The long-term scientific objective of this research program is to clarify the global role of the sea ice that moves through the Arctic Basin and overflows into the northern Atlantic Ocean by depicting the physical, energetic, and biogeochemical characteristics of the ice, ocean, and surface atmosphere; particularly in the southern Transpolar Drift where the melting process is more significant than new ice formation. This information will improve our understanding of the environmental evolution of the Northern Hemisphere and, by comparison, clarify the global impact of sea ice in the Southern Ocean. The results will aid in assessing planetary environmental problems of today. Scientific observation of sea ice provides us with the first signs of long-range climatic change caused by anthropogenetic forcing, such as the greenhouse effect and the reduction of reverine discharge in the Arctic Basin. In addition, understanding those oceanic processes which produce the highly characteristic biogenic particle flux in the Greenland Sea will improve our knowledge of the global carbon cycle and further the sensible utilization of oceanic food stocks in the northern Atlantic Ocean.
The functional objective of a Polar automated ice-ocean research station is to provide the opportunity to understand the short (hourly and daily), seasonal and inter-annual rates of change in sea-ice and their relationship to local and regional meteorology, upper ocean physics, primary production and, finally, to the process and the rate of biogeochemical cycles in the Polar ocean. In order to be useful to all disciplines of the international scientific community, the gathered data needs to be transmitted in real time.
Consequently, we undertook specific tasks to accomplish the development of such stations and these include the choice, development, and/or implementation of: