Ngokusebenzisa izibonelo ezivela embhalweni nginikeze isifinyezo sezimbangela zezikhukhula zeqhwa ezimanzi.
Context:Ngokungafani ne-powder snow avalanches, i-wet snow avalanches iyisimo sejubane eliphansi leqhwa namanzi, lapho ukugeleza kuvinjelwe endaweni yomzila (McClung, uhlelo lokuqala ngo-1999, ikhasi 108). Isivinini esiphansi sokuhamba sibangelwa ukungqubuzana phakathi kwendawo eshelelayo yesitimela nokugeleza kwamanzi agcwele amanzi. Naphezu kwejubane eliphansi lokuhamba (≈10<unk>40 km / h), ama-avalanche eqhwa elimanzi ayakwazi ukukhiqiza amandla aqinile okubhubhisa, ngenxa yobuningi bawo obukhulu nokuqina kwawo. Umzimba wokugeleza kwe-avalanche yeqhwa elimanzi ungahamba ngeqhwa elithambile, futhi ungahlanza amadwala, umhlaba, izihlahla, nezinye izitshalo; ushiya umhlaba ovulekile futhi ovame ukuhlolwa emzileni we-avalanche. Izikhukhula zeqhwa ezimanzi zingaqalwa ngokukhishwa kweqhwa elixekethile, noma ukukhishwa kwama-slab, futhi zenzeka kuphela kuma-snowpacks anamanzi anamanzi futhi alinganiselwe ngokulinganayo kuze kube sezingeni lokuncibilika kwamanzi. Isici se-isothermal se-snow avalanches esimanzi siholele ekutheni kutholakale igama lesibili le-isothermal slides ezincwadini (ngokwesibonelo eDaffern, 1999, ikhasi 93). Ezindaweni ezifudumele, izimvula zeqhwa ezimanzi zivame ukuhlotshaniswa nemijikelezo yezimvula zeqhwa ekupheleni kwenkathi yasebusika, lapho kukhona ukufudumala okukhulu emini.
Izikhukhula zeqhwa ezimanzi zingaqalwa ngokukhishwa kweqhwa elixekethile, noma ukukhishwa kwama-slab, futhi zenzeka kuphela kuma-snowpacks anamanzi anamanzi futhi alinganiselwe ngokulinganayo kuze kube sezingeni lokuncibilika kwamanzi.