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Since 1988 the regular summer hydrographic observations in the Nordic Seas and Fram Strait have been collected by the Institute of Oceanology Polish Academy of Sciences (IOPAS). Observational activities were carried out under several national programs, in the frames of EU projects VEINS, ASOF-N and DAMOCLES and within Polish-Norwegian cooperation in the AWAKE project. The main objectives are: to study the long-term variability of water mass distribution, their physical and chemical properties and different pathways in the Nordic Seas; to investigate the Atlantic water (AW) circulation in the Nordic Seas and its inflow into the Arctic Ocean; to recognize the possible feedbacks between the Atlantic water variability and local and global climate changes.
Since 2000 the regular summer hydSince 2000 the regular summer hydrographic observations in the Western Spitsbergen Fjords have been collected by the Institute of Oceanology Polish Academy of Sciences (IOPAS). Observational activities were carried out under several national programs, and in the frames Polish-Norwegian research Fund projects ALKEKONGE and AWAKE. The main objectives are: to study the variability of water mass physical and chemical properties in the Western Spitsbergen Fiords; to investigate the Atlantic water (AW) inflow into the fjords; to recognize the possible feedbacks between the Atlantic water variability, local climate and glaciers discharge.rographic observations in the Western Spitsbergen Fjords have been collected by the Institute of Oceanology Polish Academy of Sciences (IOPAS). Observational activities were carried out under several national programs, and in the frames Polish-Norwegian research Fund projects ALKEKONGE and AWAKE.
Arctic coast is extremely sensitive and important area of interaction between land and sea. The diagnosis of the mechanisms governing the polar zone is of fundamental importance for tracing the evolution of the coast caused by climate change. Diagnosis of morphogenesis and morphodynamics of the polar coast becomes important in recent years, a research priority, not only from the scientific point of view, but also practical. Therefore, the key aims of the project include: - determining the dynamics of morphogenetic processes with particular emphasis on marine processes within the coastal zone in the context of climate change after the Little Ice Age (LIA) and the development of model of the coast functioning during this period. - to try to reference this model to the development of the coast at the turn of Vistulian and Holocene (14-8 ka) by defining the stages of shaping the shoreline including glaciizostatic and eustatic and elements of tectonical and lithological features of the coastal zone.