Arctic ice melt could disrupt global ocean circulation: Study
What's the story
A recent study warns that the intensifying climate change in polar regions, could severely disrupt global ocean circulation patterns.
The research, led by Mohamed Ezat from the iC3 Polar Research Hub and published in Nature Communications, reveals that increased freshwater inflows from melting Arctic sea ice into the Nordic Seas, have historically affected ocean circulation.
This phenomenon has been linked to significant temperature drops across northern Europe.
Oceanic disruption
Climate change's impact on oceanic heat transport
The Nordic Seas, located between Greenland and Norway, are essential for oceanic heat transport and influence global weather patterns far and wide.
Ezat's study links the warming climate and increased melting of Arctic sea ice during the Last Interglacial period to regional sea-surface temperature and ocean circulation changes.
As Arctic sea ice melts further with rising temperatures, it may disrupt normal current flows by changing water salinity and density.
Methodology
Research methods and implications for future climate models
Ezat's team combined biological, organic, and inorganic geochemical tracers from sediment cores taken from the Nordic Seas for their research.
These cores contained information about past ocean conditions, which helped the team reconstruct past sea surface temperatures and salinity levels.
The study hopes to serve as a benchmark for future climate models, by highlighting how ice changes could impact regional and global climates.
Warning
Climate scientists warn of irreversible impact
Earlier this month, a number of climate scientists had warned in an open letter that the "serious risk of a major ocean circulation change in the Atlantic [that] would have devastating and irreversible impacts."
The statement highlights how severe disruptions to ocean circulation patterns could be due to climate change.
The study's findings are a reminder that our planet's climate is a delicate balance, easily disrupted by temperature and ice cover changes.