Sonke siyathanda ukuya elunxwemeni kwaye sonwabele imozulu entle, ilanga kwaye sihlambe kamnandi. Nangona kunjalo, ngeentsuku ezinomoya onamandla, amaza asithintela ukuba sihlambe. Ngokuqinisekileyo ubukhe wacinga ngendlela amaza angenasiphelo angapheliyo, kodwa awazi ukuba kutheni okanye ayintoni kanye kanye la maza.
Ngaba uyafuna ukwazi ukuba ayintoni amaza olwandle kwaye ayenziwa njani?
Yintoni iliza?
Amaza ayikho enye into ngaphandle kwempompo yamanzi esemanzini. Bayakwazi ukuhamba iikhilomitha ezininzi phezu kolwandle kwaye, kuxhomekeke emoyeni, benza njalo ngesantya esiphezulu okanye esisezantsi. Xa amaza efikelela elunxwemeni, ayaphula aze awugqibe umjikelo wawo.
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 phakathi koxinzelelo phakathi kwenye indawo kunye nomnye, kokukhona umoya uya kuvuthuza kwaye ukhokelele kwisaqhwithi.
Xa umoya uqalisa ukuvuthuza kwaye wenza njalo echaphazela umphezulu wolwandle, amasuntswana omoya ahlikihla ngokuchasene namasuntswana amanzi kunye namaza amancinci aqala ukubumba. Lawa abizwa ngokuba ngamaza e-capillary kwaye ayonto ingaphaya kwamaza amancinci kuphela ziimilimitha ezimbalwa ubude. Ukuba umoya uvuthuza ukuya kuthi ga kwiikhilomitha ezininzi, amaza e-capillary akhula makhulu kwaye akhokelele kumaza amakhulu.
Izinto ezichaphazelekayo ekubunjweni kwayo
Zininzi izinto ezinokubangela ukubekwa kwamaza kunye nobukhulu bawo. Kuyabonakala, imimoya enamandla yenza amaza aphezulu, kodwa kufuneka sithathele ingqalelo isantya kunye namandla esenzo somoya kunye nexesha lokuba lihlale kwisantya esizinzileyo. Ezinye izinto ezibeka imeko ekwakhiweni kweentlobo ezahlukeneyo zamaza yindawo echaphazelekayo nobunzulu. Njengokuba amaza esondela elunxwemeni, ahamba kancinci kuba bunobunzulu obuncinci, ngelixa indawo yokunyuka inyuka ngobude. Inkqubo iyaqhubeka de indawo ephakanyisiweyo ihambe ngokukhawuleza kunenxalenye engaphantsi kwamanzi, apho intshukumo iyazinzisa kwaye amaza ophuka.
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.
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.
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 zibangele iintlekele ezininzi kwimbali. Ngesi sizathu, izazinzulu ezininzi zifundisisa iindidi zamaza ezenzeka elwandle ukwenzela ukuba unxweme lukhuseleke kwaye, ukongeza, ukuze bakwazi ukusebenzisa amandla amakhulu ekhutshwa kuwo ukwenza umbane njengenkqubo evuselelekayo.
Iindidi zamaza
Kukho iintlobo ezininzi zamaza ngokuxhomekeke kumandla kunye nokuphakama kwabo:
- Amaza asimahla okanye ajikelezayo. La ngamaza aphezu komhlaba kwaye ngenxa yomahluko kumgangatho wolwandle. Kuzo amanzi akahambi phambili, ichaza kuphela ukujika xa usenyuka usihla phantse kwindawo enye apho kuphakama khona amaza.
- 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 yokunyuka kwamaqondo obushushu behlabathi, umgangatho wolwandle uyenyuka kwaye amaza aya esonakalisa unxweme. Ngesi sizathu, kubalulekile ukwazi yonke into enokwenzeka malunga namandla wamaza ukwenza amanxweme ethu abe yindawo ekhuselekileyo.