Snow fundamentals Roman Juras
[email protected] Why do we care about snow? Glaciology Meteorology and climatology Sport Snow science Ecology Hydrology Natural hazard History René Descartes Wilson Bentley The first Ukichiro Nakaya First descriptions of The first photographs snow crystals artificial crystals of the snow in a book: Les Johannes Kepler in laboratory crystals Météores First attempts (1930) (1931) to describe (1637) snow crystals (1611) 3 What is snow? More points of view Monomineralic rock (Schneebeli, 2018) „Snow is a highly porous, sintered material made up of a continuous ice structure and a continuously connected pore space, forming together the snow microstructure.“ (Fierz et al. 2009) ICE + AIR + Water Vapour + (Liquid water + Impurities) „All three phases of water can coexist in snow on the ground“ (Fierz et al. 2009) • Snow is part of the cryosphere – water is represented mostly in a solid form • Most of the snow/ice covered area is located in the Northern Hemisphere 3,8 mil km2 (Aug) – 46,5 (Jan) mil km2 (area of Europe ~ 10,2 mil km2) • Snowmelt contributes approx. by 50 % to annual runoff. Mountainous regions can reach 85 % (i.e. Colorado river). En.wikipedia.org Origin of a snowflake Snow flake consists of one, but more often of multiple ice crystals Supercooled water droplets in clouds is still liquid even in temperature around -40°C. Snow crystals grow in supersaturated environment. Snow crystals start to grow around nuclei (dust particles, droplets, another snow crystals) – process of nucleation See Libbrecht