Ngendlela elula ikhombisa ukuzamazama komhlaba kwakamuva, amanqamu we-tsunami kanye nezindaba zesimo sezulu e-Chile. Umcimbi ngamunye unemininingwane yobukhulu, usuku okwenzeka ngalo umcimbi nesikhathi.
Iphinde yethule ulwazi mayelana nobukhulu bokuzamazama komhlaba okubonisa ukuthi ukuzamazama komhlaba kungabangela i-tsunami, lonke lolu lwazi lufakwe ekubukeni kwemephu ukuze kwaziwe indawo eqondile yesigameko.
Ungabona imibiko yokuzamazama komhlaba yokuzamazama kuzwelonke nakwamanye amazwe ngendlela elula. Le mibiko ihlanganisa nesithombe esine-seismogram (okurekhodiwe kokuzamazama komhlaba ngethuluzi langempela), kuphela uma sitholakala.
I-Chile Alerta iyakwazi ukwazisa izehlakalo zokuzamazama komhlaba ngesikhathi sangempela, futhi ngemva kwemizuzu embalwa iletha umbiko onemininingwane eminingi yomcimbi.
Izaziso ezikhishwayo esimweni sesehlakalo sokuzamazama komhlaba noma isexwayiso se-tsunami esingase (noma singenzeki) sithinte i-Chile ngandlela thize.
Lolu hlelo lokusebenza lunezinhlobo ezi-5 ezihlukene zama-alamu:
Umlayezo/Isaziso/Umbiko omusha noma isaziso esivamile. (I-alamu No. 1).
Isexwayiso Sokuzamazama komhlaba: kokundindizela okutholwe ngesikhathi sangempela futhi kuyazwela. (I-alamu No. 2).
Isexwayiso sokuvimbela i-tsunami: uma ukuzamazama komhlaba kwenzeka kwamanye amazwe anogu lwasePacific, kwaziswa ngokuvimbela uma kunengozi engaba khona futhi kamuva kuqinisekiswa ngedatha ye-SHOA. (I-alamu No. 3).
I-Alamu Yokuzamazama komhlaba: Ifana ne-Alamu No. 2, kodwa lokhu kwenziwa kusebenze ukuzamazama komhlaba okukhulu okungathinta izifunda eziningi zase-Chile. I-oda lithunyelwa Kuhlelo Lokusebenza ukuze uvule iwindi le-popup elinomsindo ongavalwa kuphela uma lelo windi livaliwe (kuyasiza ukudonsa ukunaka noma ukuvusa umuntu ngenkathi elele). (I-alamu No. 4).
I-Alarm ye-Tsunami: efana ne-Alamu No. 3 kanye neNombolo 4. Iwindi le-pop-up liyavuleka elibonisa i-tsunami eseduze. futhi ingavalwa kuphela ngokuvala iwindi le-popup. (I-alamu No. 5).
Imithombo ye-Chile Alert yile:
Isikhungo Sikazwelonke Seismological of the University of Chile.
Isevisi ye-Hydrographic kanye ne-Oceanographic ye-Navy.
I-Meteorological Directorate yaseChile.
Isikhungo Sesexwayiso Se-tsunami yasePacific.
I-European-Mediterranean Seismological Center.
Izikhungo Zokucwaninga Ezihlanganisiwe ze-Seismology.
I-Geofon - GFZ Potsdam.
I-United States Geological Survey.
.-Isikhombi esiluhlaza (Isexwayiso seSifundazwe 1): ukuzamazama komhlaba okunamandla aphansi, izexwayiso ze-tsunami ezingahlangabezani nezici zokukhiqiza i-tsunami ogwini lwase-Chile(?).
.-Isikhombi esisawolintshi (Isexwayiso Sesifunda 2): ukuzamazama komhlaba okunamandla amaphakathi okungadala umonakalo noma izexwayiso ze-tsunami, uma kukhona isexwayiso se-tsunami ngaphansi kokuhlolwa sizophinda sibe salo mbala.
.-Inkomba ebomvu (I-alamu Yesifunda 3): ukuzamazama komhlaba okunamandla kakhulu (ukuzamazama komhlaba), izexwayiso ze-tsunami ezihlangabezana nezici zokukhiqiza i-tsunami ogwini lwase-Chile (?).
Ukuboniswa kwemephu njengokujwayelekile noma ukubuka kwesathelayithi.
*ngokusho komuntu waseChilean:
Ukuzamazama: Ukuzamazama komhlaba okuzwelayo okunamandla aphansi/amaphakathi.
Ukuzamazama komhlaba: Ukuzamazama komhlaba okuzwelayo okunamandla amakhulu okubangela umonakalo (kungaba kukhulu noma kulingane no-6.5°?).
Kubuyekezwe ngo-
Sep 1, 2025