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85 new subglacial lakes discovered in Antarctica: CryoSat satellite reveals hidden climate-critical water world

By analyzing decades of data from the European Space Agency's CryoSat satellite, scientists have discovered 85 previously unknown subglacial lakes under the ice of Antarctica. This discovery of a dynamic water system is key to understanding the stability of the ice sheet and improving projections of global sea level rise.

85 new subglacial lakes discovered in Antarctica: CryoSat satellite reveals hidden climate-critical water world

Beneath the vast, seemingly motionless ice cap of Antarctica, lies a dynamic and complex world about which humanity knows surprisingly little. Deep under kilometers of ice, in eternal darkness, there is a vast network of rivers and lakes that plays a crucial role in the stability of the entire continent, and thus in the future of global sea levels. Recent discoveries, made possible by advanced satellite technology, have shed new light on this hidden water system, revealing that it is far more active and complex than previously thought. At the heart of this breakthrough is the identification of as many as 85 previously unknown subglacial lakes, increasing the number of known active water bodies under the Antarctic ice by more than fifty percent.


A Satellite Eye that Pierces Through Ice


This revolutionary discovery would not have been possible without the tireless work of the European Space Agency's (ESA) CryoSat satellite. Launched in 2010, CryoSat was designed with one primary goal: to precisely measure the thickness of polar sea ice and monitor changes in the height of the ice sheets in Greenland and Antarctica. Its key instrument, a radar altimeter, is capable of detecting even the smallest, subtle variations in the height of the ice surface. It is precisely this capability that has allowed scientists to "see" what is happening kilometers below. Specifically, when a subglacial lake fills with water, the ice surface above it rises slightly, sometimes by only a few meters. When the lake drains, the surface subsides. By analyzing data collected over an entire decade, from 2010 to 2020, researchers were able to create a detailed map of these filling and draining cycles, revealing the locations of lakes that had been completely invisible until now.


Thanks to this decade-long data series, scientists were able to identify 12 complete filling and draining cycles, bringing the total number of such recorded events in the world to 48. This is a significant step forward in understanding processes that are extremely difficult to observe due to their inaccessibility. As explained by Sally Wilson, a PhD candidate at the University of Leeds and lead author of the study published in the prestigious journal Nature Communications, knowledge about subglacial lakes and the flow of water under the ice was very limited precisely because they are hidden under hundreds, and even thousands, of meters of ice. Observing these events in such conditions presents a huge scientific challenge.


An Expanded Map of the Hidden Water World


With the discovery of 85 new lakes, the total number of known active subglacial water bodies in Antarctica has grown to 231. But the significance of the study goes beyond mere numbers. The research also revealed new, previously unknown drainage paths under the ice sheet, including five interconnected networks of subglacial lakes. This suggests the existence of a complex "plumbing system" that transports huge amounts of water under the ice, affecting the dynamics of the entire ice sheet.


Professor Anna Hogg from the University of Leeds, a co-author of the study, highlighted the fascinating insight that the areas of subglacial lakes can change during different filling and draining cycles. "This shows that the subglacial hydrology of Antarctica is much more dynamic than previously thought, so we must continue to monitor these lakes as they evolve in the future," she emphasized. This dynamic is key to understanding how the ice sheet behaves and how it will respond to further climate change.


How Do Subglacial Lakes Form and Why Are They Important?


Subglacial meltwater is formed by a combination of two processes: geothermal heat radiating from the Earth's interior and heat generated by friction as massive glaciers slowly move over the rocky bedrock. This water can accumulate in depressions in the rock, forming lakes that periodically drain. The flow of this water has an extremely important consequence: it acts as a lubricant, reducing the friction between the ice and the rock it rests on. Reduced friction allows the ice to slide faster towards the ocean, thus accelerating the process of ice mass loss from the continent and directly contributing to global sea-level rise.


However, not all subglacial lakes are active. Many are considered stable because they are not known to fill or drain. The largest known subglacial lake in the world is Lake Vostok, located under almost four kilometers of ice in East Antarctica. It is estimated to contain between 5,000 and 65,000 cubic kilometers of water, enough to fill and overflow the Grand Canyon at least 25 times. Although Vostok is considered stable, its eventual draining would have cataclysmic consequences for the stability of the Antarctic ice sheet, the circulation of the surrounding ocean, marine ecosystems, and, of course, global sea levels. It serves as a powerful reminder of the immense forces at work beneath the ice.


The Missing Link in Climate Models


One of the most important contributions of this research lies in its application to climate modeling. Existing numerical models used to project the contribution of entire ice sheets to sea-level rise often do not include subglacial hydrology. Simply put, the complex water system under the ice represents the "missing link" in our predictions of the future.


Sally Wilson explains: "By mapping where and when these lakes are active, we can begin to quantify their impact on ice dynamics and improve projections of future sea-level rise." New datasets on the locations, extent, and time series of changes in subglacial lakes will be invaluable for developing more sophisticated models that more accurately reflect the actual processes. Martin Wearing, coordinator of the Polar Science Cluster at the ESA, confirmed the importance of the CryoSat mission, pointing out that it once again proves its key role in improving our understanding of the polar regions. The more we know about the complex processes that affect the Antarctic ice sheet, including the flow of meltwater at its base, the more accurately we will be able to predict the scale of future sea-level rise – information of vital importance to all of humanity.

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