This report is focused on answering the questions: how has Canada’s climate changed to date, why, and what changes are projected for the future?

We studied dissolved methane dynamics within a small Mackenzie River Delta lake, autonomously and continuously collecting water samples for two years at various depths.

We present a database of western North American Holocene paleoclimate records from 184 terrestrial and marine sites, spanning at least 4000 of the last 12,000 years.

The paleolimnological record of diatoms and climate, spanning the last 2800 years, was investigated in a small subarctic lake (Pocket Lake).

This is research on the Ragged Range glaciers in NWT. Approximately 110 km² of glacier cover has been lost over the last 35 years.

This compendium addendum provides a summary of the most significant academic literature about climate change in the NWT, that has been published by Wilfrid Laurier University...

This compendium addendum provides a summary of the most significant academic literature about climate change in the NWT, that has been funded by the CIMP program.

This open file presents mass balance data from glaciers in the Cordillera Glacier-Climate Observing network for the 2015 and 2016 balance years

This chapter assesses past and future climate-related changes to surface runoff (streamflow), surface water levels, soil moisture and drought, and groundwater in Canada.

This compendium provides a summary of the most significant academic literature about climate change in the NWT, organized by theme.

This report, published every four years, provides information on the state and trends of the environment in the NWT, organized over various environmental topics.