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Natalie Perlin, Eric Skyllingstad, Roger Samelson, Philip Barbour PowerPoint PPT Presentation
Natalie Perlin, Eric Skyllingstad, Roger Samelson, Philip Barbour - Ekman layer is thinner in the fully coupled case, with higher offshore velocities ... Offshore Ekman transport computed from the atmospheric wind stress differs ...
Ekman layer is thinner in the fully coupled case, with higher offshore velocities ... Offshore Ekman transport computed from the atmospheric wind stress differs ...
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Density currents and slope winds PowerPoint PPT Presentation
Density currents and slope winds - Density currents and slope winds. H. van Dop. Atmospheric boundary layers, Les ... with Schumann (1990) (for anabatic flow) With appropriate approximations ...
Density currents and slope winds. H. van Dop. Atmospheric boundary layers, Les ... with Schumann (1990) (for anabatic flow) With appropriate approximations ...
| PowerPoint PPT presentation | free to view
Natalie Perlin, Eric Skyllingstad, Roger Samelson, Philip Barbour PowerPoint PPT Presentation
Natalie Perlin, Eric Skyllingstad, Roger Samelson, Philip Barbour - College of Oceanic and Atmospheric ... Regional Ocean-Atmosphere Modeling (ROAM) system main components ... Fig.1. ROAM chart, a single-executable modeling ...
College of Oceanic and Atmospheric ... Regional Ocean-Atmosphere Modeling (ROAM) system main components ... Fig.1. ROAM chart, a single-executable modeling ...
| PowerPoint PPT presentation | free to view


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