Late Holocene glacier and climate fluctuations in the Mackenzie and Selwyn mountain ranges, northwestern Canada

• Published in: The cryosphere 2023-10, Vol.17 (10), p.4381-4397
• Main Authors: Hawkins, Adam C, Menounos, Brian, Goehring, Brent M, Osborn, Gerald, Pelto, Ben M, Darvill, Christopher M, Schaefer, Joerg M
• Format: Article
• Language: English
• Subjects: Analysis; Annual temperatures; Beryllium 10; Boulders; Catchment area; Catchments; Chronology; Cirques (landforms); Climate; Climate change; Climate models; Climate system; Cosmic rays; Digitization; Emissions; Environmental assessment; Fluctuations; Future climates; General circulation models; Glacial drift; Glacier fluctuations; Glacier melting; Glaciers; Greenhouse effect; Greenhouse gases; Holocene; Holocene glaciation; Ice ages; Ice volume; Interdisciplinary research; Interdisciplinary studies; Little Ice Age; Mean annual temperatures; Meltwater; Meteorological research; Modelling; Moraines; Mountain glaciers; Mountain regions; Mountains; National parks; Native North Americans; Precipitation; Remote sensing; Temperature changes; Valley glaciers; Valleys; Weather
• ISSN: 1994-0424; 1994-0416; 1994-0424; 1994-0416
• DOI: 10.5194/tc-17-4381-2023

Over the last century, northwestern Canada experienced some of the highest rates of tropospheric warming globally, which caused glaciers in the region to rapidly retreat. Our study seeks to extend the record of glacier fluctuations and assess climate drivers prior to the instrumental record in the Mackenzie and Selwyn mountains of northwestern Canada. We collected 27 10Be surface exposure ages across nine cirque and valley glacier moraines to constrain the timing of their emplacement. Cirque and valley glaciers in this region reached their greatest Holocene extents in the latter half of the Little Ice Age (1600–1850 CE). Four erratic boulders, 10–250 m distal from late Holocene moraines, yielded 10Be exposure ages of 10.9–11.6 ka, demonstrating that by ca. 11 ka, alpine glaciers were no more extensive than during the last several hundred years. Estimated temperature change obtained through reconstruction of equilibrium line altitudes shows that since ca. 1850 CE, mean annual temperatures have risen 0.2–2.3 ∘C. We use our glacier chronology and the Open Global Glacier Model (OGGM) to estimate that from 1000 CE, glaciers in this region reached a maximum total volume of 34–38 km3 between 1765 and 1855 CE and had lost nearly half their ice volume by 2019 CE. OGGM was unable to produce modeled glacier lengths that match the timing or magnitude of the maximum glacier extent indicated by the 10Be chronology. However, when applied to the entire Mackenzie and Selwyn mountain region, past millennium OGGM simulations using the Max Planck Institute Earth System Model (MPI-ESM) and the Community Climate System Model 4 (CCSM4) yield late Holocene glacier volume change temporally consistent with our moraine and remote sensing record, while the Meteorological Research Institute Earth System Model 2 (MRI-ESM2) and the Model for Interdisciplinary Research on Climate (MIROC) fail to produce modeled glacier change consistent with our glacier chronology. Finally, OGGM forced by future climate projections under varying greenhouse gas emission scenarios predicts 85 % to over 97 % glacier volume loss by the end of the 21st century. The loss of glaciers from this region will have profound impacts on local ecosystems and communities that rely on meltwater from glacierized catchments.