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Version 2 ROMS Model for Computation of GEMBOX Exchanges
• Version 2 model changes: Open boundary forcing of large-domain model
taken from regional model (C. Chen’s FVCOM). Spatially variable wind forcing from high-resolution
atmospheric model (also from Chen). Two additional rivers (plus WWTF) entering western
end of Greenwich Bay.• Version 2 model skill improved in comparison to
Version 1.• Have generated version 2 model dye exchanges for
2006. 2007 run in progress.• Computing flushing times for GEMBOX elements.
Large-Domain Model Forcing Changes:•Low-pass filtered sea level, velocity, temperature, and salinity from FVCOM simulation applied along open boundaries of large-domain model (in addition to tides as in standard run).•Spatially variable wind.
Fullbay Model Forcing Changes:•Addition of river inflows in W. Greenwich Bay.•Spatially variable wind.•Bay mouth open boundary forcing from new version of large domain model.
Open boundaries
Blue: “large-domain” modelRed: “fullbay” model
New Rivers
Subtidal Sea Level, Velocity
Blue: observationsBlack: model v1Red: model v2
Sea Level: Providence
Sea Level: Newport
Sea Level Difference
Velocity: E. PassageChannel
Model/Obs. Comparison, Greenwich BayVersion 2Version 1
Model Skill, Salinity at DEM StationsSurface Bottom
Version 1a: large-domain model forced with FVCOM results. spatially variable wind forcing.
Utility of Dye Exchange Estimates (In Addition to Use for GEMBOX)
Hypothesis: Dye exchange fractions can reveal details of physical exchange of materials throughout N. Bay.
• Long time series of exchange fractions provides information on exchange under a wide range of forcing conditions.
• Can compute flushing times on a daily basis for individual box model elements (or groups of elements) using exchange fractions.
• Aim is to develop a statistical description of flushing and exchange processes.
Element Flushing Times: Salt or Freshwater•Dye fluxes represent gross (one-way) advective plusdiffusive transport.•Net salt flux between elements i and j expressed using dye fractions (similar for Freshwater (FW)):
Estimate flushing time from salt (FW) mass within an element and salt (FW) flux into or out of that element:
for j where flux_salti,j < 0or
for j where flux_salti,j > 0
V2 Model: Time Evolution of Flushing Time
Version 2 Model: Median Flushing TimesUpper Layer Elements Lower Layer Elements
What Causes Variability of Flushing Time?
Seems to be complex interplay of factors.e.g. river discharge and northward wind:
northward northwardsouthward southward
Box 2, surface Box 2, bottom
Next Steps• Finish dye exchange run for 2007 using version 2 model
(within next couple of weeks).
• Simulation of additional years: 2008, and possibly 2009?
Relatively straightforward to obtain forcing data. Simulations will thus be comparable to 2006-2007.
2014?Open boundary and wind forcing data may not be available from the same source. Can explore other options. Upshot may be that simulations will not be easily compared with 2006-2007 because of different model forcing.
• Papers: 1. ROMS model description/skill assessment.2. Flushing time and its variability.