Saturday, July 2, 2022
Permafrost Heating is Moving to Arctic Seafloor by Slow Moving Groundwater with Ramifications for Clathrate Mobilization. 2-22-07-02. Joorma Jyrkkanen
Arctic Study. Rapid changes to the Arctic seafloor noted as submerged permafrost thaws
Using MBARI mapping technology, researchers have established a baseline for tracking future changes to the seafloor
Date:
March 14, 2022
Source:
Monterey Bay Aquarium Research Institute
Summary:
A new study has documented how the thawing of permafrost submerged underwater at the edge of the Arctic Ocean is affecting the seafloor.
A new study from MBARI researchers and their collaborators is the first to document how the thawing of permafrost, submerged underwater at the edge of the Arctic Ocean, is affecting the seafloor. The study was published in the Proceedings of the National Academy of Sciences on March 14, 2022.
Numerous peer-reviewed studies show that thawing permafrost creates unstable land which negatively impacts important Arctic infrastructure, such as roads, train tracks, buildings, and airports. This infrastructure is expensive to repair, and the impacts and costs are expected to continue increasing.
Using advanced underwater mapping technology, MBARI researchers and their collaborators revealed that dramatic changes are happening to the seafloor as a result of thawing permafrost. In some areas, deep sinkholes have formed, some larger than a city block of six-story buildings. In other areas, ice-filled hills called pingos have risen from the seafloor.
"We know that big changes are happening across the Arctic landscape, but this is the first time we've been able to deploy technology to see that changes are happening offshore too," said Charlie Paull, a geologist at MBARI and one of the lead authors of the study. "This groundbreaking research has revealed how the thawing of submarine permafrost can be detected, and then monitored once baselines are established."
While the degradation of terrestrial Arctic permafrost is attributed in part to increases in mean annual temperature from human-driven climate change, the changes the research team has documented on the seafloor associated with submarine permafrost derive from much older, slower climatic shifts related to our emergence from the last ice age. Similar changes appear to have been happening along the seaward edge of the former permafrost for thousands of years.
"There isn't a lot of long-term data for the seafloor temperature in this region, but the data we do have aren't showing a warming trend. The changes to seafloor terrain are instead being driven by heat carried in slowly moving groundwater systems," explained Paull.
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