Isimo sezulu ibalazwe Ukraine ONLINE
Imephu entsha yesibikezelo sezulu sesathelayithi ye-Ukraine 🔋 isebenza ngesikhathi sangempela ⚡ONLINE futhi ibonisa 🌡️izinga lokushisa lomoya, ukunyakaza 🌈 kobuningi bomoya, isivinini kanye nendlela 💨 yemimoya, isibikezelo sezulu (☔ imvula, 🌩️ ukuduma kwezulu noma 🌩️ iqhwa), . I-radar yesimo sezulu ibonisa ℹ️ ulwazi mayelana nezimo zezulu kuwo wonke amadolobha, amadolobhana nezifunda zase-🇺🇦 Ukraine namuhla, kusasa, 🗓️ izinsuku ezilandelayo, kanye nesikhathi eside. 👁️ Bona 🔝 isibikezelo sezulu esinembe kakhulu ☀️☁️☂️ sesimo sezulu e-Ukraine izinsuku ezingu-3, izinsuku ezingu-5, isonto (izinsuku ezingu-7), izinsuku ezingu-10 noma inyanga. 🗺️ Imephu yesimo sezulu esebenzisanayo isebenza 👍 emithonjeni yedatha ethembekile enikeza ulwazi lwakamuva 🌦️ lwesimo sezulu kusetshenziswa ubuchwepheshe obusha 🖥️ bedijithali nobumkhathi 🚀COSMO-EU ngokusekelwe ku-ICON yemodeli yokubikezela isimo sezulu enembe kakhulu. Ukuze uthole 🎯 ukuzimisela okunembile kakhulu kwezimo zezulu 📶, uhlelo lusebenzisa izinkomba zamanje zezindawo zokubuka 🔭 kanye neziteshi zesimo sezulu 📻 ze-Ukrainian Hydrometeorological Center (UkrHydrometeorological Center). Landela isimo sezulu sase-Ukraine ku-inthanethi usebenzisa imephu yesibikezelo esiku-inthanethi esiyingqayizivele esinikezwe isevisi yoWindy.
Isimo sezulu ibalazwe Ukraine
*Imodeli yokulandelela isimo sezulu ye-ICON-EU esetshenziswe kumephu i-matrix enokulungiswa okuphezulu ethuthukiswe 🇩🇪 yinkampani yaseJalimane i-DWD. Imodeli yesimo sezulu ye-ICON eguquguqukayo, eyakhelwe kumanethiwekhi e-neural, ingenye yamamodeli esimanjemanje esibikezelo sezulu emhlabeni 🌍, enikeza imiphumela emihle kakhulu yesifunda 🇪🇺 Europe, kuhlanganisa nase-🇺🇦 Ukraine. I-ether yedatha edluliselwe kumephu futhi yacutshungulwa 🤖 ngobuhlakani bokwenziwa ivamise ukusetshenziselwa ucwaningo nezinjongo zesayensi ezikhungweni ezithuthukile zesimo sezulu seplanethi yethu.
Ukunakwa❗ Imiyalelo 📑 enemininingwane yokuthi ungasebenzisa kanjani kahle imephu yesibikezelo sezulu esiku-inthanethi 🔆☁️☔ yase-Ukraine (imenyu yokudonsela phansi 📋 enenketho yokushintsha izendlalelo kumephu yedijithali isekhoneni eliphezulu kwesokudla, ngenhla kwezinkinobho zokusondeza ➕➖):
🌡️ Izinga lokushisa. Ngokuzenzakalelayo, imephu yesimo sezulu yesathelayithi yase-Ukraine ibonisa izinga lokushisa le-ambient kumodi yesithombe esishisayo. Ngokuya ngombala wendawo ethile yemephu, ukusatshalaliswa kwezinga lokushisa endaweni efundiwe kungabonwa. I-thermogram iboniswa kumephu ngombala ohambisanayo ku-spectrum kusukela emazingeni okushisa abandayo kakhulu ukuya emazingeni okushisa afudumele (violet-yellow-orange-red). Kanye ne-thermography, ungqimba lwesiqondiso somoya nesivinini kukhiqizwa kabusha. Ukuhamba kwemisinga yomoya kubonisa zonke izinqubo zemisinga yomoya ekujikelezeni komkhathi. Ngezansi, ibhodi yolwazi enedatha yamanje yesimo sezulu endaweni ekhethiwe iyaboniswa, okokuqala inhloko-dolobha yase-Ukraine imisiwe - idolobha laseKyiv (ungakhetha elinye idolobha noma idolobhana, futhi uthole noma iyiphi enye indawo bese ubeka ichashazi imephu endaweni oyifunayo). Ithebula libonisa izilinganiso zesimo sezulu kusukela manje, nesinyathelo sokurekhoda imiphumela yehora lokugcina lesikhathi. Izithombe ezikhethekile emugqeni wetafula lesimo sezulu (ilanga elicacile, ifu, ifu lemvula, ifu lesiphepho, ilanga elimnyama, eliguqubele, ifu elineqhwa, izigaba zenyanga nokunye) zikhumbuza isimo sesibhakabhaka. Bese, ngamunye ngamunye, kuba nemigqa elandelayo: izinga lokushisa - ngamadigri Celsius (°C), imvula “imvula” — ngamamilimitha (mm), umoya nezivunguvungu — ngamakhilomitha ngehora (km/h), isiqondiso somoya — umcibisholo ubonisa indlela okuyiyonayona yemimoya (umoya waseningizimu, umoya wasenyakatho, umoya wasempumalanga, umoya wasentshonalanga nokunye okuhlukahlukene okunjengomoya waseningizimu-mpumalanga, umoya osenyakatho-ntshonalanga, njll.). Kukhona inketho yokushintshela kwamanye amayunithi okubonisa (amadigri Celsius - °C, amadigri Fahrenheit - °F), (amamilimitha - mm, amayintshi - in), (amakhilomitha ngehora - km/h, amafindo - kt, amaphuzu eBeaufort - bft, amamitha ngomzuzwana - m/s, amamayela ngehora - mph). Ukuze ushintshe, udinga nje ukuchofoza kupharamitha edingekayo, futhi inani lokulinganisa lizoshintsha. Isibikezelo sezulu esiqondile sesathelayithi esisetafuleni siyatholakala ukuze sibukwe namuhla + izinsuku ezingu-5 (ezinhlanu), empeleni isimo sezulu sinikeza ithuba lokuthola ulwazi olubaluleke kakhulu mayelana nokuthi isimo sezulu sizoba njani e-Ukraine ngesonto elizayo. Ngokuphenya (ukuhambisa) izinsuku zeviki (ikhalenda) ngekhesa/iphedi yokuthinta kwesokunxele, kuzovela iwindi ekugcineni kohlu elinolwazi mayelana nale ndawo ebikezelwe kanye nedatha eyengeziwe (izixhumanisi zendawo ngqo - i-latitude nobude, indawo yesikhathi yesifunda, isikhathi esiqondile sokuntwela kokusa "ukuphuma kwelanga ") nokushona kwelanga "ukushona kwelanga", ukuhwalala "ukuwa kobumnyama", ukuphakama kwendawo ngaphezu kolwandle ngamamitha-m kanye nezinyawo-ft). Uma uhambisa ubuso bewashi kwesokudla, ungabona ukuthi isimo sezulu e-Ukraine sizoshintsha kanjani ebalazweni elinomfanekiso wokubuka okushisa. Lo msebenzi ikuvumela ukuthi ubonise ngeso lengqondo izinguquko zesimo sezulu sase-Ukraine engxenyeni yesikhashana ekhethiwe (ngehora) noma isikhathi eside ngezinsuku zekhalenda zesonto (ngoMsombuluko, ngoLwesibili, ngoLwesithathu, ngoLwesine, ngoLwesihlanu, ngoMgqibelo, ngeSonto).
🛰️ Isathelayithi. Kule modi yokuqapha yesikhathi sangempela, ungabuka ukusakazwa kwe-inthanethi kwesimo samanje sokuguqubala phezu kwe-Ukraine kusuka kumasathelayithi e-geostationary ngokuqondile emkhathini. Esikrinini sokuqala, isendlalelo sesathelayithi yomthombo sisethwe ukuze sithi OKULUMHLOKO (okuzenzakalelayo). Le spectrum eluhlaza okwesibhakabhaka isebenza ngemibala eminingi engezwe ngokukhethekile ukuze kube lula futhi kucace kubasebenzisi ukuthi bacabangele isimo esisemoyeni, ngaphandle kokudidwa imingcele yamazwe, izilwandle, imifula namachibi, okungahlangana ndawonye lapho bebuka izithombe zesathelayithi. ngekhwalithi yawo yasekuqaleni. Uma ushintshela ku-VISIBLE layer (bheka izinkinobho ezingezansi BLUE, VIS, INF), isithombe se-spectrum ebonakalayo sizovela, okungukuthi, yonke into izobukeka "njengoba injalo" ngokuqondile kwikhamera yesathelayithi. Uma ucindezela inkinobho ethi ▶️Play, ungabuka ividiyo yangempela, ulande okurekhodiwe kwesathelayithi kwakamuva, okubonisa ukunyakaza kwamafu emahoreni angu-2 adlule. Isendlalelo sesithathu sesathelayithi ye-INFRA+ simemezela izinga lokushisa elikhanyayo eliye laba phezulu kwamafu e-Kelvin (K). Lelizinga lokushisa linikeza ukuqonda kokuphakama kwemingcele engenhla yamafu futhi lixwayisa ngengozi yokuduma kwezulu okukhulu. Iziqongo zamafu eziphakeme ngokuvamile zikhiqiza ukuduma kwezulu nezinye izimo zezulu ezinzima ezifanayo. Lesi sendlalelo se-infrared sinikeza umbono wokuthi ukubanda kwezinga lokushisa, kuphakama ifu, ngakho-ke kungenzeka kube uhlobo lwefu lwe-cumulus oluhlotshaniswa nokuduma kwezulu, kodwa amafu e-cirrus nawo angamafu aphezulu nabandayo futhi awahlobene nhlobo nokuduma kwezulu. Ngaphambi kokwenza iziphetho zokugcina esibikezelweni sezulu, kuyadingeka ukuhlola amanye amapharamitha, isibonelo, vula isiteshi esibonakalayo VISIBLE ukuze ubone ifu eliwugqinsi noma cha. Uma kungenjalo, khona-ke ebangeni le-infrared amafu anjalo cishe angamafu e-cirrus.
💧 Imvula, ⚡ ukuduma kwezulu. Imephu yokubikezela imvula nokuduma kwezulu yase-Ukraine iyisendlalelo esibaluleke kakhulu nesiwusizo ekwenzeni isibikezelo sezulu esinembe kakhulu, ukuhlela noma yiliphi ibhizinisi, ukuzijabulisa, uhambo noma uhambo oluzayo. Emuva elimpunga lemephu yase-Ukraine, amabala anombala aphawula izindawo lapho lina khona njengamanje, isichotho, ukuduma kwezulu (isixwayiso sesiphepho sombani), ukuduma kwezulu, iqhwa elinamandla, noma kukhona isiphepho esishisayo (umoya onamandla iqhwa ezindaweni asemaqeleni, ngezinye izikhathi ibizwa ngokuthi buran). Ngokuhambisana nongqimba lwemvula nokuduma kwezulu, ukugqwayiza komoya kuyaboniswa. Izindawo zemvula zingahluka ngombala ukusuka kokuluhlaza okwesibhakabhaka kuye kokunsomi, kuye ngenani lemvula eliwayo, likalwa ngamamilimitha (mm). Imvula encane noma imvula enamandla ibukeka njengendawo enombala ongenalutho emboze indawo. Uma, lapho kuhlolwa indawo ethile, izimpawu eziyisixwayiso ezengeziwe zimakwe kungemuva elinemibala, isibonelo, izithombe ezincane ezibonisa umbani, amakhekheba eqhwa, amaconsi - lokhu kusho ukuthi kule ndawo ethile yomkhathi kukhona ukunqwabelana kwemvula noma iqhwa emkhathini. amahora angu-3 edlule. Izimpawu zombani ezikhanya kalufifi ngendlela encishisiwe zibonisa ukuduma kwezulu okuncane, kuyilapho izimpawu zombani ezikhanyayo, ezikhulisiwe nezicwebezelayo zibonisa ukuduma kwezulu okukhulu okunamandla amakhulu. Okunye imvula ibonakala ngendlela efanayo, isibonelo, iqhwa elinzima - amakhekheba eqhwa akhanya kancane futhi abe mkhulu. Kunezikhathi lapho imvula exubile ibonwa khona, ingaba yiqhwa, kwesinye isikhathi iwe ngendlela yezinhlayiya zeqhwa elincibilikayo, ezihlukaniswa njengeqhwa noma iqhwa. Imvula efanayo imelelwa izithonjana ezimbili ezincikene zamakhekheba eqhwa namaconsi. Kwezinye izimo, kukhona uhlobo oluxubile nosayizi wamakhekheba eqhwa, lapho izimpawu zeqhwa ezincane zivela eduze nezinkulu. Lokhu kusho ukuthi kuneqhwa elinzima nelilula ngesikhathi esisodwa. Ukwethula inkinobho ethi ▶️Play kuzoskrola kwisibikezelo sezulu semvula, imvula, ukuduma kwezulu nokuwa kweqhwa izinsuku ezingu-7 ezizayo futhi kuzokusiza wenze isibikezelo sezulu esinembe kakhulu iviki lonke mayelana nokuhamba kwamafu emvula (ukuduma) endaweni yase-Ukraine.
🌪️ Umoya. Imephu yomoya yase-Ukraine idlulisa idatha entsha ku-inthanethi ngesivinini nendlela yomoya kuwo wonke amadolobha, amadolobhana nezifunda. Imephu ekuboneni okuguquguqukayo ikhiqiza kabusha ithrafikhi yomoya yangempela, engasiza ukubikezela inkambiso yentuthuko yesimo sezulu esihlobene nomoya endaweni ocwaningwayo. Ukugxila namandla omoya kubalwa kumakhompuyutha amakhulu abonisa imifudlana egqwayizayo yomsebenzi womoya kumephu esebenzisanayo. Imephu yomoya ikhombisa ngokusobala isigqi sesivinini esikhulu nesiqondiso samajethi omoya anazo zonke izinhlobo ze-eddies ezingase zithinte izivunguvungu nama-anticyclone avela ku-troposphere. Ukusetshenziswa kwalolu lwazi kuzosiza ngempela ukudala isithombe esiphelele sezinqubo zesikhathi esizayo zomkhathi kanye nesibikezelo sezulu. Imephu yomoya (umoya) enohlelo lombala lokudlulisa isivinini semisinga yomoya bukhoma ibonisa ngemibala ehlukene izindawo ezinomoya onamandla noma obuthakathaka kumayunithi ajwayelekile okulinganisa, amakhilomitha ngehora - km/h. Lolu lwazi oluwusizo lungabika izinguquko zesimo sezulu eziphuthumayo, njengokubonisa isiphepho seqhwa esizayo noma ukukhombisa umoya onamandla kakhulu (imimoya ebhudlayo), iziphepho, iziphepho, izivunguvungu, izivunguvungu, noma iziphepho. ▶️Inkinobho yokuqala isibikezelo somoya sase-Ukraine izobonisa yonke imizila engenzeka kanye nesivinini sokushintsha kwezindimbane zomoya ezinsukwini ezi-5 ezilandelayo. Izikhungo zokuhlaziya zamasevisi esimo sezulu zixwayisa mayelana nezinhlekelele zemvelo ezingaba khona nezinhlekelele ezisekelwe ekuqashweni kwaleyo datha.
🌩️ I-radar yesimo sezulu (i-radar yesimo sezulu). Imephu ye-radar yesimo sezulu yase-Ukraine isebenza kubuchwepheshe be-dBZ, ngosizo lwamadivayisi akhethekile we-meteorological Doppler ahlala eqapha futhi ekala imvula (imvula, iqhwa) emkhathini. Izisetshenziswa zesimo sezulu serada ye-dBZ zibonisa ngamadecibels ukuhlolwa kokubonakaliswa kwento yesimo sezulu kanye namandla emvula endaweni ethile yocwaningo. I-radar ye-dBZ isiza ukuqoqa amasignali mayelana nemvula, iqhwa noma isichotho, futhi iphinde ihlole ukuqoqwa kwamanzi emafwini, ibikezela lokho okubizwa ngokuthi "amanzi amafu". Okwamanje, ukumbozwa kwalesi radar kuhlaziya ingxenye encane yensimu, ikakhulukazi izifunda ezisentshonalanga ye-Ukraine (Lviv, Volyn, Zakarpattia, Ivano-Frankivsk, Chernivtsi), kuhlanganise nesifunda esiseningizimu, esimelelwe esifundeni sase-Odesa.
Ukusebenza okuyinhloko kwale mephu yobuchwepheshe obuphezulu enezibikezelo zesimo sezulu ezinembile akugcini ngezendlalelo ezidume kakhulu ezibalwe ngenhla. Ukubuyekezwa kufake kuphela i-TOP-5 esetshenziswa kakhulu futhi izici ezidingekayo ukuze zisetshenziswe ngempumelelo nsuku zonke noma ukusebenza ngemephu yesibikezelo sezulu e-Ukraine ngobuningi bezivakashi. Ngokuskrolela phansi imenyu, ungathola ezinye izinketho eziningi ezithakazelisayo, ozisebenzisayo 🆓 MAHHALA ngokuphelele, uthole ulwazi olubalulekile, olubalulekile noluwusizo ℹ️ olutholakalayo ngenxa entsha. IT- ezobuchwepheshe. Phakathi kwamamephu amaningi, kufanelekile ukugqamisa okokuqala 🆕 amakhono amasha ahlukile futhi amangalisayo ezinye izendlalelo zenethiwekhi ye-neural:
⚠️ Ukugxila kwe-CO. Imephu ye-CO (i-carbon monoxide, i-carbon monoxide, i-carbon monoxide) amazinga e-Kyiv nase-Ukraine. I-Carbon monoxide igesi engenambala, engenaphunga futhi engenambitheki futhi eminyene kancane kunomoya. Izinga lokugxila kwe-CO ku-troposphere likalwa ngesistimu ebizwa ngokuthi "Izingxenye ngebhiliyoni ngevolumu" (PPBV). Imililo yehlathi, intuthu nezinye izehlakalo ezingcolisa umoya kungaba umphumela wokwanda kokugcwala kwegesi engu-CO.
💨 Inqwaba yothuli. Imephu ikhombisa izinga lothuli emoyeni wase-Ukraine. Ngokuvamile uthuli lwakhiwe izinhlayiya ezisemkhathini ezivela emithonjeni ehlukahlukene, njengenhlabathi, izingwadule, uthuli olupheshulwa ngumoya, ukuqhuma kwentaba-mlilo, nokungcoliswa komoya. Izinga lokugxila kothuli liboniswa ngama-micrograms (isigidi esisodwa segram) kuyi-cubic mitha yomoya ngayinye noma µg/m3. Izindawo zothuli e-Ukraine ziboniswa kumephu ukusuka kokumpunga kuye kokunsundu ngokumnyama.
☣️ CHA₂. Imephu yokusatshalaliswa kwegesi enobuthi NO₂ - i-nitrogen oxide e-Ukraine. I-NO₂ (i-nitrogen dioxide) igesi ebangela izinkinga zokuphefumula ezihambisana nokuncipha kokusebenza kwamaphaphu. Imithombo emikhulu ye-NO2 yizinjini ezivuthayo zangaphakathi, izitshalo zamandla ashisayo (umthombo: Wikipedia). Amazinga we-NO₂ avezwa ngo-µg/m³, futhi ukuqagela kumephu kuhambisana namanani angaphezulu. Ngokusho kwe-WHO kanye ne-EU, isilinganiso sehora se-MAC (umkhawulo wokuhlushwa ovumelekile) we-NO₂ emoyeni imizuzu engu-60 (ihora elingu-1) sisethwe ku-200 µg/m3, kodwa akufanele seqiwe ngaphezu kwamahora angu-18 ngonyaka. Izinkomba ezihlelelwe ukuqaliswa e-EU ngo-January 1, 2030 ziyi-200 µg/m3, kodwa leli zinga alikwazi ukudlula ngaphezu kokukodwa ngonyaka. Le nkomba ihlanganiswa kucatshangelwa isibikezelo se-CAMS EU yesifunda samamodeli amaningi. Ngenxa yokuxazululwa okuvundlile kwezinhlelo ezisetshenziswa yi-CAMS, akunakwenzeka ukucabanga ngemiphumela yendawo ngenxa yokusondelana kwemithombo, isibonelo, umgwaqo onethrafikhi enkulu noma imboni yezimboni. Izibikezelo ze-NO₂ zihambisana nalokho okubizwa ngamavelu "angemuva". Amazwe anemithetho ehlukene mayelana namazinga esixwayiso kanye nesaziso esiphuthumayo somphakathi mayelana nokudlula amazinga avumelekile okungcoliswa komoya.
⏲️ Ingcindezi. Imephu yokucindezela komkhathi e-Kyiv nakuyo yonke i-Ukraine. I-barometer eku-inthanethi ikuvumela ukuthi uthole mayelana nengcindezi yamanje kunoma yiliphi idolobha, idolobhana noma isifunda sase-Ukraine. ISEXWAYISO! Umfutho womoya ojwayelekile (inani elimaphakathi) ngu-1013,25 hPa (hPa) noma u-760 mm Hg. Ukuchezuka kusuka kulesi silinganiso kubonisa umfutho womoya ophansi noma ophezulu. Ukucindezela okuphansi kakhulu noma okuphezulu kungabangela izinkinga zempilo, ikakhulukazi kubantu abanezifo zenhliziyo, ngisho nakubantu abanempilo, izinguquko ezingazelelwe zokucindezela "ukweqa" zingandisa ingozi yekhanda kanye nezinye izifo (ubuthongo, ukucasuka, ukukhathala). Uma uchofoza indawo oyithandayo, ungathola ingcindezi yamanje kunoma yisiphi isifunda noma indawo. Isikali sombala esingezansi sifana nobude bekholomu ye-mercury ku-barometer yesifunda esithile sohlelo lwamazwe ngamazwe lwamayunithi - i-hPa. Umfutho we-atmospheric, obuye ubizwe nge-barometric pressure, ukucindezela okungaphakathi komkhathi womhlaba. Ezimweni eziningi, ukucindezela komkhathi kuhambisana eduze nokucindezela kwe-hydrostatic okubangelwa isisindo somoya ngaphezu kwephuzu lokulinganisa. I-Mean Sea Level Pressure (MSLP) umfutho womoya ophakathi nendawo.
🔔 Izaziso zesimo sezulu (izixwayiso zesimo sezulu). Imephu yezixwayiso ezibalulekile zesimo sezulu e-Ukraine nakwamanye amazwe aseYurophu. Izixwayiso zesimo sezulu zingaba izinhlobo ezintathu: isimo sezulu esimaphakathi (yellow), isimo sezulu esinamandla (umbala owolintshi), isimo sezulu esibi (bomvu). Uma isimo sezulu sikhona njengamanje noma sizoba phakathi kwemikhawulo evamile, indawo yezwe ivele ibonakale ngokumpunga nje kungekho zimpawu ezengeziwe. Idatha idluliswa yi-Ukraine Hydrometeorological Center (Ukrhydromettsentr) kanye nezinye izinhlangano zezulu zezulu ngendlela ethi "CAP Isaziso".
Bona eminye imininingwane ethokozisayo newusizo kuphothali: