Greenland's groundwater changes with thinning ice sheet

Date:
October 12, 2021
Source:
The University of Montana
Summary:
For more than a decade, a team of researchers and students have
studied the dynamics of the Greenland Ice Sheet as it responds to
a warming climate. But while much of their focus has been on the
importance of water in controlling processes occurring on the ice
sheet, their most recent research findings have flipped the order
of their thinking.

Researchers discovered that changes to the ice sheet have an
immediate impact on the groundwater underlying the Greenland island,
an area larger than the state of Alaska.



FULL STORY ==========================================================================
For more than a decade, a team of University of Montana researchers
and students have studied the dynamics of the Greenland Ice Sheet as
it responds to a warming climate. Department of Geosciences researchers
Toby Meierbachtol and Joel Harper said water has always been central to
their research.


==========================================================================
"The water from melting of the ice can run off the surface to the ocean
and contribute to sea level rise, it can refreeze in place and actually
warm the ice, and it can even reach the bottom of the ice sheet and
act as a sort of lubricant to make the ice slide quickly over its bed," Meierbachtol said. "The importance of water in controlling the response
of Greenland to warming is hard to overstate." But while much of their
focus has been on the importance of water in controlling processes
occurring on the ice sheet, their most recent research findings have
flipped the order of their thinking.

As outlined in their recent article in Nature Geoscience, Meierbachtol,
Harper and an international team of researchers discovered that changes
to the ice sheet have an immediate impact on the groundwater underlying
the Greenland island, an area larger than the state of Alaska.

"We have been focused on water's impacts on ice sheet change," said
Harper.

"But our most recent findings show that changes in the ice sheet
have a real impact on Arctic hydrology -- specifically the massive
groundwater system extending under the ice sheet." This latest revelation occurred thanks to a marriage of drilling techniques, with international collaborators boring an angled hole 650 meters through bedrock underneath
a Greenland glacier to measure groundwater conditions deep under the
ice sheet. Meanwhile, UM and University of Wyoming researchers drilled
32 holes from atop the glacier, through nearly a kilometer of ice,
to measure water conditions at the interface between ice and bedrock,
which forms an important boundary controlling groundwater flow below.



==========================================================================
The system that UM has perfected over the years involves drilling with
a combination of very hot water under high pressure typically for 12 or
more hours at a time.

"We practice and rehearse to make the operation flow smoothly," Harper
said, noting they always include one to two undergraduate students on
an expedition.

"Everyone on the team has an important and specific role to fill."
After drilling the team installs sensors in the ice column and at the
ice sheet bed to measure ice dynamics and water conditions as water flows
under the ice to margin. Time is always of the essence because the cold
ice freezes the hole shut in as little as two hours.

The dual drilling approach facilitated the first-ever measurements of groundwater response to a changing ice sheet, and the eight-year data
record yielded some unexpected results.

"By studying areas that were covered by ice 10,000 years ago during the
last ice age, the field has known that the huge mass and vast amounts
of water from melting ice can impact the underlying groundwater,"
Meierbachtol said, "but the paradigm has been that the groundwater
response to ice sheet change is long: thousands of years. What we've shown
here is that the groundwater response to Greenland's change is immediate."
This new understanding could have important downstream implications for
how Greenland's thinning impacts the Arctic, Harper said. The thinning
ice could reduce the rate of groundwater flow to the ocean, changing
the water temperature and salinity balance that is important for ocean circulation patterns.

"In thinking about the complex feedbacks that occur from Greenland's
ongoing change, we as a field have really neglected the groundwater
component because we thought it was more or less dormant over the decade
to century timescales that are important for us as a society," Harper
said. "But now we recognize that the groundwater system actually changes
quite rapidly, and there are some compelling reasons for why this could
really matter for the broader Arctic." Future research will need to
work toward quantifying the impacts of groundwater change on the ocean,
both Meierbachtol and Harper noted. But the first step was the discovery.

========================================================================== Story Source: Materials provided by The_University_of_Montana. Note:
Content may be edited for style and length.


========================================================================== Journal Reference:
1. Lillemor Claesson Liljedahl, Toby Meierbachtol, Joel Harper,
Dirk van As,
Jens-Ove Na"slund, Jan-Olof Selroos, Jun Saito, Sven Follin,
Timo Ruskeeniemi, Anne Kontula, Neil Humphrey. Rapid and
sensitive response of Greenland's groundwater system to ice
sheet change. Nature Geoscience, 2021; 14 (10): 751 DOI:
10.1038/s41561-021-00813-1 ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2021/10/211012130719.htm

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