Sonke siyathanda ukuya elwandle kwaye sonwabele imozulu entle, ukutshiswa lilanga, nokuqubha kamnandi. Noko ke, ngeentsuku ezinomoya, amaza ayasithintela ekuthabatheni loo diphu ihlaziyayo. Mhlawumbi ukhe wazibuza ngaxa lithile ukuba loo maza angapheliyo angazange aphele enziwa njani, kodwa awazi ukuba kutheni okanye ngawaphi amaza ngokwenene.
Ngaba uyafuna ukwazi ukuba yintoni na amaza olwandle kunye nendlela enza ngayo?
Yintoni iliza?
Amaza ayikho enye into ngaphandle kwempompo yamanzi esemanzini. Bayakwazi ukuhamba iikhilomitha ezininzi phezu kolwandle yaye, ngokuxhomekeke emoyeni, zikwenza oko ngesantya esikhulu okanye esingaphantsi. Xa amaza efika elunxwemeni, ayaqhawuka aze aphelise umjikelo wawo. Ukongeza, unokufunda ngakumbi malunga nendlela ukuphakama kwamaza kulinganiswa ngayo kweli nqaku. malunga nomlinganiselo wamaza kunye nendlela enokuba nefuthe ngayo kwi ukuthintela amaza ayingozi.
Umvelaphi
Nangona kuhlala kucingelwa ukuba amaza abangelwa sisenzo somoya, oku kudlulela phambili. Umvelisi wokwenene wamaza ayingumoya, kodwa liLanga. Lilo ilanga elitshisa umoya ojikeleze umhlaba, kodwa ayenzi iyunifomu yonke. Oko kukuthi, amanye amacala oMhlaba ashushu kwisenzo seLanga kunamanye. Xa oku kusenzeka, uxinzelelo lomoya luhlala lutshintsha. Iindawo apho umoya ushushu khona, uxinzelelo lomoya luphezulu kwaye kuyilwa imimandla yozinzo kunye nemozulu elungileyo, apho i-anticyclones ibalasele khona. Kwelinye icala, xa indawo ingatshisi kangako kwilanga, uxinzelelo lomoya lusezantsi. Oku kubangela ukuba imimoya yenze uxinzelelo ngaphandle koxinzelelo.
Amandla omoya asemoyeni asebenza ngendlela efanayo naleyo yamanzi. Ulwelo, kule meko umoya, luthanda ukuya ukusuka apho kukho uxinzelelo ngakumbi ukuya apho kukho okuncinci. Okukhona umahluko omkhulu woxinzelelo phakathi kwendawo kunye kwenye, kokukhona umoya uya kuvuthuza kwaye ubangele izaqhwithi. Ngaphezu koko, kunomdla ukubona indlela Imisinga yolwandle ichaphazela ukubunjwa kwamaza.
Xa umoya uqalisa ukuvuthuza kwaye uchaphazela umphezulu wolwandle, amasuntswana omoya akhuhla kumasuntswana amanzi kwaye amaza amancinane aqalisa ukumila. La maza abizwa ngokuba ngamaza e<em>capillary kwaye awayonto engaphezu kwamaza amancinane aneemilimitha ezimbalwa ubude. Ukuba umoya uvuthuza kumgama weekhilomitha eziliqela, amaza e-capillary ayakhula aze abangele amaza amakhulu. Kukwanika umdla ukuqwalasela indlela i ukufudumala kwehlabathi kuchaphazela umgangatho wolwandle.
Izinto ezichaphazelekayo ekubunjweni kwayo
Zininzi izinto ezinokubangela ukubekwa kwamaza kunye nobukhulu bawo. Kuyabonakala, imimoya enamandla yenza amaza aphezulu, kodwa kufuneka kwakhona sithathele ingqalelo isantya kunye nobunzulu bentshukumo yomoya kunye nexesha ohleli ngalo kwisantya esizinzileyo. Ezinye izinto ezigqiba ukubunjwa kweentlobo ezahlukeneyo zamaza yindawo echaphazelekayo kunye nobunzulu. Njengoko amaza esondela elunxwemeni, ahamba kancinane ngenxa yokuba ubunzulu buncinane, ngoxa ingqukuva isanda ngobude. Inkqubo iyaqhubeka de kube indawo ephakanyisiweyo ihamba ngokukhawuleza kunenxalenye engaphantsi kwamanzi, apho intshukumo iyancipha kwaye i-wave iphule.
Kukho ezinye iintlobo zamaza asezantsi kwaye ajikelezwe akhiwa ngumahluko kuxinzelelo, ubushushu kunye nobutyuwa beendawo ezikufutshane. Lo mahluko ubangela ukuba amanzi ashukume kwaye avelise imisinga eyenza amaza amancinci. Oku kubizwa Amaza olwandle ngasemva. Kukwanika umdla ukuphonononga ingqikelelo yamaza ukuze uqonde ngcono ukuba ezi ndlela zihlangana njani, njengoko ubona ku Eli nqaku malunga namaza.
Amaza aqhelekileyo esiwabona elunxwemeni ahlala enawo ubude obuphakathi kwe-0,5 kunye ne-2 yeemitha kunye nobude phakathi kwe-10 kunye ne-40 yeemitha, nangona kukho amaza anokufikelela kwi-10 kunye ne-15 yeemitha ukuphakama. Kwakhona kubalulekile ukuqaphela ukuba i Ubungakanani bamaza bunokwahluka kwiindawo ezahlukeneyo zeplanethi.
Enye indlela yokuvelisa
Kukho enye inkqubo yendalo ekwabangela ukwenziwa kwamaza kwaye ayingomoya. Imalunga nenyikima. Iinyikima ziinkqubo zejoloji ezithi, ukuba zenzeka kummandla wolwandle, zinokwenza amaza amakhulu abizwa ngokuba ziitsunami.
Xa inyikima isenzeka emazantsi olwandle, utshintsho olukhawulezileyo olwenzeka kumphezulu lubangela amaza amakhulu eekhilomitha ukuba ajikeleze loo ndawo. La maza ahamba ngokukhawuleza okukhulu ngokukhawuleza olwandle, ukufikelela kwi-700km / h. Esi santya singafaniswa nenqwelo-moya.
Xa amaza olwandle ekude elunxwemeni, amaza ahamba iimitha ezimbalwa ukuphakama. Kulapho isondela elunxwemeni xa iphakama phakathi kwe-10 ukuya kwi-20 yeemitha ukuphakama kwaye iyinyani yeentaba zamanzi ezinefuthe elunxwemeni kwaye zibangele umonakalo omkhulu kwizakhiwo ezikufutshane nakulo lonke ulwakhiwo kummandla.
Iitsunami ziye zabangela iintlekele ezininzi kwimbali. Ngenxa yesi sizathu, izazinzulu ezininzi zifunda iindidi zamaza enziwa elwandle ukuze zenze unxweme lukhuseleke ngakumbi kwaye, ukongezelela, zisebenzise isixa esikhulu samandla akhutshwa ngawo ukuvelisa umbane njengenkqubo ehlaziyiweyo. Ukongeza, ukufundwa kweenyikima kusinika ulwazi oluxabisekileyo malunga notshintsho kwiipropathi ezinwebekayo ze-Earth's crust, ekwanxulumene nayo. imo iyatshintsha.
Iindidi zamaza
Kukho iintlobo ezininzi zamaza ngokuxhomekeke kumandla kunye nokuphakama kwabo:
- Amaza asimahla okanye ajikelezayo. La ngamaza afumaneka kumphezulu kwaye ngenxa yokwahluka kwinqanaba lolwandle. Kuzo, amanzi akaqhubeki phambili, achaza kuphela ukujika njengoko enyuka kwaye ewa phantse kwindawo enye apho ukunyuka kwamaza kwaqala khona.
- Amaza okuguqulela. La maza avela kufutshane nonxweme. Njengoko beqhubela phambili, bachukumisa ulwandle kwaye bagqibela ngokungqubeka elunxwemeni, besenza amagwebu amaninzi. Xa amanzi ebuya kwakhona ihabango lifom.
- Amaza anyanzeliswayo. Ezi ziveliswa sisenzo sogonyamelo somoya kwaye zingaba phezulu kakhulu.
Ngenxa yokufudumala kwehlabathi, amazinga olwandle ayenyuka, kwaye amaza aya kulonakalisa ngakumbi unxweme. Ke ngoko, kubalulekile ukuqonda kangangoko malunga neentshukumo zamaza ukwenza amanxweme ethu abe yindawo ekhuselekileyo. Ukongeza, kubalulekile ukuqwalasela iindidi zeemeteors ezinokuchaphazela le nto kunye nendlela ezinokunxulumana ngayo. imo iyatshintsha.
