'Layer flow' diaporamas de présentation

Basics of Rotating Boundary-Layer Flow

Basics of Rotating Boundary-Layer Flow. Richard Rotunno NCAR, Boulder CO. http:// www.mmm.ucar.edu/people/rotunno /. NCAR is funded by the National Science Foundation. Outline. Rotating Flow / No Boundary Rotating Flow / Frictional Boundary Layer

483 views • 28 slides

? p and ? surfaces are parallel

Barotropic flow:. ? p and ? surfaces are parallel. For a barotropic flow, we have. is geostrophic current. Since. ?. Given a barotropic and hydrostatic conditions,. and. Therefore,. By definition, ? ? and ? t are both constant in barotropic flow. And. So.

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Relations between isobaric and level surfaces

Relations between isobaric and level surfaces. A level of no motion is usually selected at about 1000 meter depth In the Pacific, the uniformity of properties in the deep water suggests that assuming a level of no motion at 1000m or so is reasonable, with very slow motion below this

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Relations between isobaric and level surfaces

Relations between isobaric and level surfaces. A level of no motion is usually selected at about 1000 meter depth In the Pacific, the uniformity of properties in the deep water suggests that assuming a level of no motion at 1000m or so is reasonable, with very slow motion below this

287 views • 18 slides

? p and ? surfaces are parallel => ?=?(p)

Barotropic flow:. ? p and ? surfaces are parallel => ?=?(p). For a barotropic flow, we have. is geostrophic current. Since. ?. Given a barotropic and hydrostatic conditions,. and. Therefore,. By definition, ? ? and ? t are both constant in barotropic flow. And. So.

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Level of No Motion (LNM)

170 views • 16 slides

? p and ? surfaces are parallel

Barotropic flow:. ? p and ? surfaces are parallel. For a barotropic flow, we have. is geostrophic current. Since. ?. Given a barotropic and hydrostatic conditions,. and. Therefore,. By definition, ? ? and ? t are both constant in barotropic flow. And. So.

154 views • 15 slides

? p and ? surfaces are parallel

Barotropic flow:. ? p and ? surfaces are parallel. For a barotropic flow, we have. is geostrophic current. Since. ?. Given a barotropic and hydrostatic conditions,. and. Therefore,. By definition, ? ? and ? t are both constant in barotropic flow. And. So.

124 views • 12 slides

Giant Quasi-Slip in Flows in 500 nm Carbon Nanotubes

Giant Quasi-Slip in Flows in 500 nm Carbon Nanotubes. S. S. Ray, P. Chando , Prof. A. L. Yarin , Mechanical and Industrial Engineering Prime Grant Support: NSF-NIRT CBET-0609062, NSF-EEC 0755115 . Laminar pressure-driven flows in carbon nanotubes Bi-layer flows of liquid and gas

133 views • 1 slides