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m →Framework: changed "layers" to "levels" in explanation of the vertical grid. Fixed minor grammar and spelling problems. Added sentences explaining the vertical levels for water and sediments. |
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=== Input ===
Boundaries such as coastlines can be specified for a given region using land- and sea-masking. The top vertical boundary, the air-sea interface, uses an interaction scheme developed by Fairall et al. (1996).<ref>{{Cite journal|last=Fairall|first=C. W.|last2=Bradley|first2=E. F.|last3=Rogers|first3=D. P.|last4=Edson|first4=J. B.|last5=Young|first5=G. S.|date=1996-02-15|title=Bulk parameterization of air-sea fluxes for Tropical Ocean-Global Atmosphere Coupled-Ocean Atmosphere Response Experiment|journal=Journal of Geophysical Research: Oceans|language=en|volume=101|issue=C2|pages=3747–3764|citeseerx=10.1.1.469.6689|doi=10.1029/95jc03205|issn=0148-0227}}</ref> The bottom vertical boundary, the [[Sediment–water interface|sediment-water interface]], uses a bottom stress or bottom-boundary-layer scheme developed by Styles and Glenn (2000).<ref>{{Cite journal|last=Styles|first=Richard|last2=Glenn|first2=Scott M.|date=2000-10-15|title=Modeling stratified wave and current bottom boundary layers on the continental shelf|journal=Journal of Geophysical Research: Oceans|language=en|volume=105|issue=C10|pages=24119–24139|doi=10.1029/2000jc900115|issn=0148-0227|url=http://pdfs.semanticscholar.org/8350/d67073a1547a0a67dfb7d3693371d3865dea.pdf|archive-url=https://web.archive.org/web/20191230024109/http://pdfs.semanticscholar.org/8350/d67073a1547a0a67dfb7d3693371d3865dea.pdf|url-status=dead|archive-date=2019-12-30}}</ref>
Inputs that are needed for an implementer to run ROMS for a specific ocean region include:
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