Cryopedology
Cryopedology ko kala wiɗto jowitiingo e leydi e nguleeki les 0 degereeji Celsius, tawa ina teskaa e golle ɓuuɓɗe tiiɗɗe e leydi ɓuuɓndi duumiindi, permafrost, walla leydi ɓuuɓndi duumiindi, pergelisol.Ɗum ina jeyaa heen peeñgol mum en, ɓuuɓgol mum en, sabaabuuji mum en, kewuuji mum en gila e golle caɗtuɗe helmere cryopedology ndee ko ganndo leydi biyeteeɗo Kirk Bryan adii yaltude e hitaande 1946.Nafooje faggudu ummoraade e mahngo laabi e gollorɗe e nder Arktik ina njahda e ndeeɗoo fannu wiɗto.
Sifaaaji ɗi nees ɓuuɓɗo oo fuɗata e henndu (yeru e dow tundra) ina wiyee ko ‘formations cryopedologiques’. Laabi ɗi neesuuji ɓuuɓɗi mbaɗata sabu geɗe baɗɗe e nder mum e jowitiiɗe e nokkuuji ko ‘geɗe kiriyopedoloji’.[1]
Tuugnorgal
[taƴto | taƴto ɗaɗi wiki]The shapes into which frozen snow is blown by the wind (e.g. on the tundra) are said to be 'cryopedological formations'. The ways in which frozen snow behaves due to factors intrinsic to itself and relating to environments are 'cryopedological processes'. [4]
- ↑ "cryopedology". National Snow and Ice Data Center (in Engeleere). Retrieved 2024-02-26.