Scientists have discovered massive ancient icebergs that drifted across the North Sea about 18,000 years ago. These giant icebergs, comparable in size to mid-sized cities, left noticeable grooves on the seabed. This finding offers fascinating insights into our planet’s climate history.
During the last Ice Age, ice sheets blanketed much of northern Europe. As these sheets began to melt, huge chunks of ice broke away and floated into the North Sea, reaching the shores of Britain. Researchers from the British Antarctic Survey, led by James Kirkham, found these grooves through seismic survey data, usually collected for oil and gas exploration.
According to Kirkham, some of these icebergs were between five to tens of kilometers wide and possibly a few hundred meters thick. Their size indicates they played a significant role in shaping the landscape at the time.
Recent studies highlight that these enormous icebergs suggest the region once had ice shelves similar to today’s Antarctic shelves. In fact, today’s tabular icebergs—flat-topped ice masses—continue to break off from Antarctica. Some of the largest, like A23a and A68a, rival small U.S. states in size. The behavior of these icebergs provides vital clues about how ice shelves respond to temperature changes.
The evidence from the North Sea seabed reveals a shift in iceberg sizes over time. The large scour marks from these ancient icebergs are now covered by smaller, squiggly troughs made by much tinier ice chunks. This suggests a decline in the size of icebergs as global temperatures rose, leading to what Kirkham describes as a “regime change.”
These findings challenge our understanding of ice shelf stability. Emma MacKie from the University of Florida points out that large calving events—where big chunks of ice break away—aren’t always signs of instability. Instead, the more pressing concern may be the gradual disintegration of ice shelves over time. Her research, tracking tabular icebergs since the mid-1970s, indicates that while large calving events have stabilized, a continuous cycle of smaller events could lead to more significant ice loss and higher sea levels.
In summary, the behavior of these ancient icebergs not only sheds light on past climate but also raises important questions about our current situation. As we face rising temperatures, understanding these dynamics is crucial for predicting future sea-level changes.