Abstract

SummarySnow‐packing, a combination of ice, hoarfrost and snow on trees, and the subsequent tree damage by snow, were estimated on Norway spruce (Picea abies), Scots pine (Pinus sylvestris), and pubescent birch (Betula pubescens) in the winter of 1993‐94 in southern Lapland, northern Finland, near the local alpine timberline around 400 m a.s.l. Snow‐packing on each fully sized tree increased from a few hundred kilograms at 150–250 m a.s.l. to a maximum of 3290 kg at 300–350 m a.s.l. At 300 m a.s.l., snow‐packing per metre of stem increased from 30 to 50 kg on trees < 5 m in height up to 180–200 kg on 20‐m trees. There was 300 000‐480 000 kg/ha of snow accumulated on tree crowns. No stem breakage by snow‐packing occurred at or below 250 m a.s.l., whereas at 290–350 m a.s.l., 0‐46%, 39‐100%, and 0–33% of the spruce, pine and birch trees, respectively, had broken tops. Birch appeared to be the most resistant and pine the most susceptible to snow breakage.

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