'Boundary' diaporamas de présentation

CHAPTER 20 LAPLACE EQUATION

CHAPTER 20 LAPLACE EQUATION. Team 6: Bhanu Kuncharam Tony Rochav Wei Lu. 20.1 Introduction. Remembering from chapter 16, the Laplacian operator (in Cartesian coordinates ): There are two types of Laplacian equations, Homogeneous

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GEOL 553: Marine Sediments University of South Carolina Fall 2005

GEOL 553: Marine Sediments University of South Carolina Fall 2005. The Tools of Subsurface Analysis. Professor Chris Kendall EWS 304 kendall@sc.edu 777.2410. The Tools of Subsurface Analysis.

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Computing Stable and Compact Representation of Medial Axis

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Nickel-base Superalloy Welding

Nickel-base Superalloy Welding S. A. David & S. S. Babu Metals and Ceramics Division Oak Ridge National Laboratory Oak Ridge, TN 37831-6096 Departmental Seminar Outline Background Experimental Alloys Weld Cracking Monitoring of weld cracks Welding Process Parameters on Weld Cracking

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Clustering

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Andy Humphreys Director of Performance & Service Delivery

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Comparison of an Analytical Expression of the Value of an American Put with standard Methods

Comparison of an Analytical Expression of the Value of an American Put with standard Methods. -Vicky Sharma. Background(1). Partial Differential Equation (PDE) A differential equation of a function of 2 or more equations comprising of partial derivatives of the function .

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Jeopardy

Jeopardy. Earthquakes. Boundaries. Faults/ Stresses. Plate Tectonics and Vocabulary. Continental Drift. $100. $100. $100. $100. $100. $200. $200. $200. $200. $200. $300. $300. $300. $300. $300. $400. $400. $400. $400. $400. $500. $500. $500. $500. $500.

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GIS and SMS in Numerical Modeling of Open Channel Flow

GIS and SMS in Numerical Modeling of Open Channel Flow. Ryan Murdock November 28, 2000. SMS = Surface Water Modeling Modeling System. Graphical pre and post processor for numerical surface water models. Data Collection. Detailed Stream Elevation Data. DEMs not suitable

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Plate Tectonics

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Numerical modeling example

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Some Basic Relationships Between Pixels

Some Basic Relationships Between Pixels. Definitions: f(x,y): digital image Pixels: q, p Subset of pixels of f(x,y): S. Neighbors of a Pixel. A pixel p at (x,y) has 2 horizontal and 2 vertical neighbors: (x+1,y), (x-1,y), (x,y+1), (x,y-1)

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Thunderstorms and Tornadoes

Thunderstorms and Tornadoes. Last Lecture: We looked at severe weather events in the lower latitudes Principal weather event is the formation and movement of Tropical Cyclones Today: Today we will look at severe weather in the mid-latitudes Most severe weather is related to thunderstorms

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Overview Class #6 (Tues, Feb 4)

Overview Class #6 (Tues, Feb 4). Begin deformable models!! Background on elasticity Elastostatics: generalized 3D springs Boundary integral formulation of linear elasticity (from A RT D EFO (SIGGRAPH 99)). Equations of Elasticity. Full equations of nonlinear elastodynamics

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Facilitating Support of Transformative & Interdisciplinary Research at NSF

Facilitating Support of Transformative & Interdisciplinary Research at NSF. SBE Advisory Committee Cliff Gabriel November 2008. BIO Jim Collins Judith Verbeke BFA Jean Feldman Vernon Ross CISE Suzi Iacono Sankar Basu EHR Joan Ferrini-Mundy Linda Slakey Reid Schwebach ENG

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Plate boundaries

Plate boundaries. 8-3.6 Chapter 6, lesson 3 Page 198-205. Divergent boundary. Where 2 plates are moving apart Most are located along mid-ocean ridge (sea floor spreading) New crust forms b/c magma pushes up & hardens between separating plates. Convergent boundary.

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THE GRACCHI

THE GRACCHI. TIBERIUS GRACCHUS (163-133 BC) and GAIUS GRACCHUS (153-121 BC). Conditions in the Late Republic. Military problems: Fewer men eligible for army, military levy based on land ownership. Decline in birth rate impacted army numbers. Lower quality of troops = undisciplined.

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