Thomas Haine (PI)
Johns Hopkins University
thomas.haine@jhu.edu
Space-Based Estimates of Arctic/Sub-Arctic Exchange Using Data Assimilation
and Ocean Models
Recent studies show that interannual fluctuations in North Atlantic
climate have significant influence on transfer of freshwater
and heat into the Arctic Ocean. In turn, the strength of the dense
overflows returning south across the Greenland-Scotland Ridge
are modulated by this variability, lagged with a delay of
a few years. Other studies raise the possibility of substantial
weakening and/or freshening of the overflows, and hence the
meridional-overturning circulation, in response to anthropogenic-induced
climate change. A
particularly urgent case therefore exists to study air/sea/ice
interactions in the subpolar Atlantic and Greenland/Iceland/Norwegian
Seas.
To
address this issue we propose a project to develop, test,
and apply a prototype model/data assimilation system that
can synthesize remote-sensed and in-situ observations to
estimate climate-critical fluxes across Denmark Strait. We
seek to answer the question: What is the benefit of assimilation
to estimate this exchange, what is the current state, and
where are the greatest uncertainties?
The
approach will be to develop a hierarchy of regional models
of the Denmark Strait and Irminger Sea with horizontal resolution
between 1/12 and 1/60 deg. In tandem, we will develop a variational
data assimilation capability that synthesizes remotely-sensed
observations of sea-surface height, sea-surface temperature,
sea-surface salinity, wind stress, and sea ice with the circulation
models. Using twin experiments to test the system, we will
determine the prospects for estimating mass, heat, freshwater
exchange across the Denmark Strait and water-mass conversion
in the Irminger Sea overflow. We will then apply the model/data
assimilation system using satellite and in-situ data during
select summer periods of 2003 and 2004 to formally estimate
the oceanic state in the Denmark Strait at those times. The
result will be an optimal blend of remote-sensed data, in-situ
data, and dynamical constraints that will be of great value
to researchers studying processes and climate variability
near Denmark Strait. Other project outcomes include: a quantitative
assessment of the relative merits of each part of the observing
network in this area, guidance for climate modelers on systematic
errors in their climate forecast models, and improved practical
knowledge of accurate ocean data assimilation in very high
resolution regional models.
The
project will be a collaborative effort between 2 groups at
Johns Hopkins University: The Department of Earth and Planetary
Sciences and the Ocean Remote Sensing Group of the Applied
Physics Laboratory.
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