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above the evaporating surface becomes gradually saturated with water vapour. If this air is not continuously replaced with drier air, the driving force for water vapour removal and the evapotranspiration rate decreases. Every year avalanches kill dozens of skiers. Avalanches of snow may occur under totally different circumstances, both during periods of frost and of thaw, especially when a warm (Föhn) wind is blowing. In such a case the top layer of snow melts rapidly, especially if the sun is shining. This layer of snow can then easily start to slide. Wet snow or slush can also easily cause avalanches from the weight of the large amounts of water they contain. Rain and thawing, often in springtime, cause wet or surface avalanches. In coastal areas the wind is generally stronger, but the local population is used to it. Waves as high as houses caused by a severe gale or hurricane, can cause dangerous conditions and vdamage on the coast. Ice floes reaching the coast and slabs of drift ice forced up and over each other can be a hazard. The worst disasters of all are caused by sea surges,

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