The formation of sea ice is a crucial a part of the Earth’s local weather system, because it displays daylight again into the ambiance and helps to control the Earth’s temperature.
Polar sea ice formation is influenced by extra than simply the chilly temperatures within the winter months. According to current analysis from the University of Gothenburg and different establishments, salinity is much more vital. Their analysis reveals that the decrease salinity of floor water within the polar areas prevents hotter water from rising to the floor, contributing to the formation of sea ice.
Polar sea ice sometimes varieties within the winter months as a result of chilly temperatures. However, the sinking of colder, denser water ought to carry hotter water again to the floor and stop the formation of sea ice. The researchers have not too long ago printed a research within the journal Science Advances explaining why this does not occur. According to their research, the lower salinity of surface water in the polar regions prevents the warmer water from rising to the surface, leading to the formation of sea ice.
“The salinity of the surface water is lower, thanks to the supply of freshwater from melting ice at the poles and precipitation to the ocean. The difference in salinity between the surface water and the deeper water is an important factor in the formation of sea ice at low temperatures at the poles. Without the difference in salinity, the water would not have become stratified, leading to continuous mixing of sea water, thus preventing the formation of ice,” says Fabien Roquet, professor of physical oceanography at the University of Gothenburg.
The difference in salinity creates a “lid”
The surface of the water, with its lower salinity, creates a “lid” that prevents warm water from rising to the surface. Without that lid, the cold polar temperatures would not be sufficient to freeze continuously moving warmer water.
The strength of this salinity lid is due to the unique properties of the seawater. In freshwater, water that is colder than 4 degrees Celsius has a lower density and therefore remains at the surface and freezes into ice, without mixing with water from greater depths. In the ocean, saltwater has a density that is lowest exactly at the freezing point, around -2C. However, the density of the water varies much less with the temperature in cold water than when it is warmer, which is very unusual for a fluid.
Sea ice inhibits the greenhouse effect
“The closer you get to the poles, the more important salinity is for limiting the mixing and evening out of water temperature throughout the water,” says Fabien Roquet.
This discovery shows how important the special properties of the water molecule are for Earth’s climate. The exchange of heat between the ocean and atmosphere is affected not only by temperature differences but also by the salinity of the ocean. Without this fact, it would be impossible for sea ice to form to any greater extent. Sea ice is itself an important factor in impeding the greenhouse effect because it reflects sunlight away.
“With global warming, we see a decline in sea ice, which impairs the capacity of the polar seas to maintain the ‘lid’ of lower salinity that prevents carbon from rising into the atmosphere. But at the same time, warmer weather can lead to increased freshwater in the polar seas as glaciers melt and precipitation potentially increases. The difference in salinity can then increase, which may contribute to sustaining sea ice formation. But it’s difficult to predict which effect will be dominant; we just have to wait and see,” says Fabien Roquet.
Reference: “Unique thermal expansion properties of water key to the formation of sea ice on Earth” by Fabien Roquet, David Ferreira, Romain Caneill, Daniel Schlesinger and Gurvan Madec, 16 November 2022, Science Advances.
DOI: 10.1126/sciadv.abq0793
