwe
ku-rack enomoya ogeleza ngokukhululekile ngemuva kwamamojula; kanye nesakhiwo- kuhlanganiswe, okuyinto kusho lokho
amamojula akhiwe ngokuphelele esakhiweni sodonga noma uphahla lwe isakhiwo, esingenamoya
ukunyakaza ngemuva kwamamojula.

Ezinye izinhlobo zokukhweza ziphakathi kwalokhu okubili okweqisayo, isibonelo uma amamojula ekhona
ifakwe ophahleni olunama-tiles ophahleni agobile, avumela umoya ukuhamba ngemuva amamojula. Kunjalo
amacala, ukusebenza kuyoba ndawana thize phakathi kwemiphumela yezibalo ezimbili ezikhona
kungenzeka lapha.

Lena i-engeli yamamojula e-PV asuka endizeni evundlile, okokugxilile (okungalandeleli)
ukukhweza.

Kwezinye izinhlelo zokusebenza i-slope ne-azimuth engeli izobe seyaziwa, isibonelo uma i-PV
amamojula azokwakhiwa ophahleni olukhona. Nokho, uma unethuba lokukhetha i
umthambeka kanye/noma i-azimuth, I-PVGIS 5.3 ingase futhi ukubalela wena elilungile amanani okwehlela kanye
i-azimuth (kuthatha ama-engeli angaguquki unyaka wonke).

Ukushintsha kwe-PV
amamojula

I-Azimuth
(ukuma) kwe-PV
amamojula

I-azimuth, noma i-orientation, i-engeli yamamojula we-PV ahlobene nesiqondiso esifanele eNingizimu. -
90° eMpumalanga, 0° eNingizimu ne-90° iWest.

Kwezinye izinhlelo zokusebenza i-slope ne-azimuth engeli izobe seyaziwa, isibonelo uma i-PV
amamojula azokwakhiwa ophahleni olukhona. Nokho, uma unethuba lokukhetha i
umthambeka kanye/noma i-azimuth, I-PVGIS 5.3 ingase futhi ukubalela wena elilungile amanani okwehlela kanye
i-azimuth (kuthatha ama-engeli angaguquki unyaka wonke).

Ukuthuthukisa
umthambeka (kanye
kungenzeka i-azimuth)

Uma uchofoza ukuze ukhethe le nketho, I-PVGIS 5.3 izobala ukuthambeka kwe-PV amamojula anikeza amandla aphezulu kakhulu okukhipha unyaka wonke. I-PVGIS 5.3 kungaba futhi bala i-azimuth ephezulu uma uthanda. Lezi zinketho zicabanga ukuthi i-slope kanye ne-azimuth engele hlala uqinile unyaka wonke.

Okwamasistimu e-PV anamathelayo axhunywe kugridi I-PVGIS 5.3 ingabala izindleko kagesi okhiqizwa uhlelo lwe-PV. Isibalo sisekelwe ku-a "Ifakwe ileveli Izindleko Zamandla" indlela yokubolekwa kwempahla, efana nendlela yokubalwa kwezindlu ngesilinganiso esinqunyiwe. Kumele faka izingcezu ezimbalwa zolwazi ukuze wenze izibalo:

Ugesi we-PV
izindleko ukubala

• Izindleko eziphelele zokuthenga nokufaka uhlelo lwe-PV, ngemali yakho. Uma ufake i-5kWp njenge
usayizi wesistimu, izindleko kufanele zibe zesistimu yalowo sayizi.

• Izinga lenzalo, ngo-% ngonyaka, lokhu kucatshangwa ukuthi kuvamile kukho konke ukuphila kwe i
Isistimu ye-PV.

• Isikhathi sokuphila esilindelwe sohlelo lwe-PV, ngeminyaka.

Isibalo sithatha ukuthi kuzoba nezindleko ezimisiwe ngonyaka zokunakekela i-PV
uhlelo (njengokushintshwa kwezingxenye eziphukayo), okulingana no-3% wezindleko zangempela
kwe uhlelo.

4.2 Imiphumela yokubala yegridi ye-PV exhunywe ukubala uhlelo

Imiphumela yokubala iqukethe amanani amaphakathi wonyaka okukhiqizwa kwamandla kanye
endizeni i-solar irradiation, kanye namagrafu amanani wenyanga.

Ngaphezu kokuphuma kwe-PV okumaphakathi konyaka kanye ne-avareji yemisebe, I-PVGIS 5.3 iphinde ibike
ukushintshashintsha konyaka nonyaka kokuphumayo kwe-PV, njengokuchezuka okujwayelekile kwe- amanani onyaka ngaphezulu
isikhathi esinedatha yemisebe yelanga kusizindalwazi esikhethiwe semisebe yelanga. Uphinde uthole i
ukubuka konke kokulahlekelwa okuhlukile kokuphumayo kwe-PV okubangelwa imiphumela ehlukahlukene.

Uma wenza ukubala igrafu ebonakalayo iwumphumela we-PV. Uma uvumela i-pointer yegundane
hambisa phezulu kwegrafu ungabona amanani wenyanga njengezinombolo. Ungashintsha phakathi kwe-
amagrafu ngokuchofoza izinkinobho:

Amagrafu anenkinobho yokulanda ekhoneni eliphezulu kwesokudla. Ngaphezu kwalokho, ungalanda i-PDF
idokhumenti enalo lonke ulwazi olukhonjiswe kumphumela wokubala.

5. Ukubala uhlelo lwe-PV lokulandela ilanga ukusebenza

5.1 Okokufaka kwezibalo ze-PV zokulandelela

Owesibili "ithebhu" kwe I-PVGIS 5.3 ivumela umsebenzisi ukuthi enze izibalo ze ukukhiqizwa kwamandla kusuka
izinhlobo ezahlukene zezinhlelo ze-PV zokulandela ilanga. Amasistimu e-PV okulandelela ilanga ane amamojula we-PV
kufakwe ezisekelweni ezihambisa amamojula emini ukuze amamojula abhekane isiqondiso
welanga.
Amasistimu acatshangwa ukuthi axhumeke kugridi, ngakho-ke ukukhiqizwa kwamandla we-PV kuzimele
ukusetshenziswa kwamandla wendawo.

6. Ibala ukusebenza kwesistimu ye-PV engaphandle kwegridi

6.1 Okokufaka kwezibalo ze-PV ezingaphandle kwegridi

I-PVGIS 5.3 idinga ulwazi oluthile kumsebenzisi ukwenza izibalo zamandla e-PV ukukhiqizwa.

Lokhu okokufaka kuchazwe kulokhu okulandelayo:

Kufakiwe
isiqongo amandla

Lawa amandla umkhiqizi athi i-PV array ingakhiqiza ngaphansi kokujwayelekile
izimo zokuhlola, okuyi-1000W engaguquki yokukhanya kwelanga ngemitha yesikwele ngayinye endizeni kwe
i-array, ekushiseni kwe-array engu-25°C. Amandla aphezulu kufanele afakwe i-watt-peak (Wp).
Qaphela umehluko kusukela kugridi exhunywe kwizibalo ze-PV zokulandelela lapho leli nani kuyinto
kucatshangwa ukuthi ku-kWp. Uma ungawazi amandla aphezulu ashiwo amamojula akho kodwa kunalokho
yazi indawo yamamojula kanye nokusebenza kahle kokuguqulwa okumenyezelwe (ngamaphesenti), ungakwazi
bala amandla aphezulu njengamandla = indawo * ukusebenza kahle / 100. Bona incazelo eyengeziwe ku-FAQ.

Ibhethri
umthamo

Lona usayizi, noma umthamo wamandla, webhethri elisetshenziswa kusistimu engaphandle kwegridi, ikalwa ngayo
amahora we-watt (Wh). Uma esikhundleni salokho wazi i-voltage yebhethri (yisho, i-12V) kanye nomthamo webhethri ngaphakathi
Ah, umthamo wamandla ungabalwa njenge-energycapacity=voltage*capacity.

Umthamo kufanele kube umthamo ojwayelekile ukusuka ekushajweni okuphelele ukuya ekukhishweni ngokuphelele, noma ngabe i-
Uhlelo lusethelwe ukunqamula ibhethri ngaphambi kokuthi likhishwe ngokugcwele (bona inketho elandelayo).

Khipha
umkhawulo wokunqamula

Amabhethri, ikakhulukazi amabhethri e-lead-acid, awonakala ngokushesha uma evunyelwe ngokuphelele
khipha kaningi. Ngakho-ke isinqamuleli sisetshenziswa ukuze ukushajwa kwebhethri kungabi ngaphansi a
iphesenti elithile lokushaja okuphelele. Lokhu kufanele kufakwe lapha. Inani elizenzakalelayo lingu-40%
(okuhambisana nobuchwepheshe bebhethri le-lead-acid). Kumabhethri e-Li-ion umsebenzisi angasetha okuphansi
ukunqanyulwa isb. 20%. Ukusetshenziswa ngosuku

Ukusetshenziswa
nge usuku

Lokhu ukusetshenziswa kwamandla kwazo zonke izinto zikagesi ezixhunywe ohlelweni ngesikhathi
isikhathi esingamahora angama-24. I-PVGIS 5.3 ucabanga ukuthi lokhu kusetshenziswa kwansuku zonke kuyasatshalaliswa ngokusobala phezu
amahora osuku, ahambisana nokusetshenziswa kwasekhaya okuvamile neningi le ukusetshenziswa ngesikhathi
kusihlwa. Ingxenye yehora yokusetshenziswa ecatshangwa ngu I-PVGIS 5.3 kuboniswa ngezansi kanye nedatha
ifayela liyatholakala lapha.

Layisha
ukusetshenziswa
idatha

Uma wazi ukuthi iphrofayili yokusetshenziswa ihlukile kuleyo emisiwe (bona ngenhla) onayo
inketho yokulayisha eyakho. Ulwazi lokusetshenziswa kwehora kufayela le-CSV elilayishiwe
kufanele iqukathe amanani wamahora angama-24, ngalinye ngomugqa walo. Amanani kufayela kufanele abe yi-
ingxenye yokusetshenziswa kwansuku zonke okwenzeka ehoreni ngalinye, nesamba sezinombolo
ilingana no-1. Iphrofayela yokusetshenziswa kwansuku zonke kufanele ichazwe ngesikhathi sasendaweni esijwayelekile, ngaphandle
ukucatshangelwa kokunciphisa ukukhanya kwemini uma kuhambisana nendawo. Ifomethi iyafana ne i
ifayela elisetshenziswayo elizenzakalelayo.

6.3 Ukubala imiphumela yezibalo ze-PV ezingaphandle kwegridi

I-PVGIS ibala ukukhiqizwa kwamandla we-PV ngaphandle kwegridi kucabangela ilanga imisebe yehora nehora esikhathini esiyiminyaka eminingana. Isibalo senziwa ku- izinyathelo ezilandelayo:

Ihora nehora bala imisebe yelanga kumojula ye-PV kanye ne-PV ehambisanayo
amandla

Uma amandla e-PV emakhulu kunokusetshenziswa kwamandla kulelo hora, gcina amanye
kwe amandla ebhethrini.

Uma ibhethri ligcwala, bala amandla "kumoshile" okungukuthi amandla e-PV angakwazi kube
akudliwe noma kugcinwe.

Uma ibhethri liba lingenalutho, bala amandla angekho bese wengeza usuku ekubaleni
kwe izinsuku lapho isistimu iphelelwe amandla.

Imiphumela yethuluzi le-PV elingaphandle kwegridi iqukethe amanani ezibalo waminyaka yonke namagrafu wanyanga zonke.
amanani okusebenza kwesistimu.
Kunamagrafu amathathu ahlukene anyanga zonke:

Isilinganiso sanyanga zonke sokukhishwa kwamandla kwansuku zonke kanye nesilinganiso sansuku zonke samandla angekho
ithathwe ngoba ibhethri ligcwale

Izibalo zanyanga zonke zokuthi ibhethri ligcwala kangaki noma lingabi nalutho phakathi nosuku.

I-Histogram yezibalo zokushajwa kwebhethri

Lokhu kufinyelelwa ngezinkinobho:

Sicela uqaphele lokhu okulandelayo ukuze uhumushe imiphumela engaphandle kwegridi:

i) I-PVGIS 5.3 yenza zonke izibalo zehora nge ihora ngesikhathi esiphelele uchungechunge lwelanga
idatha yemisebe esetshenzisiwe. Isibonelo, uma usebenzisa I-PVGIS-SARAH2 uzosebenza no-15
iminyaka yedatha. Njengoba kuchaziwe ngenhla, ukuphuma kwe-PV kungu kulinganiselwa.ihora nehora kusukela ku
uthole i-irradiance esendizeni. La mandla ahamba ngqo ku umthwalo futhi uma kukhona
ngokweqile, la mandla engeziwe uya ukushaja ibhethri.

Uma kwenzeka okukhiphayo kwe-PV kulelo hora kungaphansi kunokusetshenziswa, amandla ashodayo azokwazi
kube ethathwe ebhethrini.

Ngaso sonke isikhathi (ihora) lapho isimo sokushajwa kwebhethri sifinyelela ku-100%, I-PVGIS 5.3 yengeza usuku olulodwa esibalweni sezinsuku lapho ibhethri ligcwala khona. Lokhu bese kusetshenziselwa linganisela
% wezinsuku lapho ibhethri ligcwala khona.

I-PVGIS 5.3 yengeza usuku olulodwa esibalweni sezinsuku lapho ibhethri liba lingenalutho.

ii) Ngaphezu kwamanani amaphakathi wamandla angabanjwanga ngoba yebhethri egcwele noma kwe
isilinganiso samandla alahlekile, kubalulekile ukuhlola amanani wenyanga we-Ed kanye E_ilahlekile_njenge
bazisa ngendlela isistimu yebhethri ye-PV esebenza ngayo.

Isilinganiso sokukhiqiza amandla ngosuku (Ed): amandla akhiqizwa uhlelo lwe-PV oluya ku
umthwalo, hhayi ngokuqondile. Kungenzeka ukuthi ibigcinwe ebhethrini bese isetshenziswa yi-
umthwalo. Uma uhlelo lwe-PV lulukhulu kakhulu, inani eliphakeme yinani lokusetshenziswa komthwalo.

Amandla amaphakathi angathathwanga ngosuku (E_lost_d): amandla akhiqizwa uhlelo lwe-PV okuyilo
ilahlekile ngoba umthwalo ungaphansi kokukhiqizwa kwe-PV. La mandla awakwazi ukugcinwa ku-
ibhethri, noma uma igciniwe ayikwazi ukusetshenziswa yimithwalo njengoba isivele imboziwe.

Isamba salokhu okuguquguqukayo okubili siyefana ngisho noma amanye amapharamitha ashintsha. Kuphela
kuncike kumthamo we-PV ofakiwe. Isibonelo, uma umthwalo ubuzoba ngu-0, isamba se-PV
ukukhiqizwa izoboniswa njenge "amandla awathathwanga". Noma umthamo webhethri ushintsha,
futhi ezinye eziguquguqukayo zilungisiwe, isamba salawo mapharamitha amabili asishintshi.

iii) Amanye amapharamitha

Iphesenti lezinsuku ezinebhethri eligcwele: amandla e-PV angasetshenzisiwe umthwalo aya ku-
ibhethri, futhi ingagcwala

Iphesenti lezinsuku ezinebhethri elingenalutho: izinsuku lapho ibhethri ligcina lingenalutho
(okungukuthi umkhawulo wokukhipha), njengoba uhlelo lwe-PV lukhiqize amandla amancane kunomthwalo

"Amandla amaphakathi awathathwanga ngenxa yebhethri eligcwele" ikhombisa ukuthi mangakanani amandla e-PV ilahlekile
ngoba umthwalo umboziwe futhi ibhethri ligcwele. Isilinganiso sawo wonke amandla ilahlekile phezu kwe
uchungechunge lwesikhathi oluphelele (E_lost_d) luhlukaniswa ngenani lezinsuku ibhethri elizitholayo ngokugcwele
icala.

"Amandla amaphakathi ayashoda" amandla ashodayo, ngomqondo wokuthi umthwalo angeke
kuhlangatshezwana nayo kusuka ku-PV noma ibhethri. Isilinganiso samandla angekho
(I-Consumption-Ed) yazo zonke izinsuku ochungechungeni lwesikhathi oluhlukaniswa ngenani lezinsuku ibhethri
ithola ingenalutho okungukuthi ifinyelela umkhawulo wokukhipha omisiwe.

iv) Uma usayizi webhethri ukhushulwa kanye nokunye uhlelo uhlala okufanayo, i isilinganiso
amandla alahlekile azokwehla njengoba ibhethri lingagcina amandla amaningi angasetshenziswa okwe i
ilayisha ngokuhamba kwesikhathi. Futhi isilinganiso samandla esishodayo siyehla. Nokho, kuzoba khona a iphuzu
lapho la manani aqala khona ukuphakama. Njengoba usayizi webhethri ukhula, i-PV iyanda amandla kungaba
zigcinwe futhi zisetshenziselwe ukulayishwa kodwa kuzoba nezinsuku ezimbalwa lapho ibhethri lithola khona ngokugcwele
kukhokhiswe, kukhuphula inani lesilinganiso “isilinganiso samandla asithathwanga”. Ngokufanayo, lapho
kuyoba, ngokuphelele, amandla amancane angekho, njengoba amaningi angagcinwa, kodwa Lapho kuzoba inombolo encane
kwezinsuku lapho ibhethri liba ngenalutho, ngakho-ke amandla aphakathi ayashoda iyanda.

v) Ukuze wazi ngempela ukuthi angakanani amandla anikezwa yi- I-PV isistimu yebhethri ku-
imithwalo, umuntu angasebenzisa amanani ajwayelekile wenyanga we-Ed. Phindaphinda ngayinye ngenombolo ye
izinsuku ku inyanga kanye nenani leminyaka (khumbula ukucabangela iminyaka ye-leap!). Isamba
imibukiso Kanjani amandla amaningi aya emthwalweni (ngokuqondile noma ngokungaqondile ngebhethri). Okufanayo
inqubo kungaba zingasetshenziswa ukubala ukuthi mangakanani amandla ashodayo, kukhumbula ukuthi
isilinganiso amandla hhayi okuthunjiwe nokulahlekile kubalwa kucatshangelwa inani lezinsuku
ibhethri liyathola ngokugcwele ishajiwe noma ayinalutho ngokulandelana, hhayi inani eliphelele lezinsuku.

vi) Ngenkathi ohlelweni oluxhunywe kugridi siphakamisa okuzenzakalelayo inani ngokulahleka kwesistimu
ku-14%, asikwenzi’t inikeza lokho okuguquguqukayo njengokufakwayo ukuze abasebenzisi bakulungisele i izilinganiso
yesistimu ye-off-grid. Kulokhu, sisebenzisa inani isilinganiso sokusebenza salo i ephelele
isistimu ye-off-grid engu-0.67. Lokhu kungase kube ukulinganisa okuvamile, kodwa kuhlosiwe ku hlanganisa
ukulahlekelwa okuvela ekusebenzeni kwebhethri, i-inverter kanye nokuwohloka kwe- ezahlukene
izingxenye zesistimu

7. Isilinganiso sanyanga zonke sedatha yemisebe yelanga

Le thebhu ivumela umsebenzisi ukuthi abone ngeso lengqondo futhi alande idatha emaphakathi yanyanga zonke yemisebe yelanga kanye
izinga lokushisa phakathi nenkathi yeminyaka eminingi.

Izinketho zokufaka kuthebhu yemisebe yanyanga zonke

Umsebenzisi kufanele aqale akhethe unyaka wokuqala nowokugcina wokukhiphayo. Bese kuba khona a
inani lezinketho ongakhetha kuzo ukuthi iyiphi idatha ongayibala

Umhlaba jikelele evundlile
ukukhishwa kwemisebe

Leli nani isamba sanyanga zonke samandla emisebe yelanga esifinyelela kumitha yesikwele esisodwa sika-a
indiza evundlile, ikalwa ngo-kWh/m2.

Okujwayelekile okuqondile
ukukhishwa kwemisebe

Leli nani liyisamba sanyanga zonke samandla emisebe yelanga efinyelela kumitha yesikwele esisodwa sendiza
njalo ibheke ngaselanga, ikalwa ngo-kWh/m2, okuhlanganisa nemisebe kuphela
ukufika ngqo kusuka ku-disc yelanga.

Umhlaba jikelele
iradiation, elilungile
i-angle

Leli nani liyisamba sanyanga zonke samandla emisebe yelanga efinyelela kumitha yesikwele esisodwa sendiza
ibheke ngasenkabazwe, engeli yokuthambekela enikeza inani eliphakeme kakhulu lonyaka
ukukhanya, kukalwa ngo-kWh/m2.

Umhlaba jikelele
ukukhanya,
i-engeli ekhethiwe

Leli nani liyisamba sanyanga zonke samandla emisebe yelanga efinyelela kumitha yesikwele esisodwa sendiza
kubheke ngasenkabazwe, ku-engeli yokuthamba ekhethwe umsebenzisi, kukalwa ngo
kWh/m2.

Isilinganiso se sabalalisa
emhlabeni jikelele
imisebe

Ingxenye enkulu yemisebe efika phansi ayiveli ngokuqondile elangeni kodwa
ngenxa yokuhlakazeka okuvela emoyeni (isibhakabhaka esiluhlaza) amafu kanye nenkungu. Lokhu kwaziwa ngokuthi i-diffuse
imisebe.Le nombolo inikeza ingxenye yesamba semisebe efika phansi okuyiyona ngenxa yokusabalalisa imisebe.

Ukukhishwa kwemisebe yanyanga zonke

Imiphumela yezibalo zenyanga zemisebe ikhonjiswa kuphela njengamagrafu, nakuba i
amanani afakwe kuthebula angalandwa ngefomethi ye-CSV noma ye-PDF.
Kunamagrafu afika kwamathathu ahlukene eziboniswa ngokuchofoza izinkinobho:

Umsebenzisi angase acele izinketho eziningana ezahlukene zemisebe yelanga. Konke lokhu kuzoba kuboniswe ku
igrafu efanayo. Umsebenzisi angafihla ijika elilodwa noma amaningi kugrafu ngokuchofoza ku
izinganekwane.

8. Idatha yephrofayela yemisebe yansuku zonke

Leli thuluzi livumela umsebenzisi ukuthi abone futhi alande iphrofayili emaphakathi yansuku zonke yemisebe yelanga nomoya
izinga lokushisa lenyanga enikeziwe. Iphrofayili ikhombisa ukuthi imisebe yelanga (noma izinga lokushisa)
izinguquko kusuka ehoreni kuya ehoreni ngokwesilinganiso.

Izinketho zokufaka kuthebhu yephrofayela yemisebe yansuku zonke

Umsebenzisi kufanele akhethe inyanga azoyibonisa. Okwenguqulo yesevisi yewebhu yaleli thuluzi kunjalo futhi
kungenzeka ukuthola zonke izinyanga eziyi-12 ngomyalo owodwa.

Umphumela wokubala kwephrofayela yansuku zonke amanani wamahora angama-24. Lezi zingaboniswa noma
njengoba a umsebenzi wesikhathi ngesikhathi se-UTC noma njengesikhathi endaweni yesikhathi yasendaweni. Qaphela ukuthi ukukhanya kwasendaweni
ukulondoloza isikhathi AKUNAKEKWE.

Idatha engaboniswa iwela ezigabeni ezintathu:

I-Irradiance endizeni egxilile Ngale nketho uthola okomhlaba jikelele, okuqondile, nokusabalalisa
irradiance amaphrofayili emisebe yelanga endizeni engashintshi, enethambeka ne-azimuth ekhethiwe
ngomsebenzisi. Ngokuzithandela ungabona futhi iphrofayili ye-light-sky irradiance
(inani lethiyori okwe i-irradiance uma engekho amafu).

I-Irradiance endizeni elandela ilanga Ngale ndlela uthola i-global, eqondile, kanye
sabalalisa amaphrofayili we-irradiance wemisebe yelanga endizeni ehlala ibhekene ne-
isiqondiso se ilanga (elilingana nenketho yama-eksisi amabili ekulandeleleni
Izibalo ze-PV). Ngokuzithandela ungakwazi futhi bona iphrofayili ye-irradiance ecacile
(inani lethiyori le-irradiance ku ukungabi khona kwamafu).

Izinga lokushisa Le nketho ikunikeza isilinganiso sanyanga zonke sezinga lokushisa lomoya
ihora ngalinye emini.

Okukhiphayo kwethebhu yephrofayela yemisebe yansuku zonke

Ngokuqondene nethebhu yemisebe yanyanga zonke, umsebenzisi angabona kuphela okukhiphayo njengamagrafu, nakuba
amatafula amanani angalandwa ngefomethi ye-CSV, json noma ye-PDF. Umsebenzisi uyakhetha
phakathi kokuthathu amagrafu ngokuchofoza izinkinobho ezifanele:

9. Ngehora ngemisebe yelanga kanye nedatha ye-PV

Idatha yemisebe yelanga esetshenziswa yi I-PVGIS 5.3 iqukethe inani elilodwa lehora ngalinye a
isikhathi seminyaka eminingi. Leli thuluzi linikeza umsebenzisi ukufinyelela kokuqukethwe okugcwele kwe-solar imisebe
database. Ngaphezu kwalokho, umsebenzisi angaphinda acele ukubalwa kokuphuma kwamandla e-PV kokukodwa
ihora ngesikhathi esikhethiwe.

9.1 Izinketho zokufaka emisebeni yehora ne-PV ithebhu yamandla

Kukhona ukufana okuningana Ekubalweni kokusebenza kwesistimu ye-PV exhunywe kugridi
njenge kahle njengamathuluzi wokulandela umkhondo wesistimu ye-PV. In the ithuluzi ngehora kungenzeka
khetha phakathi indiza engaguquki kanye nesistimu yendiza yokulandelela eyodwa. Okwendiza engaguquki noma i
ukulandelela kwe-eksisi eyodwa i ukuthambeka kufanele kunikezwe umsebenzisi noma i-engeli eyehlelayo elungiselelwe kufanele
kukhethwe.

Ngaphandle kohlobo lokukhweza nolwazi mayelana nama-engeli, umsebenzisi kufanele khetha eyokuqala
nangonyaka odlule ngedatha yehora.

Ngokuzenzakalelayo okukhiphayo kuhlanganisa i-global in-plane irradiance. Nokho, kukhona ezinye ezimbili
izinketho zokukhipha idatha:

Amandla e-PV Ngale nketho, namandla esistimu ye-PV enohlobo olukhethiwe lokulandela umkhondo
izobalwa. Kulokhu, ulwazi mayelana nohlelo lwe-PV kufanele lunikezwe, njengoba nje okwe
ukubala kwe-PV exhunywe kugridi

Izingxenye zemisebe Uma le nketho ikhethiwe, futhi iqondile, isakazwa futhi iboniswa phansi
izingxenye zemisebe yelanga zizokhishwa.

Lezi zinketho ezimbili zingakhethwa ndawonye noma ngokwehlukana.

9.2 Okukhiphayo kwethebhu yemisebe yehora ne-PV yamandla

Ngokungafani namanye amathuluzi ku I-PVGIS 5.3, ngedatha yehora kunenketho kuphela yokuthi ukulanda
idatha ngefomethi ye-CSV noma ye-json. Lokhu kungenxa yenani elikhulu ledatha (kufika ku-16 iminyaka ngehora
values), lokho kungenza kube nzima futhi kudle isikhathi ukukhombisa idatha njenge amagrafu. Ifomethi
yefayela eliphumayo lichazwe lapha.

9.3 Qaphela ku I-PVGIS Izitembu zesikhathi zedatha

Amanani wehora we-irradiance we I-PVGIS-SARAH1 kanye I-PVGIS-SARAH2 amasethi edatha atholiwe
kusukela ekuhlaziyweni kwezithombe ezivela ku-geostationary European amasathelayithi. Nakuba, lezi
amasathelayithi athatha isithombe esingaphezu kwesisodwa ngehora, sinqume ukwenza kanjalo kuphela sebenzisa isithombe esisodwa ngehora
futhi unikeze lelo nani elisheshayo. Ngakho-ke, inani le-irradiance kuhlinzekwe ku I-PVGIS 5.3 yi
i-irradiance esheshayo ngesikhathi esikhonjiswe ku i isitembu sesikhathi. Futhi nakuba sikwenza
ukucabanga ukuthi lelo nani le-irradiance esheshayo ngabe kube inani eliyisilinganiso salelo hora, ngo
iqiniso liyi-irradiance ngalowo mzuzu.

Isibonelo, uma amanani e-irradiance eku-HH:10, ukulibaziseka kwemizuzu eyi-10 kuphuma
isathelayithi esetshenzisiwe kanye nendawo. Isitembu sesikhathi kudathasethi ye-SARAH yisikhathi lapho
isathelayithi “ubona” indawo ethile, ngakho-ke isitembu sesikhathi sizoshintsha nge indawo kanye
isathelayithi esetshenzisiwe. Okwamasathelayithi e-Meteosat Prime (ahlanganisa iYurophu ne-Afrika ukuze 40deg East), idatha
zivela kumasathelayithi e-MSG kanye ne "iqiniso" isikhathi siyahlukahluka nxazonke Imizuzu emi-5 ngemuva kwehora
ENingizimu Afrika ukuya emaminithini angu-12 eNyakatho Yurophu. OkweMeteosat Amasathelayithi aseMpumalanga, i "iqiniso"
isikhathi sihluka kusukela cishe imizuzu engu-20 ngaphambi kwehora ukuya ngaphambi nje kwehora lapho usuka
ENingizimu kuya eNyakatho. Ezindaweni zaseMelika, i-NSRDB database, nayo etholakala ku
amamodeli asekelwe kwisathelayithi, isitembu sesikhathi sihlala sikhona HH:00.

Ukuze uthole idatha evela kumikhiqizo yokuhlaziya kabusha (ERA5 kanye ne-COSMO), ngenxa yendlela i-irradiance elinganiselwe eyiyo
kubalwa, amanani wehora ayinani elimaphakathi le-irradiance elinganiselwe ngalelo hora.
I-ERA5 ihlinzeka ngamavelu kokuthi HH:30, egxile kakhulu ehoreni, kuyilapho i-COSMO ihlinzeka ngehora.
amanani ekuqaleni kwehora ngalinye. Okuguquguqukayo ngaphandle kwemisebe yelanga, njenge-ambient
izinga lokushisa noma isivinini somoya, nazo zibikwa njengamavelu esilinganiso sehora.

Ukuze uthole idatha yehora usebenzisa oen of the I-PVGIS-SARAH yolwazi, isitembu sesikhathi yisona kwe
idatha ye-irradiance kanye nokunye okuguquguqukayo, okuvela ekuhlaziyweni kabusha, kungamanani
elihambisana nalelo hora.

10. Idatha Ejwayelekile Yonyaka Wesimo Sezulu (TMY).

Le nketho ivumela umsebenzisi ukuthi alande isethi yedatha equkethe Unyaka Ojwayelekile Wesimo Sezulu
(TMY) yedatha. Isethi yedatha iqukethe idatha yehora yezinto eziguquguqukayo ezilandelayo:

Usuku nesikhathi

I-Global irradiance enezingqimba

I-irradiance evamile

Sabalalisa i-irradiance evundlile

Umfutho womoya

Izinga lokushisa le-bulb (izinga lokushisa elingu-2m)

Isivinini somoya

Indawo yomoya (amadigri ukuya kwewashi ukusuka enyakatho)

Umswakama ohlobene

I-long wave downwelling emisebeni ye-infrared

Isethi yedatha yenziwe ngokukhetha inyanga ngayinye kakhulu "ejwayelekile" inyanga iphumile kwe
isikhathi esigcwele esitholakalayo isb iminyaka eyi-16 (2005-2020) ye I-PVGIS-SARAH2. Okuguquguqukayo okusetshenziselwa ukwenza
khetha inyanga ejwayelekile kukhona i-global irradiance enezingqimba, umoya izinga lokushisa, kanye nomswakama ohlobene.

10.1 Izinketho zokufaka kuthebhu ye-TMY

Ithuluzi le-TMY linenketho eyodwa kuphela, okuyisizindalwazi semisebe yelanga kanye nesikhathi esihambisanayo
isikhathi esisetshenziselwa ukubala i-TMY.

10.2 Izinketho zokuphuma kuthebhu ye-TMY

Kungenzeka ukukhombisa enye yezinkambu ze-TMY njengegrafu, ngokukhetha inkambu efanele phakathi
imenyu yokudonsela phansi bese uchofoza "Buka".

Kunamafomethi amathathu okukhiphayo atholakalayo: ifomethi ye-CSV ejwayelekile, ifomethi ye-json kanye ne-EPW
(EnergyPlus Weather) ifomethi ifanele isofthiwe ye-EnergyPlus esetshenziswa ekwakheni amandla
izibalo zokusebenza. Le fomethi yakamuva ngokobuchwepheshe nayo i-CSV kodwa yaziwa njengefomethi ye-EPW
(isandiso sefayela .epw).

Mayelana nama-timestanps kumafayela e-TMY, sicela uqaphele

Kumafayela we-.csv kanye ne-.json, isitembu sesikhathi singu-HH:00, kodwa ibika amanani ahambisana
I-PVGIS-SARAH (HH:MM) noma ERA5 (HH:30) izitembu zesikhathi

Emafayeleni e-.epw, ifomethi idinga ukuthi okuhlukile ngakunye kubikwe njengenani
elihambisana nenani phakathi nehora elandulela isikhathi esikhonjiwe. I I-PVGIS .epw
uchungechunge lwedatha luqala ngo-01:00, kodwa lubika amanani afanayo nawoku amafayela we-.csv kanye ne-.json kokuthi
00:00.

Ulwazi olwengeziwe mayelana nefomethi yedatha yokuphumayo itholakala lapha.

OKUQUKETHWE IKHASI