Imisinga ocean bengafani nasemagagasini? Imvelo kanye nokwenzeka kulezi zinkanyezi

Uyazi ukuthi amanzi olwandle ukuhambisa? I imisinga ocean bengafani nasemagagasini? Kungakhathaliseki inzuzo lezi izinqubo nalokho sivela laba bantu? Ake sizame ukuba siphendule le mibuzo ...

ocean amanzi

Olwandle uba umzimba owodwa ukuthi ungalokothi sisesenjalo. Kuyinto umzimba ngobukhulu amanzi emhlabeni. Oceans zihlukaniswe ezindaweni ezine (ngezinye izikhathi ezinhlanu) - Pacific, Atlantic, Indian, Arctic kanye North, ngokuya umehluko yayo futhi izici ezindaweni ezahlukene.

Kutfutfukisa futhi baxhumana uqweqwe eMhlabeni kanye nomkhathi. Olwandle akemi namanje, njalo iqhubekela phambili, umphumela okuyizinto namagagasi, amagagasi, imisinga. Izehlo zalezi zenzakalo ukukhuthaza izinqubo eziningi. Ezinye izenzakalo njalo, abanye zavele.

Ukunyakaza kwabantu noma izithunzi amanzi olwandle incike komoya kanye lokushisa yayo nomthelela ekwakhekeni izakhiwo ezithile amanzi. Ngesikhathi esifanayo, kuba nomphumela reverse lapho ulwandle kuthinta ukugeleza izinqubo ozungeze umhlaba wethu.

Imisinga ocean bengafani nasemagagasini?

Ukubukeka amagagasi, imisinga, amagagasi ikhuthaza kwegazi njalo ebangelwa umkhathi, okuvela kuyo imimoya. Efundweni kuthinta Luhambo kwelanga nokwenyanga. Izimo letitsintsa amandla nobunjalo amandla amanzi imifudlana sendawo ngezansi kanye nokunyakaza Earth.

Ukuze ubone ukuthi yini yolwandle zihlukile kusukela amagagasi, cabanga kokubili izenzakalo ngokuningiliziwe. Kafushane singasho ukuthi ifomu wave kungokwesikhashana, bavame ukunezela lokhu emoyeni ageleza phezu kwamanzi. Ngezinye izikhathi imbangela ekuzamazameni komhlaba, khona-ke akukho nje amagagasi nama-tsunami.

Flow, kunalokho, imiphumela yesikhathi eside. umehluko ngokuyinhloko kusukela amagagasi ukuthi ngeke ngempela zimiswe phezu kwamanzi kungenzeka ekhona ingosi yayo. Abanaso njalo kuxhomeke emoyeni futhi ngokuvamile babe kolunye uhlangothi kuso.

ulwandle imisinga

Sesikhathele mayelana ukuthola ukuthi yini yolwandle zihlukile kusukela amagagasi. Manje ake sixoxe ngokuningiliziwe ngalokhu. Currents ngokuthi ovundlile amanzi ukusakaza izilwandle nezilwandle, ezithinta indlela njalo futhi beqondiswa nguye. Kufana umfula phakathi kwezinye amanzi.

Kuye ukujula zingabantu eligcizelela ukubukeka kwangaphandle, demersal futhi ijulile. Ngu lokushisa yabo yahlukaniswa abandayo, efudumele futhi singathathi hlangothi, okusekelwe umehluko kuqhathaniswa amanzi ezungezile. Labizwa ngokuthi zamanje ubunjalo imvelaphi, uhlobo izici ukunyakaza, ngokomzimba futhi amakhemikhali.

Isizathu nokuhlanzeka kwangaphandle nokuziphatha kwabo, afane namagagasi, kungaba ohelezayo. Kuphela kulesi simo umoya kufanele kube njalo (ezindaweni ezithile) noma ngezikhathi ezithile zonyaka, is abasafufusa ngezikhathi ezithile zonyaka. Dala angafuneka ukuze amanzi okweqile (isib ngesikhathi ukuncibilika kwezinguzunga zeqhwa okwakungokokuqala ngqá) noma iyehla iyenyuka seiche level yayo.

Isizathu esiyinhloko kumiswa imisinga kuyinto emkhathini. Ukushisa Kungalingani ngemazinga lomoya Ezindaweni ezahlukene kudala ukusakazwa kwalo, ekhuthaza kumiswa yolwandle. Warm, ngokuvamile athwale amanzi abo yenkabazwe, amakhaza - nenkabazwe.

amagagasi Imvelo

Ajwayelekile kithi amagagasi kuvame kwakheka umoya notshwala phezu kwamanzi, okuyinto nishaye izinga onhlobonhlobo. Lesi simo esiyingqayizivele sibangelwa kungokwemvelo, ngakho-ke, amandla abo futhi ubukhulu kuncike emandleni umoya. Esikhathini evulekile ulwandle wave ukuphakama ngezinye izikhathi ifinyelela 30 amamitha.

Ngesikhathi uhambisa amagagasi kancane kancane amandla akhe. ijubane wabo wakhona obuphelele. Isikhathi esining impela, basuke ahlanganisiwe, ngokwesibonelo, lapho ebamba eside Ngamafuphi nje, kungenxa lapho kukhona ukuphulwa noma igagasi okhulisa.

ukunyakaza Crustal kungacupha negagasi elikhulu kakhulu - i-tsunami. Baphakamisa yesivinini 800 amakhilomitha ngehora. amandla kwabo okulimazayo isiba eziyingozi kakhudlwana nangokucacile njengoba kusondela ogwini, lapho zifinyelela ubude obungamamitha omkhulu, ashaya ogwini. Esikhathini evulekile ulwandle i-tsunami ukuphakama uphansi.

ukubukwa ngamanye ukuphakama kwamagagasi ogwini. Basuke kubuswa amabutho Luhambo kwezindikimba zasezulwini. Ngesikhathi ukuphakama amagagasi kakhulu ukuthonywa indawo, isimo sezwe, ikakhulukazi ugu sihlehliswe. Ezinye izazi zithi mayelana ubuhlobo magagasi futhi yolwandle, okusikisela ukuthi namagagasi kwenyanga kubangele Imisinga ulwandle.

Umthelela futhi ingozi yamanzi ukunyakaza

imiphumela Iningi unomphela babe ulwandle imisinga. Bathwala amakhaza futhi efudumele mass amanzi, ezinomthelela amazwekazi sezulu. ofudumele ukwenza kube ezimanzi, ukuletha imvula, abandayo neqhaza ukuze ome sezulu. Isikhathi eside ukuchayeka ukugeleza ebandayo hleze ukukhiqiza ezingwadule, isib, Atacama eNingizimu Melika.

Phakathi ngokuvamile amagagasi esindayo akhiwa sidabukile zamanje, noma sidabukile. Kuyinto ekusakazeni ewumngcingo yamanzi ezihambayo perpendicular ogwini, oniselwa. Backflow ingozi olwandle, ukuthi amanzi jet ebusweni ngokoqobo ukudansela isiginci sakhe konke olwandle oluvulekile.

Uma ukuthola isivinini, bese ukuphuma kunzima, nakuba kungenzeka. Ngenxa yale njongo Asibona ababegwedla isikebhe ogwini, kuse ecaleni. Lokho beshiya isiminyaminya nesiphithiphithi sasemadolobheni musa ukuwela rips, phansi Lokudabuka zawo ngokuvamile kutholakala izimpawu ezikhethekile noma namafulege abomvu.

amandla wave

indlela Old ugesi esebenzisa enuzi izitshalo amandla onganelisekile umphakathi wezwe lonke. Ukuba kubekwe izindlela ukuza. Omunye wabo ukuthola amandla kusuka amagagasi olwandle. Ithuba le ikhona e-Australia, eNingizimu Afrika, e-Western Europe, eNyakatho naseNingizimu Melika abaye ogwini Pacific.

Ungasebenzisa futhi i-namagagasi kungeyona. Nokho, le ndlela ibiza kakhulu, amanzi anosawoti buqeda konke, ukuze silondoloze imishini kunokuba nje egijima.

Okwamanje, amathuba ukuxhashazwa olwandle lungaphansi kokuthuthukiswa. Ngaphandle namagagasi, abacwaningi uhlela ukusebenzisa amandla olwandle, imisinga, wezinto zokubasa.