November 2, 2024

“Jaw-Dropping” New Clues to Future Ice Sheet Change From Ancient Ice Age Valleys

The deep valleys carried large quantities of meltwater far from under the ice sheets that covered the UK and Europe. Credit: James Kirkham/ BAS
Deep valleys buried under the seafloor of the North Sea record how the ancient ice sheets that used to cover the UK and Europe expelled water to stop themselves from collapsing.
A brand-new research study greatly amazed the research group, who discovered that the valleys took just hundreds of years to form as they transported large quantities of meltwater away from under the ice and out into the sea. When the huge ice sheets melted 20,000 years earlier has ramifications for how glaciers may react to climate warming today, this new understanding of. The results were published on October 5, 2022, in the journal Quaternary Science Reviews.
Tunnel valleys are enormous channels that drain pipes water from below melting ice sheets. They are in some cases approximately 150km (93 miles) long, 6km (4 miles) large, and 500m (1600 feet) deep (each numerous times bigger than Loch Ness). There are thousands buried below the seafloor of the North Sea that record the melting of ice sheets that have actually covered the UK and Western Europe over the last two million years.

This brand-new paper responses these concerns by hunting for clues about how tunnel valleys are worn down in the 3D seismic reflection data, and utilizing modern computer simulations of the last ice sheet to cover the UK to compute how quickly the tunnels form underneath a rapidly melting ice sheet. The results have crucial ramifications for how the modern Greenland and Antarctic ice sheets will develop in the future. The authors highlight the need to consider crucial small processes that can not be solved in the present generation of ice sheet models– in essence, a mechanism that is missing out on from models of how ice sheets will melt in the future and contribute to water level increase.
The novel data used in this study were recycled from the oil and gas market. The information were offered a new lease of life by analyzing ancient glacial epoch landscapes that offer a window into a future warmer world that we are heading towards due to environment change. These new information were combined with restorations from a state-of-the-art computer model of the ice sheet that used to cover the UK (the BRITICE-CHRONO task) led by scientists at the University of Sheffield.
The seismic data were originally collected by Gardline Limited, a UK-based website study company that established the first 3D high-resolution seismic system to operate effectively in the North Sea. The data were initially used for risk assessments at drill sites but it was clear from the beginning that the seismic data had even more to provide, especially in the scholastic world.
This research was conducted by the British Antarctic Survey in cooperation with the Scott Polar Research Institute at the University of Cambridge, the University of Manchester, the University of Sheffield, the British Geological Survey, and the Geological Survey of Norway. The high-resolution 3D seismic reflection data was collected by Gardline Limited on behalf of companies consisting of Harbour Energy, Equinor Energy AS, and bp.

Lead author James Kirkham, from the University of Cambridge and the British Antarctic Survey (BAS), says:
” This is an interesting discovery. We understand that these spectacular valleys are carved out throughout the death throes of ice sheets. By utilizing a combination of cutting edge subsurface imaging techniques and a computer design, we have learned that tunnel valleys can be eroded quickly below ice sheets experiencing severe warmth.”
Seismic images
The research study group analyzed jaw-droppingly detailed seismic images that provide a 3D scan of the Earths buried layers. Informed by fragile clues found within the valleys, the scientists carried out a series of computer modeling experiments to imitate valley advancement. This allowed them to evaluate how quickly they formed as the last ice sheet to cover the UK disappeared at the end of the most recent ice age about 20,000 years earlier.
According to the findings, this process is fast by geological timescales, with the melting ice forming giant tunnel valleys within centuries, expelling water that could otherwise accelerate rates of ice loss.
Typically, the drain of water from below ice sheets is believed to support ice circulation, a process that could possibly buffer modern ice sheets from collapse in a warming environment. Nevertheless, while inspecting the detailed seismic scans, the authors started to discover telltale signatures of both rapid and stagnant ice motion within the valleys,. These made complex the image of how these quickly forming channels may impact future ice sheet behavior.
What is particular, is that the surprisingly quick rate at which these tunnels form suggests that researchers need to begin considering their results in models of how todays ice sheets will develop in the coming decades to centuries.
There are no modern-day analogs for this rapid procedure, however these ancient valleys, now buried numerous meters below the muds of the North Sea seafloor, record a system for how ice sheets react to severe heat that is missing out on from present-day ice sheet designs. Such models do not currently fix fine-scale water drainage procedures, in spite of them seeming an essential control on future ice loss rates and ultimately water level increase.
Credit: BAS
James Kirkham continues:
” The rate at which these giant channels can form ways that they are a crucial, yet presently disregarded, mechanism that might potentially assist to stabilize ice sheets in a warming world. As environment modification continues to drive the retreat of the modern-day Greenland and Antarctic ice sheets at ever-increasing rates, our results require renewed examination of how tunnel valleys may assist to stabilize modern ice losses, and for that reason sea level increase, if they turn on underneath the Earths ice sheets in the future.”
This research study allows scientists to comprehend ice sheet melting processes in order to forecast what may occur to the polar ice sheets in the future. Credit: Huw Griffiths/ BAS
Dr. Kelly Hogan, co-author and a geophysicist at BAS, states:
” We have actually been observing these substantial meltwater channels from locations covered by ice sheets in the past for more than a century however we did not actually comprehend how they formed. Our outcomes show, for the very first time, that the most crucial system is probably summer melting at the ice surface that makes its way to the bed through cracks or chimneys-like avenues and then streams under the pressure of the ice sheet to cut the channels. Surface melting is currently extremely important for the Greenland Ice Sheet today, and this procedure of water transportation through the system will just increase as our climate warms. The sixty-four-thousand-dollar question now is will this “additional” meltwater circulation in channels cause our ice sheets to stream faster, or more gradually, into the sea.”
The work highlights a currently overlooked procedure that can rapidly switch on below melting ice sheets. Whether these channels will act to stabilize or destabilize the Earths contemporary ice sheets in a warming world stays a important and open concern.
Tunnel valley development beneath deglaciating mid-latitude ice sheets: Observations and modelling by James D. Kirkham, Kelly A. Hogan, Robert D. Larter, Neil S. Arnold, Jeremy C. Ely, Chris D. Clark, Ed Self, Ken Games, Mads Huuse, Margaret A. Stewart, Dag Ottesen, Julian A. Dowdeswell is released in Quaternary Science Reviews here
References:
” Tunnel valley development underneath deglaciating mid-latitude ice sheets: Observations and modelling” by James D. Kirkham, Kelly A. Hogan, Robert D. Larter, Neil S. Arnold, Jeremy C. Ely, Chris D. Clark, Ed, Self, Ken Games, Mads Huuse, Margaret A. Stewart, Dag Ottesen and Julian A. Dowdeswell, 5 October 2022, Quaternary Science Reviews.DOI: 10.1016/ j.quascirev.2022.107680.
” Growth and retreat of the last British– Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE-CHRONO restoration” by Chris D. Clark, Jeremy C. Ely, Richard C. A. Hindmarsh, Sarah Bradley, Adam Ignéczi, Derek Fabel, Colm Ó Cofaigh, Richard C. Chiverrell, James Scourse, Sara Benetti, Tom Bradwell, David J. A. Evans, David H. Roberts, Matt Burke, S. Louise Callard, Alicia Medialdea, Margot Saher, David Small, Rachel K. Smedley, Edward Gasson, Lauren Gregoire, Niall Gandy, Anna L. C. Hughes, Colin Ballantyne, Mark D. Bateman, Grant R. Bigg, Jenny Doole, Dayton Dove, Geoff A. T. Duller, Geraint T. H. Jenkins, Stephen L. Livingstone, Stephen McCarron, Steve Moreton, David Pollard, Daniel Praeg, Hans Petter Sejrup, Katrien J. J. Van Landeghem and Peter Wilson, 7 September 2022, BOREAS.DOI: 10.1111/ bor.12594.
Background details.
These delicate landforms demonstrated for the first time that tunnel valleys alter how ice sheets circulation. Pressing questions stayed over how the tunnels were cut, how quickly they formed, and how urgently researchers require to consider them when attempting to forecast how the Earths modern ice sheets will evolve in the future.

Tunnel valleys are massive channels that drain water from underneath melting ice sheets. By using a combination of advanced subsurface imaging techniques and a computer system design, we have actually learned that tunnel valleys can be worn down rapidly beneath ice sheets experiencing severe warmth.”
Traditionally, the drain of water from beneath ice sheets is believed to stabilize ice circulation, a process that could potentially buffer modern ice sheets from collapse in a warming climate. Our results show, for the first time, that the most crucial mechanism is most likely summertime melting at the ice surface that makes its method to the bed through cracks or chimneys-like channels and then flows under the pressure of the ice sheet to cut the channels. The authors highlight the requirement to consider essential small-scale processes that can not be dealt with in the existing generation of ice sheet designs– in essence, a mechanism that is missing from designs of how ice sheets will melt in the future and contribute to sea level rise.