Characteristic of a high mountain climate are lower temperatures, frequency and intensity of wind and a more irregular distribution of precipitation. High mountain climate is defined by small-scale, terrain-dependent and short-term changeability.
CITATION STYLE
Larcher, W. (2012). Bioclimatic temperatures in the high alps. In Plants in Alpine Regions: Cell Physiology of Adaption and Survival Strategies (Vol. 9783709101360, pp. 21–27). Springer-Verlag Wien. https://doi.org/10.1007/978-3-7091-0136-0_3
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