Firns is a plural form of firn, which is a type of snow that has undergone partial melting and refreezing over multiple years. The spelling of firns is straightforward, as it follows the standard English pronunciation rules. The word is pronounced as /fɜːns/, with the "i" being replaced by its long vowel sound "ɜː". The final "s" represents the plural form, effectively changing the singular firn into multiple firns. So, firns simply refers to multiple compacted masses of snow that have been altered by time and weather.
Firns are defined as a type of consolidated snow with a denser and more compact structure than fresh snowfall but not as dense as glacial ice. They are transitional formations between snow and ice in the process of glacial formation. Firns are typically found in regions of high elevation, where accumulating snow remains throughout the year.
The formation of firns occurs through several stages. Initially, fresh snow accumulates on the surface and undergoes compaction due to the weight of subsequent snowfall. Over time, continued accumulation and further compaction cause the air between the snow grains to be expelled. This expulsion leads to an increase in density and the conversion of snow into firn.
Firns typically exhibit a granular appearance and a bluish hue. Their density is noticeably higher than fresh snow but still considerably lower than solid ice. This porosity allows firns to retain a small amount of their original structure, enabling them to retain some air bubbles. However, they differ from snow in that they cannot be easily compacted or kicked up as loose powder.
Firns play a significant role in glacier formation and dynamics. Under specific conditions, the further compaction of firns can eventually lead to the formation of glacier ice. Consequently, firns serve as an intermediate stage in the transformation of snowfall into long-lasting glaciers, playing a crucial role in the preservation and accumulation of freshwater reserves in ice-rich regions around the world.
The word "firn" is derived from the Middle High German term "vurne", which means "last year's snow" or "old snow". This German term is ultimately derived from the Old High German word "firni", meaning "old" or "aged". The usage of "firn" in English to specifically refer to partially compacted snow came into existence in the mid-19th century.