'Dx dy' diaporamas de présentation

UNIT I: Theory of the Consumer

UNIT I: Theory of the Consumer. Introduction: What is Microeconomics? Theory of the Consumer Individual & Market Demand. 6/ 25. Theory of the Consumer. Preferences Indifference Curves Utility Functions Optimization Income & Substitution Effects. How do consumers make optimal choices?.

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How accurately can you (1) predict Y from X , and (2) predict X from Y ?

How accurately can you (1) predict Y from X , and (2) predict X from Y ?. 6 5 4 Y 3 2 1. 4/9. 2/9. 1/9. 1/9. 1/9. 1 2 3 4 5 6 X. How accurately can you (1) predict Y from X , and (2) predict X from Y ?. 6 5 4 Y 3 2 1.

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680XX Instruction Set

Outline Addressing Modes Move Instructions Arithmetic & Logical Instructions Shift/Rotate/Bit Instructions Compare & Bounds Checking Instructions Branch/Jump & Subroutine Instructions Synchronization Instructions Exception Instructions Misc. Instructions Goal Understand addressing modes

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Phenomenology, Simulation and Parameterization of Atmospheric Convection

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Chapter 4 Traversing

Chapter 4 Traversing. Definitions Traverse Series of straight lines connecting survey stations (begin at known points as baseline) Traversing : Determination of horizontal coordinates by measuring horizontal angles & distances Classification : closed vs. open

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The CATchment HYdrology (CATHY) Model

UNESCO-IHP Water Programme for Environmental Sustainability - WPA II. The CATchment HYdrology (CATHY) Model. Working Group: Claudio Paniconi and Mauro Sulis INRS-ETE, University of Quebec, Canada Mario Putti and Matteo Camporese University of Padova, Italy

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Coordinate Spaces and Transformations

Coordinate Spaces and Transformations. Jihoon.Yim 22/04/2008. Contents. Transformation of Coordinate Spaces World-space to Page-space Transformations Page-space to Device-space Transformations Device-Space to Physical-Device Transformation Default Transformations

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68000 Instruction Set (2)

68000 Instruction Set (2). Lecture Overview. The 68000 Instruction Set continued The understand and effectively use an architecture must understand the register set and the instruction set. Last time we looked at data movement and arithmetic instructions Now cover remaining instructions.

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Assimilating Reflectivity Observations of Convective Storms into Convection-Permitting NWP Models

Assimilating Reflectivity Observations of Convective Storms into Convection-Permitting NWP Models. David Dowell 1 , Chris Snyder 2 , Bill Skamarock 2 1 Cooperative Institute for Mesoscale Meteorological Studies, Norman, Oklahoma, USA

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3-2 ???????

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Electricity and Magnetism II

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a ? x ? b ? 1 ( x ) ? y ? ? 2 ( x )

Suppose that D is a simple region (a region which is both x -simple and y -simple) and that F = P ( x,y ) i + Q ( x,y ) j where P ( x,y ) and Q ( x,y ) are each functions with continuous first partial derivatives. y. y. a ? x ? b ? 1 ( x ) ? y ? ? 2 ( x ). c ? y ? d

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Evolutionary Computation on the Connex Architecture

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Outline of the presentation: - Tools : equations - potential vorticity anomalie (PVA)

Erosion of a surface vortex by a seamount on the beta plane Steven Herbette (PhD-SHOM), Yves Morel (SHOM), Michel Arhan (IFREMER). Outline of the presentation: - Tools : equations - potential vorticity anomalie (PVA) - Presentation of the problem - configuration - Erosion - one example

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Scan Conversion

Scan Conversion. Scan Conversion. Last step in the graphics pipeline Efficiency is a central issue Common primitives Lines (done last class) Polygons (fill polygons, today) Circles Hardware implementations preferable. Filling Polygons: Scan Line Algorithm. 14. 12. 10. 8. 6. 4. 2.

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Fill Algorithms

Fill Algorithms. Soon Tee Teoh CS 116B. Fill Algorithms. Given the edges defining a polygon, and a color for the polygon, we need to fill all the pixels inside the polygon. Three different algorithms: 1. Scan-line fill 2. Boundary fill 3. Flood fill. Scan Line Fill Algorithm.

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Consider a non-rectangular region D which can be described as

Suppose we want to integrate f ( x,y ) over a region D which is not necessarily a rectangle but can be contained inside a rectangle R . It will be helpful to classify certain types of non-rectangular regions. Consider a non-rectangular region D which can be described as

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Introduction to Implicit Differentiation

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y=f(x)

The function. has no inverse. f(x1)=f(x2)=f(x3)=y, so. y. y=f(x). y. x. x1. x2. x3. has no inverse. But if we treat g as a function. then it does have an inverse. y. y=g(x). y. x. y. y=f(x). x. Graphs of a function and its inverse are reflections in the line y=x. y.

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