Globe's glaciers have less ice than previously thought
Findings on glacier speed and depth revise outlook for freshwater
availability and sea level rise

Date:
February 7, 2022
Source:
Dartmouth College
Summary:
Research revises estimates of glacial ice volume, suggesting
that there is less ice in the world's glaciers than previously
thought. The findings have implications on freshwater and global
sea level rise.



FULL STORY ==========================================================================
The first atlas to measure the movement and thickness of the world's
glaciers gives a clearer, but mixed picture of the globe's ice-bound
freshwater resources, according to researchers from the Institute of Environmental Geosciences (IGE) and Dartmouth College.


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The worldwide survey, published in Nature Geoscience, measures the
velocity and depth of more than 250,000 mountain glaciers. The research
revises earlier estimates of glacial ice volume, now suggesting that
there is 20% less ice available for sea level rise in the world's glaciers
than previously thought.

The results have implications on the availability of water for drinking,
power generation, agriculture and other uses worldwide. The findings
also change projections for climate-driven sea level rise expected to
affect populations around the globe.

"Finding how much ice is stored in glaciers is a key step to anticipate
the effects of climate change on society," said Romain Millan, a
postdoctoral scholar at IGE and lead author of the study. "With this information, we will be closer to knowing the size of the biggest glacial
water reservoirs and also to consider how to respond to a world with
less glaciers." "The finding of less ice is important and will have implications for millions of people around the world," said Mathieu
Morlighem, the Evans Family Professor of Earth Sciences at Dartmouth and co-author of the study. "Even with this research, however, we still don't
have a perfect picture of how much water is really locked away in these glaciers" The new atlas covers 98% of the world's glaciers. According
to the study, many of these glaciers are shallower than estimated in
prior research. Double counting of glaciers along the peripheries of
Greenland and Antarctica also clouded previous data sets.



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The study found less ice in some regions and more ice in others,
with the overall result that there is less glacial ice worldwide than previously thought.

The research found that there is nearly a quarter less glacial ice in
South America's tropical Andes mountains. The finding means that there
is up to 23% less freshwater stored in an area from which millions of
people depend during their everyday lives. The reduction of this amount
of freshwater is the equivalent of the complete drying of Mono Lake, California's third largest lake.

On the contrary, Asia's Himalayan mountains were found to have over
one-third more ice than previous estimates. The result suggests that about
37% more water resources could be available in the region, although the continent's glaciers are melting quickly.

"The overall trend of warming and mass loss remains unchanged. This
study provides the necessary picture for models to offer more reliable projections of how much time these glaciers have left," said Morlighem.

The melting of glaciers due to climate change is one of the main causes
of rising sea levels. It is currently estimated that glaciers contribute
25-30% to overall sea level rise, threatening about 10% of the world's population living lower than 30 feet above sea level.



==========================================================================
The reduction by 20% of glacial ice available for sea level rise lessens
the potential for glacial contribution to sea level by 3 inches, revising
it downward from 13 inches to just over 10 inches. This projection
includes contributions from all the world's glaciers except the two
large ice sheets of Greenland and Antarctica, which have a much larger potential contribution to sea level rise.

"Comparing global differences with previous estimates is just one side
of the picture," said Millan. "If you start looking locally, then the
changes are even larger. To correctly project the future evolution of
glaciers, capturing fine details is much more important than just the
total volume." According to the study, depth measurements previously
existed for only about 1% of the world's glaciers, with most of those
glaciers only being partially studied.

The glacial ice estimates that did exist prior to the new study
were almost entirely uncertain, according to the research team. The
uncertainty is due, in part, to the lack of ice flow measurements showing
the location of thick and thin ice, all of which is gathered through
indirect techniques.

To create the massive ice flow database, the research team studied more
than 800,000 pairs of satellite images of glaciers, including large ice
caps, narrow alpine glaciers, slow valley glaciers and fast tidewater
glaciers. The high- resolution images were acquired between 2017-18 by
NASA's Landsat-8 and the European Space Agency's Sentinel-1 and Sentinel-2 satellites. The data was processed using more than 1 million hours of computation at IGE.

"We generally think about glaciers as solid ice that may melt in the
summer, but ice actually flows like thick syrup under its own weight,"
said Morlighem.

"The ice flows from high altitude to lower elevations where it eventually
turns to water. Using satellite imagery, we are able to track the motion
of these glaciers from space at the global scale and, from there, deduce
the amount of ice all around the world." The resulting first global
map of flow velocities covers most of the world's terrestrial glaciers, including regions where no previous mapping existed, such as the southern cordilleras of South America, sub-Antarctic islands, and New Zealand.

Although the new atlas marks a major improvement in glacier ice and water potential estimates, the thickness distribution of the world's glaciers
is still subject to large gaps of information.

"Our estimations are closer, but still uncertain, particularly in regions
where many people rely on glaciers," said Millan. "Collecting and sharing measurements is complicated, because glaciers are spread throughout
so many countries with different research priorities." According to
the team, without direct field measurements, the estimate of glacier
freshwater resources will remain uncertain.

The study calls for a re-evaluation of the evolution of the world's
glaciers in numerical models as well as direct observations of ice
thicknesses in the tropical Andes and the Himalayas, which are major
water towers but that remain poorly documented.

Je're'mie Mouginot and Antoine Rabatel, of the Institute of Environmental Geosciences (IGE) -- Grenoble Alpes University, the French National
Center for Scientific Research (CNRS), the French National Research
Institute for Sustainable Development (IRD) and Grenoble INP Graduate
Schools of Engineering and Management, made significant contributions
to the study. Millan and Morlighem conducted part of the research at the University of California Irvine. Millan is also affiliated with CNRS and
the Department of Geosciences and Natural Resources Management of the University of Copenhagen. Research was supported by France's National
Center for Space Studies (CNES).

========================================================================== Story Source: Materials provided by Dartmouth_College. Original written
by David Hirsch.

Note: Content may be edited for style and length.


========================================================================== Journal Reference:
1. Millan, R., Mouginot, J., Rabatel, A. et al. Ice velocity and
thickness
of the world's glaciers. Nat. Geosci., 2022 DOI: 10.1038/s41561-021-
00885-z ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2022/02/220207112647.htm

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