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 ethambile ekama izinwele zakho futhi ishelela phansi ngobuso bakho futhi ngezinye izikhathi, ingasondela kuwe ngokushesha kangangokuthi ingakuphakamisa esibhakabhakeni esiqhele ngamakhilomitha angamakhulu. Ukuze ufunde kabanzi mayelana nomthelela womoya, vakashela lesi sihloko ngokuthi ini ukhiqiza umoya.
Iyini isenzakalo somoya?
Umoya ukugeleza kwamagesi ngama-magnitude amakhulu. Eplanethini enguMhlaba lesi senzo siwukuhamba kwenqwaba yomoya eguquguqukayo futhi engaguquki emkhathini, ojikeleza 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 ajwayelekile, njengokuthi, isibonelo, umoya, isiphepho, isiphepho, isiphepho kanye nesishingishane.
Lesi simo sezulu singenzeka ngezilinganiso ezihlukahlukene ezaziwayo: kusukela ekusebenzeni okuneziphepho okungahlala amashumi emizuzu, kuya kumoya ohelezayo kancane kancane okhiqizwa ukushisa okuhlukene kwendawo yoMhlaba enamatshe, imimoya enjalo ingahlala amahora amaningana; ngisho imimoya global, okuyinto umphumela umehluko ukumuncwa amandla elanga phakathi kwe- izindawo ezahlukene ze-geoastronomical Zomhlaba, lokho ekuqaleni esasikubiza ngokuthi amandla angaphandle. Ukuze ufunde kabanzi mayelana nemimoya yendawo nokuhlukaniswa kwayo, bheka isihloko sethu ku imimoya yendawo e-Argentina.
Kunezinhlobo ezahlukene zokukhiqiza umoya. Kuye ngokujikeleza komkhathi ku isikali esikhulu Ziyimimoya ekhiqizwa ukufudumeza okuhlukile kobuso boMhlaba kuye ngokuthi i-latitude, kanye namandla aphansi kanye ne-centrifugal akhiqizwa ukunyakaza okujikelezayo kweplanethi.
Ngokufanayo ezindaweni ezishisayo, ukujikeleza kokucindezeleka okushisayo okuhlukile ngaphezu komhlabathi kanye amathafa aphakeme Inamandla okukhuthaza ukujikeleza kwama-monsoon amakhulu.
Ngakolunye uhlangothi, ezindaweni ezisogwini, umjikelezo okhiqizwa phakathi komoya ohelezayo nolwandle/umoya ovunguzayo wezwe ungabonisa imimoya yendawo; Uma ufuna ukwazi okwengeziwe mayelana ne-curiosities yomoya, ngikumema ukuthi uthole izinto ezimangalisa kakhulu zemvelo.
ukufuduka womoya endaweni engezansi Umkhathi, indawo ebizwa ngokuthi: troposphere, iyona ebona kakhulu abantu, lo moya unezici ezimbili:
isici esime mpo, ebangeni elisukela kumakhilomitha ayi-10 noma ngaphezulu futhi ukunyakaza kwayo ukuya phansi noma phezulu kunxephezela umoya ovundlile; kanye nesici esivundlile, esifinyelela emakhulwini amakhilomitha futhi esifaneleka kakhulu kokubili.
Uyini umsebenzi we-Anemometer
Ezinye izinsimbi ziyinkimbinkimbi kunezinye
Uma kucatshangelwa ukuthi umoya ungomunye wamandla amakhulu emvelo, angaba yinzuzo enkulu ezintweni eziphilayo, futhi ungaba namandla amakhulu abhubhisayo, ngakho isidingo sokulinganisa ukuqina kwawo kuyisici esibalulekile ekutadisheni nasekubikezeleni kwawo.
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. Lolu cingo luphinde lusebenze kakhulu ekundizeni kwendiza enomthwalo osindayo kunomoya, ngaleyo ndlela inquma ibanga lokundiza eliphephile kanye nomzila othembeke kakhulu. Ukuze uthole ukwaziswa okwengeziwe mayelana imimoya, ungavakashela isihloko mayelana unkulunkulu u-Aeolus, unkulunkulu womoya ezinganekwaneni.
Ezifundweni ze-meteorology, inkomishi noma ama-anemometers e-windmill asetshenziswa kakhulu, amise okwesigayo esincane, esinamacembe amathathu anezinkomishi lapho 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, njengoba idatha eshiwo irekhodwa futhi ihlaziywe yikhompyutha, ekwazi ukubikezela izinguquko ezithile kanye nokuhlukahluka emoyeni okusiza ekubikezelweni okunembile kwesimo sezulu. Lezi zisetshenziswa zobuchwepheshe.
Thola okwengeziwe 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.
Enye insimbi esebenza ukunikeza inkomba engacacile yendlela kanye nokuqina okufanayo 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 nesimo sensimbi, iyalinganiswa ukuze irekhode izinguquko emoyeni. Uma umoya ungekho, i-windsock ihlala imile, ilenga ku-shaft yayo. 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 amandla omoya, isikali sokulinganisa ngobuhle sithi: Beaufort. Lesi sikali sidalwe ngu Sir Francis Beaufort, owayeyisikhulu samasosha asolwandle sase-Ireland kanye nomdwebi wama-hydrographer, cishe ngonyaka we-1805. Ngonyaka ka-1800 izikhulu zamasosha asolwandle zazihlola isimo sezulu esivamile, kodwa zazingenaso isikali sokulinganisa futhi izilinganiso zazivumelana kakhulu ukuze ziqondwe, futhi yilapho ukubaluleka kwazo kulele khona.
