AUS
NZ
UK
CA
USA
FRA
GER
ESP
ITA
NLD
PRT
SWE
GRC
IND
POL
BRA
ZAF
RUS
CHN
UAE
The findings, published in the peer-reviewed journal Geophysical Research Letters, reveal an alarming acceleration in glacier melt rates in the regions between 2021 and 2024 – doubling the pace observed in the previous decade.
During the four-year span, glaciers in western Canada and the conterminous United States lost approximately 22.2 gigatonnes of ice per year, while Swiss glaciers lost 1.5 gigatonnes annually. Since 2020, total ice volumes declined by 12 per cent and 13 per cent, respectively.
To put the loss in Western North America into perspective, that’s enough meltwater to submerge the metropolitan area of Toronto (630 km²) under 35 metres of water each year.
“Even against the backdrop of rapid glacier loss since the start of this century, what we’re witnessing now is unprecedented,” says Menounos, a Professor in UNBC’s Department of Geography, Earth and Environmental Sciences. “The melt rates over the last four years far exceed anything we’ve observed in the past six decades, posing serious implications for freshwater availability, increased geohazard risks and the loss of cultural and tourism values tied to mountain landscapes.”
With funding from the Tula Foundation and the National Science and Engineering Research Council of Canada, Menounos worked with scientists from the Hakai Institute, Natural Resources Canada (Geological Survey of Canada), Environment and Climate Change Canada, the United States Geological Survey and researchers from Europe. The team used airborne laser altimetry data from the Hakai Airborne Coastal Observatory in addition to other datasets and modeling to calculate the glacier mass loss reported in the study.
In both regions, the researchers identified a combination of factors driving the record losses: low winter snow accumulations, early-season heat waves and prolonged warm, dry conditions.
“We’re seeing the effects of meteorological events compounding one another – these conditions rapidly depleted snowpacks, exposing darker glacier ice and firn – multiyear snow - which can absorb more energy from sunlight and further accelerate melting,” says Menounos. “We believe these firn and ice surfaces are becoming darker from deposition of ash in Western North America and Saharan dust in Europe. Unfortunately, this darkening provides unhelpful feedback in a warming climate that will allow high melt rates to continue.”
Based on projected rates of glacier mass loss to 2060, the study is consistent with previous research suggesting the period of peak glacier runoff – when meltwater contributions to rivers are at their highest - has likely already occurred and streamflow from glaciers will decline in coming decades.
The researchers are advocating for improved, next-generation physical models that better represent the response of glaciers to extreme weather events and processes like surface impurity deposition from dust and wildfires.
“Current global models of glacier change do not include ways to track physical processes which lead to glacier darkening’, says Menounos “If we’re going to plan for the future, we need to improve our physical models to include these critical feedbacks."
Michelle Cyr-Whiting, Communications Officer
University of Northern British Columbia
+1 250-612-7249
[email protected]
Legal Disclaimer:
EIN Presswire provides this news content "as is" without warranty of any kind. We do not accept any responsibility or liability for the accuracy, content, images, videos, licenses, completeness, legality, or reliability of the information contained in this article. If you have any complaints or copyright issues related to this article, kindly contact the author above.
