A puzzling past sea level rise might have its missing piece
About 14,650 years ago, sea level jumped 12 meters in just a few centuries.
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About 14,650 years ago, as the thawing of the last ice began to hit its stride, sea level made a remarkable jump of 12 meters or more—and did so in less than 400 years. It's an event known to scientists as Meltwater Pulse 1A.
Figuring out where all that water came from hasn’t been easy. ... , but models of past ice sheet change haven’t quite added up.
A new study led by Jo Brendryen at the University of Bergen takes an interesting route to discover that the melting of the Eurasian Ice Sheet, which has largely been overlooked, might just explain things.
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Back to the ice sheets. During the last glacial period, an ice sheet once stretched across Scandinavia and the Barents Sea. The record of its shrinking is based on carbon dating of seafloor sediment cores, pinpointing times that ice retreated and life returned to a location. The reconstructions have indicated that the ice here had basically melted before the start of Meltwater Pulse 1A, giving it a clear alibi. But the carbon-dated ages assumed that the deep ocean carbon-14 delay in that region was constant over time, matching the modern pattern.
In this new study, the researchers looked carefully at that assumption. They turned to a seemingly unlikely source—a cave in China. There is actually a pretty good correlation between ocean circulation, the temperatures in the North Atlantic, and the Asian Monsoon rains, linked by a series of climatic dominoes. Cave records have excellent timelines, with annual layers and uranium radiometric dating.
By lining up the wiggles in the cave record and Norwegian Sea sediment records, the researchers avoid having to guess the unknown deep ocean carbon-14 delay. Instead, they can calculate that delay and its changes, providing a new calibration for seafloor paleoclimate records in this region.
With that done, the reconstructed timing of Eurasian Ice Sheet melt shifts. Rather than showing that the local ice melted before Meltwater Pulse 1A even started, they see a major loss of ice during this event. Previous reconstructions gave the Eurasian Ice Sheet credit for perhaps one meter of the 12 or more meters of sea level rise that occurred then. This study pushes that contribution up to about five meters—plus another meter or so in the century following.
There are obvious challenges to working out which giant block of ice melted thousands of years ago. But there are valuable clues. When an ice sheet melts, sea level rise doesn’t rise equally all around the world. The gravitational attraction of a massive ice sheet actually pulls seawater to it, raising sea levels near the sheet a bit. As the ice sheet shrinks, its gravitational pull relaxes, so sea level can actually fall right next to the ice sheet, even as it rises elsewhere. And the records of sea level change in various places are actually consistent with the Eurasian Ice Sheet being a big source: sites around Norway and Finland show a drop in sea level during this period of high-speed global sea level rise.
Re-aligning the Eurasian Ice Sheet history would make it significantly easier to understand where 12 meters of sea level came from, but it also raises some interesting questions. For example, such a massive flow of freshwater into the Norwegian Sea could be expected to gum up the critically important south-to-north conveyor belt current in the Atlantic Ocean, but records indicate it was actually quite strong during this time. And how, exactly, did this portion of the Eurasian Ice Sheet collapse so quickly?
That question about the past is of interest to our future. The portion of the Eurasian Ice Sheet in question straddled topographic lows in contact with the ocean, making it vulnerable to rapid collapse. The same is true of the West Antarctic Ice Sheet today—the biggest wildcard for future sea level rise. Every ice sheet is different and the local details matter, but an equally rapid collapse of ice in Antarctica would be a worst-case scenario.
Nature Geoscience, 2020. DOI: 10.1038/s41561-020-0567-4 (About DOIs).
https://arstechnica.com/science/2020/04/a-puzzling-past-sea-level-rise-might-have-its-missing-piece/