Pacific Ocean Boundary Ecosystems:
Response to Natural and Anthropogenic Climate Forcing
Funded by: |
National Science Foundation (NSF) |
Principal Investigator: |
Andrew Thomas |
Co-Principal Investigators: |
E. DiLorenzo, A. Bracco, P.J. Franks, P.T. Strub,
W.T. Peterson, S. Bograd, R. Mendelssohn, F.
Schwing, J. Keister
These PIs are supported by
collaborative teams from Chile, Japan and
Canada. |
Large-scale decadal Pacific
climate indices such as the Pacific Decadal Oscillation
(PDO) have been linked to changes across multiple
trophic levels of marine ecosystems along the eastern
and western boundaries. Recent studies of the Northeast
Pacific by the PIs show that other independent climate
modes are equally important in explaining changes in
coastal ocean upwelling and transport dynamics – the
fundamental processes controlling regional nutrient
fluxes and planktonic ecosystem dynamics. This suggests
that the interplay of forcing functions associated with
multiple large-scale climate modes must be considered to
adequately diagnose the dynamics and mechanics
underlying variations in regional ecosystems. With this
framework, our study combines extensive national and
international in situ and satellite observations with
numerical and statistical physical-biological models to
diagnose the response of four Pacific boundary
ecosystems to large-scale natural and anthropogenic
climate forcing. The focus regions are: the Gulf of
Alaska (GOA), the California Current System (CCS), the
Peru-Chile Current System (PCCS), and the
Kuroshio-Oyashio Extension (KOE) region. We approach
this goal through four core research objectives.
(1)
Assess to what extent, and by what mechanisms,
large-scale climate modes (e.g. PDO, NPGO, ENSO, and
others) drove coherent changes across Pacific boundary
ecosystems over the period 1960-2007.
(2)
Quantify and explain how changes in regional ocean
processes (e.g. upwelling, transport dynamics, mixing
and mesoscale structure) at each boundary control
phytoplankton and zooplankton dynamics. Then, use those
results to test the degree to which changes in each
study region reflect bottom-up control of their
respective ecosystems.
(3)
Quantify the extent to which changes in the statistics
of shorter-period events (e.g. intraseasonal
oscillation, timing of spring transitions) during
different phases of the longer-period climate modes
(e.g. PDO, NPGO and others) determine the climate state
of boundary-current ecosystems.
(4) Explore the range of uncertainties in the
response of regional ocean dynamics and their ecosystems
to climate change using forcing scenarios from selected
climate model integrations that are part of the IPCC
2007 report. This last objective begins an assessment of
the potential impacts of climate change on regional
ocean ecosystems, a topic poorly addressed in the latest
IPCC report, but the chief instrument for most fisheries
and coastal management.
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