Iplanethi yethu iyikhaya lezimo zezulu ezingenakubalwa, eziningi zazo eziwumkhiqizo wokujikeleza kwamandla angaphakathi nangaphandle ashaya iplanethi esuka eLangeni, enye yazo, eyaziwa kakhulu, ithi: The Wind. Lesi simo sezulu siyiqiniso elinelukuluku kakhulu futhi elifanele, kodwa uyazi Uyini umoya futhi ulinganiswa kanjani?
Umoya yinto yemvelo esingayiboni ezikhathini eziningi, ungasondelana njengoba uqhelelene. izindaba zemizuzwana, emsuka wencazelo yezinto zeplanethi yethu, kwakukholelwa ukuthi umoya ungenye yezakhi ezine, okwakhiwa kuzo zonke izinto eziseplanethini engumhlaba, kungakhathaliseki ukuthi izinto eziphilayo noma cha.
Umoya ungadala umonakalo eMhlabeni
Kodwa-ke, lokhu kungumqondo olinganiselwe kakhulu wesenzo somoya. Kunezindlela eziningana zokwazisa le meteor. Kanye kungaba i-caress emnene ekama izinwele zakho futhi ishelela phansi ngobuso bakho futhi, ngezinye izikhathi, ingavala kuwe ngokushesha ngokwanele ukukuthatha amakhulu wamakhilomitha unqamule esibhakabhakeni.
Ngalo mqondo, ngokwesilinganiso sejubane lawo singasho ukuthi umoya ungaba umngane othambile okubingelela ohambweni lwasekuseni, kanye nesilo esinonya esingenakuvinjwa esingathatha izimoto, izindlu, namapulazi endleleni yawo. . Noma uma ungazange uyibone inkomo endizayo engavamile ezivunguvungwini.
Iyini isenzakalo somoya?
Umoya ukugeleza kwamagesi ngama-magnitude amakhulu. Eplanethini enguMhlaba lesi senzo siwukuhamba kwezixuku eziguquguqukayo nezingashintshi zomoya emkhathini, ozungeza endaweni ezungezile. ukunyakaza okuvundlile. Ezinye izazi zezulu zichaza isenzo saso ngenxa yokunxeshezelwa kwamazinga ahlukene okucindezela komkhathi phakathi kwamaphoyinti amabili anqunyiwe.
Kusukela kusayensi yesimo sezulu, isimo semimoya sinqunywa ngokwamandla ayo kanye nesiqondiso esivela kuso. Ukwenyuka okungazelelwe kwesivinini somoya isikhathi esifushane kubizwa ukuqhuma.
Imimoya enamandla amakhulu nesivinini kodwa yesikhathi esimaphakathi, cishe umzuzu owodwa, iyabizwa iziqhwaga. Imimoya yesikhathi eside inama-nomenclature ahlukahlukene, maqondana namandla ayo amaphakathi, njengokuthi, isibonelo, umoya, isiphepho, isiphepho, isiphepho kanye nesishingishane.
Lesi simo sezulu singenzeka ngezilinganiso ezihlukahlukene ezaziwayo: kusukela emisebenzini eneziphepho engathatha amashumi emizuzu, kanye nomoya ohelezayo kancane kancane obangelwa ukushisa okuhlukahlukene kwendawo enamatshe omhlaba, yathi imimoya ingahlala amahora amaningana. ngisho imimoya global, okuyinto umphumela umehluko ukumuncwa amandla elanga phakathi izindawo ezahlukene ze-geoastronomical Zomhlaba, lokho ekuqaleni esasikubiza ngokuthi amandla angaphandle.
Kunezinhlobo ezahlukene zokukhiqiza umoya. Kuye ngokujikeleza komkhathi isikali esikhulu ziyimimoya ekhiqizwa ukushisa okuhlukile kobuso bomhlaba kuye ngokuthi i-latitude, kanye namandla e-inertia kanye ne-centrifugal akhiqizwa ukunyakaza okujikelezayo kweplanethi.
Ngendlela efanayo ezindaweni ezishisayo, ukujikeleza kwezindawo ezishisayo ezihlukene ngaphezu komhlabathi kanye amathafa aphakeme inamandla okushayela ukujikeleza kwama-monsoon amakhulu.
Ngakolunye uhlangothi, ezindaweni ezisogwini, umjikelezo okhiqizwa phakathi komoya ohelezayo nolwandle/umoya ovunguzayo wezwe unganikeza isimilo emimoyeni yasendaweni, nokho, ezindaweni zokuphumula okuhlukahlukene, imimoya evela ezigodini nezintaba inganquma imimoya yendawo.
Funda kabanzi ngesihloko lapha: AMAQINISO 4 AMANGALISAYO NGEMANDLA ENGAPHEZULU ESIKHATHINI SOMHLABA
ukufuduka womoya endaweni engezansi Umkhathi, indawo ebizwa ngokuthi: troposphere, iyona ebona kakhulu abantu, lo moya unezici ezimbili:
isici esime mpo, ehamba amakhilomitha ayi-10 noma ngaphezulu futhi ukunyakaza kwayo phansi noma phezulu kunxephezela umoya ovundlile; kanye nesici esivundlile, esifinyelela emakhulwini amakhilomitha futhi esifaneleka kakhulu kokubili
Uma siqaphela ngokucophelela inkanyamba singayiqonda le mibono, ngoba ngenkathi isakhiwo sayo esizungezayo siqala ukuzungeza ngesivinini esikhulu kakhulu, size sicekele phansi, futhi lesi sivinini esifanayo siyancipha njengoba sihamba. umoya uyehla, ngoba ubukhulu bekhoni banda endaweni ebanzi kakhulu kunasendaweni encane kakhulu.
Uyini umsebenzi we-Anemometer
Ezinye izinsimbi ziyinkimbinkimbi kunezinye
Uma sicabangela ukuthi umoya ungomunye wamandla amakhulu emvelo, angaba yinzuzo enkulu ezidalwa eziphilayo, umoya ungaba namandla amakhulu abhubhisayo, ngakho isidingo sokulinganisa ukuqina kwawo kuyisici esibalulekile.sokucwaninga nokubikezela.
Thola okwengeziwe ngokufunda lesi sihloko: EZIYI-10 EZINGAKUMBI ZENZIWA Ubisi ONGAKUPHUTHI
Kulokhu i i-anemometer o i-anemograph Kuyithuluzi lokulinganisa lesimo sezulu, elisetshenziselwa ukukala isivinini somoya futhi ngaleyo ndlela lisize ekubikezelweni kokushintsha kwesimo sezulu. Lo mshini futhi unomsebenzi omkhulu ekundizeni kwendiza enesisindo esingaphezu kwendiza, ngale ndlela kunqunywa uhla oluphephile lwendiza kanye nomzila othembeke kakhulu.
Ezifundweni ze-meteorology, ama-anemometers enkomishi noma e-pinwheel asetshenziswa kakhulu, asesimweni segayo elincane, elinezinsimbi ezintathu ezinenkomishi yimaphi amandla asebenzayo womoya ngesikhathi sokungqubuzana nawo, awenze azungeze. Ngale ndlela, inani lama-laps aqoshwe imishini lingafundwa ngokuqondile kwikhawunta noma lirekhodwe ebhandeni lephepha, elibizwa ngokuthi i-anemogram.
Kukhona nezinto ezikala isivinini somoya ezingafaki igrafu ephepheni, ngoba le datha iqoshwa futhi ihlaziywe ngekhompyutha, ekwazi ukubikezela izinguquko ezithile kanye nokuhlukahluka emoyeni okusiza ekubikezelweni okunembile kwesimo sezulu. Lezi zisetshenziswa zobuchwepheshe.
Nweba lolu lwazi lapha: BELUNJANI UHAMBO LOKUQALA LOMNTU LOKUYA ESIKHALENI
Isiqondiso somoya nakho kuyisici esibalulekile okufanele silinganiswe mayelana nezinguquko zesimo sezulu, kwezinye izinsuku noma izinkathi wonyaka, kulokhu kusetshenziswa i-vane yesimo sezulu, ekhombisa isiqondiso lapho umoya uvela khona, le datha irekhodwa ngendawo yabo eyikhadinali.
Elinye ithuluzi elinikeza inkomba engacacile yesiqondiso nokuqina kwe-miso yilokho okuvame ukubizwa ngokuthi. isivunguvungu. Leli thuluzi lobuchwepheshe obuphansi lisetshenziswa kakhulu ezikhumulweni zezindiza. Kuwuhlobo lweshubhu yendwangu evulekile ezinhlangothini ezimbili futhi ilengiswe ngaphezu kwesigxobo.
Ngokuya ngempahla, isisindo kanye nezimo zensimbi, iyalinganiswa ukuze irekhode izinguquko emoyeni.Uma kungekho moya, umkhono uhlala umile, ulenga esigxotsheni sawo. Lapho kuvunguza umoya, ibekwe endaweni engaphezulu noma engaphansi kwe-oblique, futhi uma kwenzeka umoya unamandla kakhulu, umkhono uzohlala uphakanyiswe ngokuhambisana nomhlabathi.
Isandulela sesikali sokulinganisa Umoya
Ukunquma ukushuba komoya, isikali sokulinganisa ngobuhle sithi: Beaufort. Lesi sikali sidalwe ngu Sir Francis Beaufort, owayeyisikhulu samasosha asolwandle sase-Ireland kanye nomdwebi wezithombe zamanzi, cishe unyaka ka-1805. Ngonyaka ka-1800 izikhulu zamasosha asolwandle zazisibheka njalo isimo sezulu, kodwa zazingenaso isikali sokulinganisa futhi izilinganiso zazingaphansi kakhulu ukuze ziqondwe. yona.