Geoscience Reference
In-Depth Information
5.1 Introduction
and thinning of the summer sea ice in the Arctic Ocean are perhaps the most visible in-
dicators of the major physical changes underway in the Arctic Ocean (Kwok
et
al.,
2009
;
Walsh,
2013
). While rates and even causes of ice loss remain under debate (Carmack and
a few decades the Arctic will see a mostly ice-free summer. The biological implications
of this change depend, to a large extent, upon the interplay between altered abiotic condi-
tions (e.g. temperature, salinity, stratification, nutrient availability, wind, underwater light,
climate, etc.) and the response of organisms on all trophic levels changing, for example,
patterns in primary production, respiration, and diversity (e.g. timing, magnitude, and qual-
ity of algal blooms, microbial processes, etc.). Changes in these physical/biological inter-
actions will occur across a variety of spatial and temporal scales and may be mitigated or
strengthened based on widely varying rates of evolutionary adaptation. Studies, monitor-
ing activities, and adaptive experiments that are focused on the often non-linear biophysical
changes that are occurring and the linkages among them will likely offer new insights in-
to the mechanisms, trajectories, and dynamics of ecological and evolutionary change in the
2011
;
Sunday
et al
.,
2011
;
Wassmann
et al
.,
2011
;
Duarte
et al
.,
2012
)
. Here we briefly dis-
cuss some of the basic knowns about the interactions of physical change and the correspond-
ing biological response in the Arctic Ocean, identify significant unknowns, and propose a
new structural framework to guide further Arctic marine research in policy-relevant direc-
tions.
A novel way to view the interaction among various physical and biological changes
and their social relevance is through the systems theory perspective of 'panarchy' proposed
tures, scales, and linkages of complex-adaptive systems, including those of nature (e.g. the