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Ocean Layer Shifts in Southern Hemisphere Raise Climate Questions

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Science Desk

In Short: Scientists propose a shift in Southern Hemisphere Westerly Winds as a cause for warming in ocean layers.

Eddies in the Southern Ocean, NASA
NASA (GSFC_20171208_Archive_e000750) — public domain

An international team of scientists has proposed that a shift in the Southern Hemisphere Westerly Winds could be responsible for warming in intermediate water masses in the Southern Ocean, according to a study published in Nature.

The study, which focuses on the last deglaciation period from 18 to 11 thousand years before present, highlights the warming of intermediate waters in the southwestern Pacific Ocean that occurred simultaneously with some upper ocean waters in the Atlantic during Heinrich Stadial 1.

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The researchers suggest that this warming signal could be explained by the increased temperature of intermediate water masses produced in the Southern Ocean due to the shift in the Southern Hemisphere Westerly Winds.

This finding is significant as it indicates that the Southern Hemisphere climate system may play a role in regulating interhemispheric oceanic heat transport at millennial timescales.

The study also raises questions about the mechanisms behind the major climatic transition during the last deglaciation, a period marked by melting ice sheets, rising oceanic and atmospheric temperatures, and increasing atmospheric carbon dioxide concentrations.

The warming of the Antarctic Intermediate Water (AAIW), which is typically a cool and relatively fresh layer between 800 and 1500 meters, suggests a need for a mechanism capable of producing rapid warming in nearly antipodal ocean basins.

The research team's observations require a mechanism that can explain the simultaneous warming in the southwestern Pacific and the Atlantic during Heinrich Stadial 1.

While the exact cause of this warming remains an outstanding problem in paleoclimatology, the study provides new insights into the complex interactions between ocean currents and atmospheric winds in shaping global climate patterns.

What this adds

The study does not provide direct evidence for the shift in the Southern Hemisphere Westerly Winds but suggests it as a plausible explanation for the observed warming in ocean layers.

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