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Pihal bo šibak do zmeren severozahodnik. Ledišče bo na nadmorski višini okoli 2000 m. Jutri dopoldne bo sončno, popoldne pa spremenljivo oblačno s krajevnimi plohami. Zvečer in v noči na sredo bodo padavine pogostejše in izrazitejše, meja sneženja se bo prehodno spet spustila do okoli 1500 m nadmorske višine. Predvidoma bo v visokogorju zapadlo od 10 do 20 cm snega, krajevno lahko tudi do 30 cm. Ob padavinah bo pihal severni veter. V sredo se bo razjasnilo, popoldne bo spremenljivo oblačno s krajevnimi plohami in nevihtami. V četrtek bo dopoldne sončno, popoldne bo nastalo nekaj ploh. Ob koncu tedna, zlasti v noči z nedelje na ponedeljek, je v visokogorju zahodnih in južnih Julijskih Alp zapadlo tudi več kot 50 cm snega, drugod od 10 do okoli 20 cm. Močan jugozahodnik ga je spihal v zamete. Danes zjutraj se je meja sneženja spustila do okoli 1500 m, zapihal je okrepljen severni veter. V teh nadmorskih višinah je sneg mehak, višje suh, nižje moker. Veliko je zametov. Nižje je stari sneg razmočen. Predvsem v visokogorju so razmere povsem zimske. V sredogorju bo snežna odeja še naprej kopnela, sneg zaradi visoke vlage ter precej oblačnosti ne bo pomrznil. V visokogorju bo občasno snežilo. Novi sneg se bo sproti sesedal, zato večjega prirastka snežne odeje ne bo. Ker bo novega snega manj kot ob preteklem koncu tedna, ne pričakujemo povečanja nevarnosti snežnih plazov. Še bodo nekoliko bolj nevarna strma pobočja ter mesta z napihanim snegom predvsem od sredine dopoldneva do poznega popoldneva. Lahko se bo plazil novi sneg, plaz pa boste lahko sprožili tudi sami. Nižje pa je snežna odeja večinoma uležana in preobražena ter, kljub premočenosti, dokaj stabilna. Nevarnost snežnih plazov je v visokogorju Julijskih Alp ZNATNA, 3. stopnje, drugod v visokogorju ZMERNA, 2. stopnje, nižje pa MAJHNA, 1. stopnje. Nad nadmorsko višino okoli 2000 m je nov sneg, največ ga je v Posočju, ki se bo lahko plazil s strmih pobočij. Predvsem danes pričakujemo posamezne spontane plazove, plaz pa lahko sprožite tudi ob manjši obremenitvi snežne odeje. V visokogorju so nastali številni zameti. Nižje je dež razmočil staro snežno odejo, ki je zato postala manj stabilna. V sredogorju pa se je sneg talil in kopnel.