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The permafrost zone covers about half of the Canadian landmass and presents unique challenges to development in the north. Within this zone, permafrost continuously underlies the land in the far north and may be several hundred metres thick. At the s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bff7427f684a697de226fa8862568351
https://doi.org/10.4095/212229
https://doi.org/10.4095/212229
Active layer and permafrost thermal state have been identified as key cryospheric variables for monitoring through the World Meteorological Organization’s Global Climate Observing System. An international network, the Global Terrestrial Network for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8982fca54aa97af0209f0cad4d2480d3
https://doi.org/10.4095/211621
https://doi.org/10.4095/211621