'Momentum equations' presentation slideshows

CE 374K Hydrology

CE 374K Hydrology. Review for Second Exam April 14, 2011. Hortonian Flow. Sheet flow described by Horton in 1930s When i < f , all i is absorbed When i > f , ( i-f ) results in rainfall excess Applicable in impervious surfaces (urban areas) Steep slopes with thin soil

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AOSS 401 Geophysical Fluid Dynamics: Atmospheric Dynamics Prepared: 20130924 Scale Analysis

AOSS 401 Geophysical Fluid Dynamics: Atmospheric Dynamics Prepared: 20130924 Scale Analysis. Richard B. Rood (Room 2525, SRB) rbrood@umich.edu 734-647-3530 Cell: 301-526-8572. Class News. Ctools site ( AOSS 401 001 F13 ) Disruption of schedule Lectures for missed classes posted.

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Center of Mass and Momentum

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Multigrid Methods The Implementation

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Recoil and Collisions 8.01 W07D1

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Recoil and Collisions 8.01 W07D1 Associated Reading Assignment: Young and Freedman: 8.3-8.4

Recoil and Collisions 8.01 W07D1 Associated Reading Assignment: Young and Freedman: 8.3-8.4. Math Review Night this Week Tuesday 9-11 pm in 26-152 Test Two Next Week Thursday Oct 27 7:30-9:30 Rooms TBA Pset 6 Due Tuesday at 9 pm Next Reading Assignment W07D2: Young and Freedman: 8.3-8.4.

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What Is a Numerical Weather Prediction Model?

What Is a Numerical Weather Prediction Model?. Seek relationships (equations) between variables you want to know (e.g. - v, T, p, z, q) and the forcing mechanisms that cause changes in these variables. Example:. Presented by Fred Carr COMAP Symposium 99-1. In meteorology, we solve for Du/Dt

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Sea-Ice in ROMS

Sea-Ice in ROMS. Kate Hedstrom, UAF Paul Budgell, Bergen Enrique Curchitser, LDEO. Outline. Equations Dynamics Thermodynamics Code cppdefs.h SeaIce directory ice.in Papers and plans. Dynamics. Momentum equations: Viscous-plastic term:. More Dynamics. Ice strength: Rearrange VP:

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CE 3372 Water Systems Design

CE 3372 Water Systems Design. SWMM Dynamic Wave. Dynamic Wave. Used when: Need to investigate backwater effects; gradually varied flow Need to investigate looped systems Need to approximate overland flow and inundation Need to investigate time-varying flow. St. Venant Equations.

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Lecture Objectives

Lecture Objectives. Review Define Residual and Relaxation SIMPLE CFD Algorithm SIMPLE Semi-Implicit Method for Pressure-Linked Equations. Review. Conservation equations Turbulent flow and turbulence modeling RANS Equation Discretization System of equation and solution methods

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Lecture Objectives

Lecture Objectives. Review SIMPLE CFD Algorithm SIMPLE Semi-Implicit Method for Pressure-Linked Equations Define Residual and Relaxation. Review. Conservation equations Turbulent flow and turbulence modeling RANS Equation Discretization System of equation and solution methods

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Objective

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