Warmer winters are starting to alter the structure of the Black Sea, which could foreshadow how ocean compositions might shift from future climate change, according to new research.
A new study published in AGU’s Journal of Geophysical Research: Oceans analyzing water temperatures, density and salinity in the Black Sea from 2005 to 2019 finds warming winter weather is warming the middle water layer of the Black Sea, known as the cold intermediate layer, which exists between the oxygen-free bottom layer of the sea and the oxygenated top layer of water. This warming is causing the cold intermediate layer to mix with the other two layers of water, according to the new research.
This intermediate layer has fluctuated in the past, but in the last 14 years its core temperature has warmed 0.7 degrees Celsius (1.26 degrees Fahrenheit). The blending of the cold intermediate layer with the other layers of water could enable the water masses from the deeper layers of the sea to eventually infiltrate the top layer, which would have unknown impacts on the sea’s marine life.
The new study suggests climate change is causing the intermediate layer to warm and change, but natural fluctuations could also be playing a role, according to the study’s authors.
Read more at American Geophysical Union
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