Do changes in the formation and distribution of sea ice affect our global climate? Yes. The role of sea ice is greater than you might think.
The sun’s rays strike the polar regions at a more grazing angle than over equatorial regions, where the rays strike at a more direct angle. The sun’s angle is the primary reason why the polar regions are cold and the equatorial regions are warm.
Sea ice is white, so nearly all of the sunlight that hits the sea ice surface is reflected back into space; thus, it has a high albedo.* High albedo helps keep the polar regions cold, because the sunlight reflected back into space does not warm the surface. When the climate changes enough to warm the Arctic and to melt sea ice, the polar regions have less of a reflective surface. More heat is absorbed, which causes more melting, which amplifies the warming. This cycle is known as a positive feedback loop that ultimately alters the circulation of the atmosphere.
Atmosphere and Ocean Circulation
The atmosphere and ocean act as “heat engines,” always trying to restore a temperature balance by transporting heat toward the poles. Our weather is a manifestation of this phenomenon. Low-pressure systems, such as storms, which can be especially strong in winter, are one of nature’s best ways of transporting heat poleward by atmospheric circulation.* The oceans, by contrast, tend to transport heat in a slower and less violent fashion. Changes in the amount of sea ice alter how cold the poles are, which could affect atmospheric and ocean circulation.
Ocean currents transport heat from the equator to the poles through a heat- and saline-driven process called thermohaline circulation. Warm water moves from the equator northward along the ocean surface and eventually cools. As it cools, it becomes dense and heavy and sinks. This cold water then moves south along the lower part of the ocean and rises near the equator to complete the cycle. Like the atmospheric heat transport discussed earlier, this is a natural process that contributes to a proper temperature balance across the earth. It also explains why Europe is relatively warm, because as northward flowing surface water in the Atlantic Ocean cools, heat is released to the atmosphere.
Thermohaline circulation can be disrupted if the ocean surface receives a layer of fresh water. How might this happen? One mechanism involves changes in Arctic winds that move sea ice from the Arctic Ocean through Fram Strait into the North Atlantic.
Although the ocean is salty, the sea ice on top of the Arctic ocean is fresh–-fresh enough to drink. Sea ice is fresh because sea ice expels salt into the water as it forms. When the ice moves south through the Fram Strait into the North Atlantic, it melts, creating a layer of fresh water over the ocean surface. This fresh water is less dense than salty water, so it tends to stay at the top of the ocean. This lower density discourages the normal process of sinking at high latitudes (poles) that supports thermohaline circulation, which makes it harder to move the warm water north from the equator. Strong evidence shows that this stagnation process happened over a period of several years in the late 1960s and early 1970s, when extra fresh water entered the North Atlantic and affected the climate of northern Europe. Scientists call this event the “Great Salinity Anomaly.”
While this process involves the transport of ice out of the Arctic, other processes are at work within the Arctic Ocean itself.
During winter, the Arctic’s atmosphere is very cold. In comparison, the ocean is much warmer. The sea ice cover separates the two, preventing heat in the ocean from warming the overlying atmosphere. This insulating effect is another way that sea ice helps to keep the Arctic cold. But heat can escape rather efficiently from areas of thin ice and especially from leads* and polynyas*, small openings in the ice cover. Roughly half of the total exchange of heat between the Arctic Ocean and the atmosphere occurs through openings in the ice. With more leads and polynyas, or thinner ice, the sea ice cannot efficiently insulate the ocean from the atmosphere. The Arctic atmosphere then warms, which, in turn influences the global circulation of the atmosphere.
a non-dimensional, unitless quantity that measures how well a surface reflects solar energy; ranges from 0 – 1; a value of 0 means the surface is a “perfect absorber,” where all incoming energy is absorbed, a value of 1 means the surface is a “perfect reflector,” where all incoming energy is reflected and none is absorbed.
the large-scale movement of air, and the means by which heat is distributed on the surface of the Earth; may vary from year to year.
long, linear areas of open water that range from a few meters to over a kilometer in width, and tens of kilometers long; they develop as ice diverges, or pulls apart.
irregularly shaped areas of persistent open water that are sustained by winds or ocean heat; they often occur near coasts, fast ice, or ice shelves.
a large area of freely navigable water in which floes may be present in concentration under 1/10th; if there is no sea ice present, the area may be termed open water, even though icebergs are present.
ice that is anchored to the shore or ocean bottom, typically over shallow ocean shelves at continental margins; fast ice is defined by the fact that it does not move with the winds or currents.