Science, 29 September 2022
Rapid loss of Arctic sea ice over the past three decades has accelerated the rate of long-term acidification in the Arctic Ocean, at rates three to four times those occurring in lower latitude oceans. When sea ice melts, it creates a layer of freshwater along the surface of the ocean that readily absorbs carbon dioxide from the air, especially without the protective sea ice cover separating it somewhat from the atmosphere. This surface layer is buoyant; it cannot easily mix into deeper waters. These changes prevent the proper dissolving or “neutralizing” of these high levels of carbon dioxide in surface waters, increasing levels of acidification. Rising global emissions and the retreat of sea ice cover will continue to increase the acidification of Arctic waters over the next few decades, particularly at higher latitudes. Ocean acidification threatens the survival of shell-building species and other species that rely on them throughout the food chain, including human communities built on a stable and productive Arctic marine ecosystem.
ICIMOD, April 24, 2026 2026 marks the fourth consecutive year of below-average snow conditions in…
Ocean Science, 20 Apr 2026 Global warming and increased freshwater input from melting ice are…
Science, 23 Apr 2026 Specially-adapted species living in glacier regions face rapid snowpack and ice…
Science Advances, 24 Apr 2026 Observations from the grounding zone beneath the Ross Ice Shelf…
The Hindu Kush Himalaya faces rising climate extremes that threaten mountain communities, demanding a shift…
Philosophical Transactions of the Royal Society, 23 April 2026 Observations suggest we are currently tracking…