'Magnitude' diaporamas de présentation

Chap 4 Image Enhancement in the Frequency Domain

Chap 4 Image Enhancement in the Frequency Domain. Any periodic function can be expressed as the sum of sines and cosines of different frequencies, each multiplied by a different coefficient. We called this sum a Fourier series.

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Chapter 5 Design

Chapter 5 Design. Acceptable vibration levels (ISO) Vibration isolation Vibration absorbers Effects of damping in absorbers Optimization Viscoelastic damping treatments Critical Speeds Design for vibration suppression . 5.1 Acceptable levels of vibration.

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Implementing XBRL for a cross-border banking group in Europe

Implementing XBRL for a cross-border banking group in Europe. Giancarlo Pellizzari Head of Prudential Policy Dexia Group. Paris, June 22nd to 25th, 2009. Agenda . Implementing XBRL for a cross-border banking group in Europe. Agenda. Introduction. What does XBRL mean for Dexia? .

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Health, work & well-being

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Vectors

Vectors. Sections 6.6. Objectives. Rewrite a vector in rectangular coordinates (in terms of i and j ) given the initial and terminal points of the vector. Determine the magnitude and direction of a vector given in terms if i and j .

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Force and Motion-II: continued Friction and Drag;Circular Motion

Force and Motion-II: continued Friction and Drag;Circular Motion. Lecture 6 Monday:2 February 2004. UNIFORM CIRCULAR MOTION. CIRCULAR MOTION. When an object travels in a circle, its velocity is constantly changing (in direction-at least).

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Newton 3 & Vectors

Newton 3 & Vectors. Action/Reaction. When you lean against a wall, you exert a force on the wall. The wall simultaneously exerts an equal and opposite force on you. . You Can OnlyTouch as Hard as You Are Touched. He can hit the massive bag with considerable force.

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Can we use a statistical cloud scheme coupled to convection and moist turbulence parameterisations to simulate all clo

Can we use a statistical cloud scheme coupled to convection and moist turbulence parameterisations to simulate all cloud types? Colin Jones CRCM/UQAM jones.colin@uqam.ca. 1-D TKE equation used in HIRLAM. A. B. C. D. A is buoyant production. B is shear production.

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San Andreas Fault

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Lesson 9-3

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Factors Affecting the Magnitude of Muscle Force

Factors Affecting the Magnitude of Muscle Force. Velocity of muscle shortening Length of the muscle when it is stimulated Time interval between muscle stimulation and tension development (electromechanical delay). Force-Velocity Relationship. Concentric Contraction

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Vision Screening for Children

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Forces Affecting Movement

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Magnetometer calibration and detection

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1958 Lituya Bay, Alaska Earthquake Magnitude 7.9 Rupture Length 90 to 280 km Surface Displacement 3.5 to 6.5 m

1958 Lituya Bay, Alaska Earthquake Magnitude 7.9 Rupture Length 90 to 280 km Surface Displacement 3.5 to 6.5 m. Photographs by Lloyd Cluff and George Plafker. Fairweather fault. 1958 Lituya Bay Earthquake, M 7.9 Rupture length 95 to 280 km Fairweather fault 6.2 m RL. Lituya Bay.

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Earnings Surprises and Signal Analysis

Earnings Surprises and Signal Analysis . matt mcConnell David Nabwangu Eskil Sylwan Johnson Yeh. Agenda. Background Hypothesis Methodology Data Fitting Explanatory Variables Regression Results Conclusion. Market Reaction to News . In an Ideal World. Reality.

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Balanced and Unbalanced Forces

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Balanced and Unbalanced Forces

Balanced and Unbalanced Forces. What is a force?. A force is a push or pull that causes an object to move, stop, or change direction In physics a force is anything that makes an object accelerate. Force. Forces come in pairs Forces have a magnitude and a direction. Magnitude: 5N

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The Hertzsprung-Russell Diagram (a.k.a. H-R Diagram)

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Blank Bode Amplitude Plot

Blank Bode Amplitude Plot. Edit the scale labels/exponents as needed Use Drawing tools to add straight-line asymptotes. 40. 30. 20. 10. 0. Magnitude, |H|, dB. -10. -20. -30. -40. -50. -60. 10 -2. 10 -1. 10 0. 10 1. 10 2. 10 3. 10 4. Frequency, ? , [rad/s].

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