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To the best of our knowledge, climate change will have effects on all
aspects of life and natural resources in Arctic marine systems, from
molecular to ecosystem level. The consequences will ultimately also have
effects on the global carbon flux. However, despite circumarctic
attempts to investigate the last "white spot" in the ocean,
predominantly focusing upon the rim of the Arctic ice cover, our
knowledge of marine ecosystems in this region is scarce. To meet the
overall goals given in the Rio-Convention and Kyoto Protocol, underlying
the aim of the Norwegian Minister of Environment, it is important to
strengthen and improve marine research in the European sector of the
Arctic.
Marine ecologists in northern Norway have established the network
ARCTOS to give more thrust to marine ecological research, support
international cooperation and integration, and to proliferate the
visibility of Norway's research contribution to research in the Arctic.
ARCTOS attempts to figure out how climate change influences the system
from a molecular to the community level and how this acts on ecosystems,
biodiversity and the biological global flux in the Arctic.
Arctic regions are predicted to incur some of the most pronounced
effects of global climate change. Preliminary forecasts estimate a
reduction of the Arctic ice pack of 20% during winter and 80% during
summer by the end of this century. The dramatic northwards retreat of
the sea ice zone will result in a profound widening of the marginal ice
zone. In the European sector of the Arctic, the retreat results in an
extensive stratified area that stretches from the Spitsbergen and
Barents Sea shelf deeply into the Arctic Ocean. This situation would
change radically from the present state, where a multitude of regions in
the European marginal ice zone each support local ecosystem
characteristics and processes. Weakly stratified water masses,
characteristic of the central Barents Sea today, will spread northwards.
Water temperature will increase, the distribution of Atlantic species
will spread northwards and new production will probably triple. Changes
in weather will further modify the annual patterns and magnitude of
primary production. The low productive, presently ice-covered waters in
the north will turn into a stratified marginal ice zone with nutrient
depletion after a short, intense ice edge bloom. In particular, the
shelf-break of the Arctic Ocean in the European sector that presently
has quasi-permanent ice-cover, will encounter changes. Seasonally open
water in this deep-water region will result in a large spring bloom off
the shelf, with concomitant decoupling of the pelagic and benthic
systems, and export to the deep ocean.
The above-described ongoing climatic change will increase the speed
of industrial development and cause a stronger integration of these
geographical areas into global commercial activities. It is of great
importance that this development is carried out in a sustainable manner,
and based upon scientific knowledge. ARCTOS has therefore a linkage to
applied research and its knowledge and expertise will be valuable and
useful for a wide range of stakeholders in the Arctic region, from
fisheries/aquaculture, oil/gas exploitation, the quality of life for
adjacent circumarctic inhabitants, in particular indigenous people, to
tourism. Issues such as environmental protection, biodiversity and
ecosystem-based pollution assessment are additional aspects where ARCTOS
will contribute to the prosperity of the Arctic community as a whole. |