Active Layer - Qausuittuq

"Permafrost and the active layer (the soil layer above the permafrost that freezes and thaws annually) are directly affected by climate. It is anticipated that rising temperatures in the Arctic will lead to permafrost warming/melt and thickening of the active layer. Probable impacts of permafrost degradation on the tundra ecosystem include ground instability and changes to local hydrological patterns and surface vegetation.

In 2024, a Circumpolar Active Layer Monitoring (CALM) Grid was installed in Qausuittuq National Park near Dundee Bight as part of an international program to monitor the effects of climate change on the active layer and near-surface permafrost. Active layer thickness measurements are taken each summer, at 100 points within the 100 m x 100 m grid, using a metal probe. "

Data and Resources

Additional Info

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Last Updated April 17, 2026, 21:50 (UTC)
Created April 17, 2026, 21:50 (UTC)
contact_email Maryse.Mahy@pc.gc.ca
contact_person {}
criticality_level ["educators", "nongovernmental_organizations", "scientists", "students"]
data_dictionary []
geographic_scope ["62"]
open_canada_collection primary
open_canada_date_published 2024-12-16 00:00:00
open_canada_keywords {"en": ["Qausuittuq National Park", "active layer", "permafrost", "climate change", "Dundee Bight", "May Inlet", "Bathurst Island"], "fr": ["Parc national Qausuittuq", "couche active", "pergélisol", "changements climatiques", "Dundee Bight", "May Inlet", "Bathurst Island"]}
open_canada_subject ["nature_and_environment"]
sensitivity_level unrestricted
title_fr Couche active - Qausuittuq
update_frequency P1Y