'Surface marine data nodc' diaporamas de présentation

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Wind Driven Circulation I: Ekman Layer

Wind Driven Circulation I: Ekman Layer

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357 views • 26 slides
Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface. Monin-Obukhoff Similarity Theory. Surface layer (several tens of meters above surface, 10-15% of the planetary boundary layer) in nearly steady condition Vertical turbulent flux is nearly constant

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237 views • 23 slides
Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface. Monin-Obukhoff Similarity Theory. Surface layer (several tens of meters above surface, 10-15% of the planetary boundary layer) in nearly steady condition Vertical turbulent flux is nearly constant

★ ★ ★ ★ ★

559 views • 21 slides
Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface. Monin-Obukhoff Similarity Theory. Surface layer (several tens of meters above surface, 10-15% of the planetary boundary layer) in nearly steady condition Vertical turbulent flux is nearly constant

★ ★ ★ ★ ★

229 views • 21 slides
Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface

Wind Driven Circulation I: Planetary boundary Layer near the sea surface. Monin-Obukhoff Similarity Theory. Surface layer (several tens of meters above surface, 10-15% of the planetary boundary layer) in nearly steady condition Vertical turbulent flux is nearly constant

★ ★ ★ ★ ★

218 views • 21 slides

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