Underground World Revealed: Clarity Like Never Before
- For decades, what lies beneath Antarctica's miles-thick ice sheet has remained largely unknown.
- Published in the prestigious journal Science, the study details how researchers analyzed satellite observations of Antarctica's ice surface and applied the physics governing how glaciers flow to calculate...
- Helen Ockenden describes the resulting map as a transition "from a blurry film camera to a high-resolution digital image." According to Ockenden, the structure beneath Antarctica is now...
For decades, what lies beneath Antarctica‘s miles-thick ice sheet has remained largely unknown. Now,a new map created by scientists reveals the landscape under the ice with unprecedented detail.
Published in the prestigious journal Science, the study details how researchers analyzed satellite observations of Antarctica’s ice surface and applied the physics governing how glaciers flow to calculate the underlying bedrock topography. The result is the discovery of thousands of previously unknown peaks, ridges, and subglacial mountain ranges.
Study led author Dr. Helen Ockenden describes the resulting map as a transition “from a blurry film camera to a high-resolution digital image.” According to Ockenden, the structure beneath Antarctica is now visible more clearly than ever before.
Previously, scientists relied on radar measurements taken from the ground or air to “see” beneath the ice. However, these measurements were often taken along lines tens of kilometers apart, with gaps filled in by assumptions. The new method analyzes small changes in the ice surface and variations in flow speeds to trace the contours of the rock below.
Researchers compare this process to understanding the rocks beneath the surface of a river by observing the whirlpools in the water. As ice flows over rock ridges and peaks,it alters both its surface shape and speed,providing clues about the topography underneath.
The new map especially details hidden mountainous regions in East Antarctica and a massive subglacial channel within the Maud Basin, approximately 400 kilometers long, averaging 50 meters deep, and 6 kilometers wide. This channel is roughly the distance between London and Newcastle.
Researchers emphasize that the map isn’t definitive; assumptions about ice flow contain uncertainties, and much remains unknown about the rock and sediments beneath the ice. Nevertheless, the study is being hailed as a significant turning point in the scientific community.
enabling Better Modeling of Future Movement
Experts highlight that this level of detail will allow for more accurate modeling of how Antarctic glaciers will move in the future. The mountains, valleys, and channels beneath the ice directly influence glacial speed and retreat.
This, in turn, could provide clearer answers to questions about how quickly Antarctica is melting and how much it will contribute to global sea level rise. According to scientists, Antarctica’s future melt rate remains one of the biggest unknowns in climate science.
Source: Gazete Oksijen
