Storm Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Very Likely
- Tamaño
- 1–2
Unstable storm slabs will continue to increase in size until snowfall becomes rain later today. They have an upside-down, dense over light, character from the warming temperatures and rising snow levels which contributes to their unstable nature. Size of these slabs will be determined by elevation and when the snow switches to rain. Areas of greatest concern for storm slabs will be higher elevations where precipitation remains all snow and may receive 20” or more. High peaks and ridges are also where SW wind will be strongest and will likely build large new wind slabs.