Ice flows fill the Merrimack River as it heads towards the Atlantic Ocean in Newburyport, Massachusetts during the extreme cold temperatures caused by the Polar Vortex, bringing temperatures below freezing, on January 31, 2019.

A recent study has found that the cooler temperatures of the ocean's surface layer help absorb more carbon dioxide (COâ‚‚), significantly contributing to climate change mitigation. 

Researchers from the University of Exeter conducted this study in the Atlantic Ocean, revealing that it absorbs approximately 7% more COâ‚‚ each year than previously thought. While this may seem like a small increase, it amounts to one and a half times the amount of carbon absorbed by all the trees in the Amazon rainforest each year.

'Ocean Skin' Temperature Differences Linked to COâ‚‚ Absorption 

The researchers focused on the "ocean skin," which is a thin layer less than 2 millimeters deep at the surface of the ocean. This layer is slightly cooler than the water beneath it. 

Past theories suggested that this temperature difference could lead to increased COâ‚‚ absorption, but this study is the first to successfully observe this phenomenon in the ocean.

According to Science Daily, the study useed advanced measurement techniques to analyze the temperature and COâ‚‚ levels at the ocean surface. These observations were made during two projects backed by the European Space Agency. 

The researchers measured tiny differences in COâ‚‚ levels in the air near the ocean surface to understand how much carbon the ocean is absorbing. Their findings suggest that temperature differences at the ocean's surface play a crucial role in determining how much COâ‚‚ is absorbed from the atmosphere.

The ocean is essential for managing carbon emissions, absorbing about a quarter of humanity's total emissions. This new knowledge enhances our understanding of how oceans interact with the atmosphere and helps improve global carbon assessments used for emission reduction strategies. 

According to the study's lead author, the results reinforce previous theoretical predictions regarding COâ‚‚ fluxes at the ocean surface.

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