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Joint Metoc Handboo - IHMC Ontology and Policy Management

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7-Navy<br />

> Model tends to develop systems faster <strong>and</strong> retain energy longer, however,<br />

explosive deepening systems continue to be lagged<br />

> Increased skill in detecting tropical low formation verified<br />

- Coupled Ocean / Atmosphere Mesoscale Prediction System (COAMPS)<br />

> Incorporates non-hydrostatic physics, explicit moisture <strong>and</strong> improved data<br />

assimilation<br />

> Globally relocatable<br />

> Supports nested grids at resolutions of less than 10 km<br />

> Can be run st<strong>and</strong>-alone basis or fully coupled<br />

> Provides for a fully interactive two-way coupling between the ocean <strong>and</strong><br />

atmosphere<br />

> Typically run at FNMOC, with capabilities being fielded at the regional centers<br />

- Third-Generation Wave Model (WAM)<br />

> Replaces Global Spectral Ocean Wave Model<br />

> Based on wind stresses from either NOGAPS or NORAPS<br />

> Produces wave forecasts out to 72 hours<br />

> Run on a global 1.0 degree spherical grid with 15 degree angular resolution for<br />

directional spectra, using a 20 minute propagation <strong>and</strong> source term time step<br />

> Wave heights exhibit smaller mean errors, RMS errors, <strong>and</strong> scatter index<br />

indices than those predicted by the GSOWM<br />

- Thermodynamic Ocean Prediction System (TOPS 4.0)<br />

> Predicts response of upper thermal structure of ocean to local atmospheric<br />

forcing <strong>and</strong> provides surface currents for Search <strong>and</strong> Rescue applications<br />

> Synoptic mixed-layer model consisting of conservation equations for<br />

temperature, salinity, <strong>and</strong> momentum in the upper ocean<br />

> Forced by heat flux <strong>and</strong> wind stress predicted by NOGAPS<br />

> Includes horizontal advection of temperature <strong>and</strong> salinity due to wind drift <strong>and</strong><br />

geostrophic components of the current<br />

- Optimal Thermal Interpolation System (OTIS 4.0)<br />

> Produces SSTs on a global basis <strong>and</strong> a surface to bottom analysis of<br />

temperature <strong>and</strong> salinity in two western boundary current regions<br />

> Optimum interpolation data assimilation scheme which incorporates real-time<br />

observational data <strong>and</strong> makes use of bogus front <strong>and</strong> eddy features provided by<br />

NAVOCEANO<br />

> Noted improvements in representation of warm <strong>and</strong> cold eddies <strong>and</strong> front <strong>and</strong><br />

eddy interaction events<br />

> Grid mesh of 0.2 deg. latitude by 0.2 deg. longitude<br />

> In Atlantic, western boundary region includes entire coastal <strong>and</strong> littoral<br />

environments with bogus routine providing the Florida Loop Current, Gulf<br />

Stream, North Atlantic Current, <strong>and</strong> the Shelf-Slope frontal system<br />

7-13

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