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Igloo effect. The Igloo effect refers to the phenomenon that allows igloos and similar structures to remain warm on the inside, despite being made of snow and located in frigid environments. The effect is primarily due to two factors: insulation and body heat.
An igloo (Inuit languages: iglu, [ 1 ] Inuktitut syllabics ᐃᒡᓗ [iɣˈlu] (plural: igluitᐃᒡᓗᐃᑦ [iɣluˈit])), also known as a snow house or snow hut, is a type of shelter built of suitable snow. Although igloos are often associated with all Inuit, they were traditionally used only by the people of Canada's Central Arctic and the ...
The Inuit tradition of living in tents during summer and in igloos and qarmait (singular: qarmaq, warm half-subterranean houses made from boulders, whale bones and sod) in winter still followed the Thule practices. The most important principle of all building constructions was the lowered entrance tunnel, which served as a windscreen and cold trap.
More importantly, the Merrick Inn has not one, but four fireplaces — a wood-burning one in the bar, and gas fireplaces in three of the dining rooms, quadrupling your chances of staying warm here.
A quinzhee or quinzee / ˈkwɪnziː / is a Canadian snow shelter made from a large pile of loose snow that is shaped, then hollowed. This is in contrast to an igloo, which is built up from blocks of hard snow, and a snow cave, constructed by digging into the snow. The word is of Athabaskan origin [1][2] and entered the English language by 1984. [3]
Snow cave. A snow cave is a shelter constructed from snow by certain animals in the wild, human mountain climbers, winter recreational enthusiasts, and winter survivalists. It has thermal properties similar to an igloo and is particularly effective at providing protection from wind as well as low temperatures. A properly made snow cave can be 0 ...
Foehn wind. A Foehn, or Föhn (UK: / fɜːn /, US: / feɪn / fayn, [2][3] US also / fʌn, fɜːrn / fu (r)n[4][5]), is a type of dry, relatively warm downslope wind that occurs in the lee (downwind side) of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture ...
A warm front is a density discontinuity located at the leading edge of a homogeneous warm air mass, and is typically located on the equator-facing edge of an isotherm gradient. Warm fronts lie within broader troughs of low pressure than cold fronts, and move more slowly than the cold fronts which usually follow because cold air is denser and ...