Isijikelezi-langa sethu sikhaya kwiziganeko ezingenakubalwa zemozulu, uninzi lwazo ziyimveliso yokujikeleza kwamandla angaphakathi nangaphandle abetha iplanethi esuka eLangeni, enye yazo, eyaziwayo, yile: Umoya. Le meteorology yinto enomdla kakhulu kwaye ifanelekile, kodwa uyazi Yintoni umoya kwaye ulinganiswa njani?
Umoya yinto yendalo enokuthi kwiimeko ezininzi asiyiqapheli, inokuba kufutshane njengoko ikude. imiba yemizuzwana, kwimvelaphi yengcaciso yezinto zesi sijikelezi-langa, kwakukholelwa ukuba umoya wawungomnye wezakhi ezine, apho yonke into esemhlabeni, enoba i-organic okanye ayikho, yenziwa.
Umoya unokwenza umonakalo eMhlabeni
Nangona kunjalo, le yingqikelelo encinci kakhulu yesenzeko somoya. Kukho iindlela ezininzi zokuyixabisa le meteor. Kanye kunokuba yi-caress ethambileyo edibanisa iinwele zakho kunye tyibilika phantsi ubuso bakho kwaye, ngamanye amaxesha, inokukuvala ngokukhawuleza ngokwaneleyo ukuba ikuthabathe amakhulu eemayile ukunqumla esibhakabhakeni.
Ngokwale ngqiqo, ngokomlinganiselo wesantya sawo sinokuthi umoya unokuba ngumhlobo othe-ethe okubulisa kuhambo lwakusasa, kwakunye nerhamncwa elinoburhalarhume elingenakunqandeka elinokuthabatha iimoto, izindlu, neefama endleleni yalo. . Okanye ukuba awuyibonanga inkomo ephaphazelayo engaqhelekanga kwiinkanyamba.
Yintoni isenzeko somoya?
Umoya kukuhamba kweegesi kubukhulu obukhulu. KwiPlanethi yoMhlaba le ntshukumo yintshukumo yomoya oguquguqukayo kunye nongaguqukiyo ngaphakathi kwiatmosfera, ojikeleza kwindawo enye. intshukumo ethe tyaba. Ezinye iimeteorologists zichaza isenzo sayo ngenxa yembuyekezo yamanqanaba ahlukeneyo oxinzelelo lwe-atmospheric phakathi kwamanqaku amabini amisiweyo.
Ukusuka kwinzululwazi yezemozulu, isenzeko somoya simiselwa ngokwamandla azo kunye necala apho zisuka khona. Ukunyuka ngesiquphe kwisantya somoya ixesha elifutshane kubizwa ngokuba ukugqabhuka.
Imimoya evuthuza ngamandla kunye nesantya esiphezulu kodwa eyexesha eliphakathi, malunga nomzuzu omnye, iyabizwa iziqhulo. Imimoya yexesha elide inamagama ahlukeneyo, ngokunxulumene namandla awo aphakathi, afana, umzekelo, impepho, isaqhwithi, isaqhwithi, inkanyamba kunye nenkanyamba.
Esi siganeko sezemozulu singenzeka kwimilinganiso eyahlukeneyo eyaziwayo: ukusuka kwimisebenzi yezaqhwithi enokuhlala amashumi emizuzu, kunye nempepho ehamba ngokuthe ngcembe eveliswa kukufudumeza okwahlukeneyo kummandla wamatye omhlaba, yathi imimoya inokuhlala iiyure eziliqela. nkqu imimoya yehlabathi, ezisisiphumo somahluko wokufunxa amandla elanga phakathi kwe iindawo ezahlukeneyo ze-geoastronomical Zomhlaba, yintoni ekuqaleni esasiyibiza njengamandla angaphandle.
Kukho iindlela ezahlukeneyo zokuvelisa umoya. Kuxhomekeke kumjikelezo we-atmospheric isikali esikhulu ziyimimoya eveliswa kukufudumala okungafaniyo komphezulu womhlaba ngokuxhomekeke kwisibanzi, kunye ne-inertia kunye ne-centrifugal force eveliswa yintshukumo yokujikeleza kweplanethi.
Ngendlela efanayo kwiindawo ezitshatyalaliswayo, ukujikeleziswa kweentlobo ezahlukeneyo zoxinzelelo lwe-thermal ngaphezu komhlaba kunye amathafa aphezulu inamandla okuqhuba ukujikeleza kweemonsoon ezinkulu.
Ngakolunye uhlangothi, kwiindawo eziselunxwemeni, umjikelo oveliswa phakathi kwempepho yomoya kunye nolwandle / impepho yasemhlabeni unokunika iimpawu kwimimoya yendawo, nangona kunjalo, kwiindawo ezahlukeneyo zokunceda, imimoya evela kwiintlambo kunye neentaba inokumisela imimoya yendawo.
Funda ngakumbi ngalo mbandela apha: 4 IINYANISO EZOMANGALISAYO NGOMxhuzulane EMZINDI WOMHLABA
ukufuduswa yomoya kwindawo esezantsi I-atmosfera, indawo ebizwa ngokuba yi-troposphere, yeyona nto ibonwa ngabantu, lo moya unezinto ezimbini:
into ethe nkqo, ehamba iikhilomitha ezili-10 okanye ngaphezulu kwaye intshukumo yayo ezantsi okanye ephezulu ihlawulela umoya othe tye; kunye nendawo ethe tye, efikelela kumakhulu eekhilomitha kwaye yeyona ifanelekileyo kwezi zimbini
Ukuba siqwalasela ngononophelo inkanyamba sinokuziqonda ezi ngqikelelo, kuba ngelixa isakhiwo sayo esijikelezayo siqala ukujikeleza ngesantya esiphezulu kakhulu, ukuya kwinqanaba lokutshabalalisa, kwaye isantya esifanayo siyancipha njengoko sihamba. umoya uyehla, ngenxa yokuba imilinganiso yekhowuni iyanda endaweni ebanzi kunaleyo imxinwa.
Yintoni umsebenzi weAnemometer
Ezinye izixhobo ziphucukile kunezinye
Ukuqwalasela ukuba umoya ungomnye wamandla amakhulu endalo, anokuba luncedo olukhulu kwizinto eziphilayo, umoya unokuba namandla amakhulu atshabalalisayo, ngoko imfuno yokulinganisa ubunzulu bawo yinto ebalulekileyo.ukufunda kunye nokuqikelela.
Fumana ngakumbi ngokufunda eli nqaku: I-10 IMICANDELO YOBUSI ONGENAKO UNGAYIPHOSEKI
Kule meko i i-anemometer o ianemograph Sisixhobo sokulinganisa imozulu, esisetyenziselwa ukulinganisa isantya somoya kwaye ngaloo ndlela sincede kuqikelelo lokutshintsha kwemozulu. Esi sixhobo sikwanazo nokusebenza okukhulu ekubalekeni kobunzima kuneenqwelomoya, ngale ndlela kumiselwa uluhlu olukhuselekileyo lwenqwelomoya kunye neyona ndlela inokuthenjwa.
Kwizifundo zemozulu, ii-anemometers zekomityi okanye ipinwheel zisetyenziswa ikakhulu, ezimile okwesingqusho esincinci, esinamaphiko amathathu anekomityi amandla asebenzayo zomoya ngexesha lokungqubana nazo, zisenza ukujikeleza. Ngale ndlela, inani leempuphu ezirekhodwa zizixhobo zingafundwa ngokuthe ngqo kwi-counter okanye zirekhodwe kwiphepha lephepha, elibizwa ngokuba yi-anemogram.
Kukwakho nezixhobo ezilinganisa isantya somoya ezingenagrafu ephepheni, kuba idatha exeliweyo irekhodwa kwaye ihlalutywe yikhompyutha, enokuqikelela utshintsho oluthile kunye nokwahluka emoyeni okunceda kuqikelelo oluchanekileyo lwemozulu. Ezi zixhobo zeze-elektroniki.
Yandisa olu lwazi apha: ZENZENJANI UHAMBO LOKUQALA NGENANI LOKUYA ETHUBENI
Icala oya kulo umoya likwayinto ebalulekileyo yokulinganisa malunga nokutshintsha kwemozulu, kwizinto ezithile imihla okanye amaxesha onyaka lonyaka, kule meko kusetyenziswa i-vane yemozulu, ebonisa icala apho umoya uvela khona, ezi datha zirekhodwa kwindawo yazo yekhadinali.
Esinye isixhobo esisebenza ukunika isalathiso esisisiseko sesalathiso kunye nobunzulu be-miso yinto ebizwa ngokuba yi. isaqhwithi. Esi sixhobo sobuchwepheshe obuphantsi sisetyenziswa kakhulu kwizikhululo zeenqwelomoya. Luhlobo lwetyhubhu yelaphu evulekileyo kumacala amabini kwaye ixhonywe ngaphezu kwepali.
Ngokuxhomekeke kwizinto, ubunzima kunye neemeko zesixhobo, silinganiswe ukurekhoda utshintsho emoyeni.Ukuba akukho moya, umkhono uhlala ume nkqo, ujinga kwipali yawo. Xa kuvuthuza umoya, ibekwe kwindawo engaphezulu okanye engaphantsi kwe-oblique, kwaye kwimeko apho umoya unamandla kakhulu, umkhono uya kuhlala uphakanyiswe ngokuhambelana nomhlaba.
Umanduleli wesikali somlinganiselo woMoya
Ukumisela ubunzulu bomoya, isikali somlinganiselo ngokugqwesileyo yile: Beaufort. Lo mlinganiselo wenziwa ngu UMhlekazi uFrancis Beaufort, owayeligosa lomkhosi wasemanzini wase-Ireland kunye nomenzi we-hydrographer, malunga nonyaka ka-1805. Ngonyaka we-1800 amagosa omkhosi wasemanzini ayesoloko eqwalasela imozulu, kodwa ayengenasikali somlinganiselo njengoko kunjalo kwaye imilinganiselo yayixhomekeke kakhulu ukuba ingaqondwa. yona.