Mesoscale Ocean Forecast/Assimilation Studies

The long-term goal over this three-year project has been to develop computer software needed to optimize initial conditions, internal parameters and external parameters for the Harvard primitive equation (PE) model in order to produce the best forecasts in an arbitrary region. This new tool invokes...

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Bibliographic Details
Main Authors: Miller, Arthur J., Cornuelle, Bruce D.
Other Authors: CALIFORNIA UNIV REGENTS LA JOLLA CA SCRIPPS INST OF OCEANOGRAPHY
Format: Text
Language:English
Published: 1998
Subjects:
Physical and Dynamic Oceanography
*FRONTS(OCEANOGRAPHY)
*FORECASTING
SOFTWARE TOOLS
ICELAND
FAROE ISLANDS
INTERPOLATION
PARAMETERS
OCEAN MODELS
CURRENT MEANDERING
HAMMERHEAD BAROCLINIC INSTABILITY
HYDROGRAPHIC DATA
ICELAND-FAEROE FRONT
MODEL FITTING
NONLINEARITY
OCEAN FORECAST MODELS
OCEAN FORECASTING
PARAMETERIZATION
PRIMITIVE EQUATION MODEL
UNSTABLE REGIONS
Faroe Islands
Iceland
Online Access:http://www.dtic.mil/docs/citations/ADA542113
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA542113
Description
Summary:The long-term goal over this three-year project has been to develop computer software needed to optimize initial conditions, internal parameters and external parameters for the Harvard primitive equation (PE) model in order to produce the best forecasts in an arbitrary region. This new tool invokes an inverse technique to fuse all available data types, gathered non-synoptically, with optimized model dynamics. The technique is distinct from (and complementary to) the optimal interpolation and Kalman filter assimilation strategies now being developed and used at Harvard (e.g., Lermusiaux, 1997). The scientific objectives of this research include answering the following questions. Can forecast skill in a highly unstable region like the Iceland-Faeroe Front be extended to 7 days? Can a diagnostic simulation over a 10-day interval in that region include all the data in an inverse calculation, or is it too nonlinear? What are the relative impacts of the various data types (CTD/XBT/XCTD casts, current meters, surface drifters) on making forecasts in this region? The technical objectives encompass the details of the model fitting process. How nonlinear is the fit? Can the nonlinearity be reduced by optimizing large-scale structure first? How much data can be fit at one time? Is the distribution of the data sufficient to initialize the model? Are the open boundaries causing instabilities in the model? See also ADM002252.

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