A type of old snow which has gone through multiple thaw and refreeze cycles and thus is made of numerous small icy grains, though it is not nearly as saturated with water as snow-cone slush is; can be hard or somewhat soft depending on recent and current weather conditions, Névé on a glacier that survives the year's ablation season With time much of the firn is transformed into glacial ice, A permeable aggregate of small ice grains with densities greater than 0 55 up to 0 82 where begins glacial ice, consolidated granular snow left over from the previous year Closer to ice than snow in density, it may require the use of crampons, An intermediate stage in the conversion of snow to ice through accumulation, a type of old snow which has gone through multiple thaw and refreeze cycles and thus is made of numerous small icy grains, though is not nearly as saturated with water as snow-cone slush is; can be hard or somewhat soft depending on recent and current weather conditions, Old snow that has become granular and compacted as a result of melting and refreezing, or neve snow that has lain on the ground for a full calendar year Firn is common at the tops of mountains; for example, the Alps in Europe After many years, compaction turns fim into ice and aglacier forms, Material that is transitional between snow and glacier ice It is formed from snow after passing through one summer melt season and becomes glacier ice after its permeability to liquid water falls to zero (Source: Carbon Dioxide Information Analysis Center, 1990), Old snow on top of glaciers, granular and compact and not yet converted into ice It is a transitional stage between snow and ice Also called Neve, (firn snow) Old snow on the top of glaciers, granular and compact but not yet converted into ice It is a transitional stage between snow and ice Also called ne've', An imperfectly consolidated mixture of granular snow and ice that will ultimately become ice alone as time progresses, a material transitional between snow and glacier ice Snow becomes firn after existing through one summer melt season; firn becomes glacial ice when its permeability to liquid water becomes zero, Firmly packed snow that has survived a summer melting season Firn has a density of about 0 4 gram per cubic centimeter Ultimately, firn turns into glacial ice, Granular, partially consolidated snow that has passed through one summer melt season but is not yet glacial ice. Also called old snow,
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A type of old snow which has gone through multiple thaw and refreeze cycles and thus is made of numerous small icy grains, though it is not nearly as saturated with water as snow-cone slush is; can be hard or somewhat soft depending on recent and current weather conditions
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Névé on a glacier that survives the year's ablation season With time much of the firn is transformed into glacial ice
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A permeable aggregate of small ice grains with densities greater than 0 55 up to 0 82 where begins glacial ice
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consolidated granular snow left over from the previous year Closer to ice than snow in density, it may require the use of crampons
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An intermediate stage in the conversion of snow to ice through accumulation
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a type of old snow which has gone through multiple thaw and refreeze cycles and thus is made of numerous small icy grains, though is not nearly as saturated with water as snow-cone slush is; can be hard or somewhat soft depending on recent and current weather conditions
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Old snow that has become granular and compacted as a result of melting and refreezing
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or neve snow that has lain on the ground for a full calendar year Firn is common at the tops of mountains; for example, the Alps in Europe After many years, compaction turns fim into ice and aglacier forms
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Material that is transitional between snow and glacier ice It is formed from snow after passing through one summer melt season and becomes glacier ice after its permeability to liquid water falls to zero (Source: Carbon Dioxide Information Analysis Center, 1990)
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Old snow on top of glaciers, granular and compact and not yet converted into ice It is a transitional stage between snow and ice Also called Neve
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(firn snow) Old snow on the top of glaciers, granular and compact but not yet converted into ice It is a transitional stage between snow and ice Also called ne've'
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An imperfectly consolidated mixture of granular snow and ice that will ultimately become ice alone as time progresses
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a material transitional between snow and glacier ice Snow becomes firn after existing through one summer melt season; firn becomes glacial ice when its permeability to liquid water becomes zero
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Firmly packed snow that has survived a summer melting season Firn has a density of about 0 4 gram per cubic centimeter Ultimately, firn turns into glacial ice
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Granular, partially consolidated snow that has passed through one summer melt season but is not yet glacial ice. Also called old snow
Some etymologies, pronunciations, function and usage date content for the English translation portion are from Merriam-Webster Online at www.Merriam-Webster.com. Thanks to Online Yunanca Dil Eğitimi for providing some parts of online greek dictionary. To contribute more resources please contact us. Visuals(images) are provided by Google Image Search API. Some parts of the dictionary is contributed by many users, thank you! The content on this site is for informational purposes only. Bu aramada firn kelimesinin sözlük anlamı ve eşanlamı nedir, nasıl okunur hakkında bilgi verilmektedir. firn kelimesinin etimolojik ve eşanlamları ile ilgili açıklamalar ve bilgiler eksiksiz ve hatasız olarak anılmamalıdır. Burada yer alan firn kelimesi ile ilgili tüm açıklamalar bilgi amaçlıdır. Eksik ve hatalı çevirileri lütfen bildiriniz.
