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133 – Polar Climate System
Principal Investigator(s): L. Boisvert
A polynya is a persistent opening or hole in sea ice that occurs in locations or times when sea ice is otherwise thought to be present. They come in many different shapes and can range in size from hundreds to thousands of square kilometers. Even though their relatively small size in comparison so the sea ice itself, polynyas have a large impact on the Arctic in a number of ways. Polynyas affect the surrounding atmosphere, the radiation budget, the local ocean salinity, the ocean circulation, and wildlife. In the winter months their effects are most prominent. They provide the surrounding air with excess heat and moisture, which cools the ocean and heats up the surrounding boundary layer. This excess moisture leaves the ocean surface, quickly cools and condenses, and creates plume clouds, which can be transported downstream via winds. Polynyas are relatively under sampled due to their remote locations and harsh wintertime conditions. Observations are done on field campaigns, on ships and by weather stations, but data is collected for short time periods and instrument error can occur due to harsh conditions.
In the past decade there has been an abundance of satellite data that has spatial and temporal scales that provide much more coverage of the Arctic and polynyas than field campaigns. Being able to use this valuable data to study polynyas in detail would greatly enhance our understanding of polynyas and their effects on the Arctic system.