El ukusebenza kwekorioli Yaziwa ngokubanzi kwisayensi ukubhekisa kumjikelo wamanzi kunye nomoya kwii-hemispheres ezahlukeneyo. Kuthiwa oko izaqhwithi kwaye iinkqwithela zijikeleza enye indlela kumantla e-hemisphere kwaye enye indlela kwi-hemisphere esemazantsi. Kutheni le nto ifanelekile? Kukwanjalo nakwimizimba yamanzi kunye nakwinyani edumileyo yokujika okuchasene namanzi endlu yangasese kwiihemispheres ezahlukeneyo. Konke oku kuhambelana nefuthe lekoriyoli.
Ngaba uyafuna ukwazi ngakumbi malunga nefuthe leCoriolis? Apha siza kukucacisela yonke into.
Yintoni impembelelo yekoriolis
Umfumanisi owayephethe ngokuchaza ngokwezibalo lo mkhosi yayinguGaspard-Gustave Coriolis. Ngombulelo kule nto ifumana eli gama hayi elinye. Ifunyenwe ngo-1935 kwaye incede yazi ngakumbi ngeplanethi kunye nomhlaba. Kuzo zonke iintshukumo ezijikelezayo kukho amandla e-coriolis.
Iziphumo zilula ukuzichaza. Ngamandla okwenzeka ngenxa yokujikeleza komhlaba kwi-axis yawo. Oku kujikeleza kuko okusenza sibe nemini nobusuku. Ngenxa yale spin, imizila yezinto ehambayo emhlabeni iyaphambuka. Yinto ebonakalayo ukuba siyenza kwinto ejika ngokukhawuleza. Kwaye kunjalo noMhlaba. Nangona kunjalo, ngenxa yamandla omxhuzulane, asiqapheli ukuba uMhlaba ujikeleza ngokuqhubekayo kwaye ngaphandle kokuma.
Izinto ezinxaxhileyo ekunene kuyo yonke into emantla e-hemisphere kunye nasekhohlo kuyo yonke into ese-hemisphere esemazantsi. Esi sizathu sokuba izivunguvungu kunye neenkanyamba zihamba kumacala ahlukeneyo njengoko zikwindawo enye okanye kwenye.
Xa oku kusenzeka, ukukhawulezisa okunxulumene nomzimba kwenzeka ngokungafaniyo nesantya esihambelanayo ngoku. Ke, Kuxhomekeka kwisantya apho into ihamba khona, isiphumo sekhoriyoli siya komelela okanye hayi.
Iziphumo zecoriolis kwimeteorology nakwilwandlekazi
Amandla e-coriolis achazwe kumaphepha okuqala esayensi emva kokufunyanwa kwawo njengamandla e-centrifugal. La mandla ngalawo omzimba oshukuma ngokunxulumene nenkqubo efana nesalathiso kunye nokujikeleza. Yiyo eyenzekayo noMhlaba. Ukuze siyiqonde kakuhle, Kufana nokubeka ibhastile kwigiya elihambayo. Ukuhamba kwayo kuya kuguqulwa kuxhomekeke kwisantya semarble, kuba siya kuthatha ukuba isantya esijikeleza ngaso izixhobo sihlala sihleli. Oku kwenzeka ngesantya sokujikeleza komhlaba, kuhlala kunjalo.
Ke ngoko, ukuphambuka kunye nokubiza kwayo ukuba umkhondo wezinto ezisemhlabeni uya kulungiswa ngesantya. Siza kuhlalutya ukubaluleka kwesi siphumo kwicandelo lemeteorology kunye nolwandle.
Xa ubunzima bomoya okanye bamanzi buhamba, balandela imelidians yasemhlabeni. Isantya sayo, ke, siyalungiswa kunye nokuhamba kwayo ngokwenziwa yimpembelelo yekoriolis.
Esi siphumo sisinceda sazi ukuba xa kukho intshukumo ejikelezayo, ii-vortices ziya kulandela imeko echaziweyo. Oku kwenzeka ngezaqhwithi kunye nee-anticyclone kuyo nayiphi na iplanethi hayi eMhlabeni kuphela. Kananjalo amandla e-coriolis ayenzeka ngokujikeleza kwelanga kunye neenkwenkwezi.
Esi siphumo senzeka ngendlela ethe kratya kwi-ikhweyitha kuba injalo indawo apho isantya siphezulu sikhulu. Kwiipali ziyacotha. Kungenxa yokuba kwi-ikhweyitha, umgama oya embindini woMhlaba mkhulu.
Kutheni iinkanyamba zijika ziye kwelinye icala?
Izitya zokuhlambela ezinobume obufanelekileyo, ezinje nge-North Atlantic basin kunye noMzantsi, isiphumo sijika imisinga yaselwandle. Kwi-hemisphere esemantla iyabaphambukela ngasekunene nakwisiqingatha esisezantsi ngasekhohlo. Kukwanjalo nakwimimoya.
Ngokuphathelele Amarhe okusasazeka kwendlu yangasese e-Australia ayinyani. Azijikelezi kwicala elichaseneyo njengoko zisenza kwihlabathi liphela ngenxa yesi siphumo. Ukuba oku kuyenzeka, kungenxa yokuba abavelisi bazakhela ukujikeleza ngaloo ndlela.
Kwelinye icala, ezo zijikeleza ngendlela eyahlukileyo ngenxa yempembelelo yekoriyoli ziziqhwithi. Ezi nkqwithela zilinganisa iikhilomitha ezininzi kwaye kunokuba kunjalo ukuba ukugqwesa kwabo kukwiihemispheres ezahlukeneyo. Xa oku kusenzeka, baya kujikeleza kwelinye icala kwilizwe ngalinye, kuba isiphelo ngasinye siya kuba nesantya esahlukileyo njengoko uMhlaba ujikeleza. Ke ngoko, iinkanyamba ziphela zikhula.
Kwimeko yeminyele, umxhuzulane ubangela ukuba umbindi womnyelezi ubekho kumngxuma omkhulu omnyama ojikelezayo notsale wonke umbandela ojikelezileyo. Nangona kunjalo, amandla omxhuzulane ayancipha njengoko sisuka kude kumbindi weminyele. Oku kunciphisa izinto kwaye kudala isiphumo esijikelezayo. Masingalibali ukuba iziko leminyele lakhiwa ngu- Umngxunya omnyama.
Izigqibo
Nangona kwabanye ayisiyonto inemeko, amandla e-coriolis yinto ebaluleke kakhulu. Iyenzeka kwiziganeko ezininzi eMhlabeni kwaye inoxanduva lokuhamba komoya kunye nolwandle. Le yinto ebalulekileyo ekufuneka uyiqwalasele xa ucwangcisa iindlela zomoya zeenqwelomoya.
Ndiyabulela kolu lwazi, sikwazi ukuqonda okuninzi malunga namandla eigalaksi, imisinga yomoya kunye nemisinga yamanzi. Kwiimeteorology kusetyenziswa ukuxelwa kwezi zinto zemozulu.
Ndiyathemba ukuba ngolu lwazi uyazi ngakumbi malunga nefuthe le-coriolis