'Small perturbation' presentation slideshows

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Towards lattice studies of Anomalous transport

Towards lattice studies of Anomalous transport

Towards lattice studies of Anomalous transport. Pavel Buividovich (Regensburg). To the memory of my Teacher, excellent Scientist, very nice and outstanding Person, Prof. Dr. Mikhail Igorevich Polikarpov. Before 2008: classical hydro = conservation laws shear/bulk viscosity

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538 views • 42 slides
Chapter 13

Chapter 13

Chapter 13. Time-Dependent Perturbation Theory. 13.A. The eigenproblem Let us assume that we have a system with an ( unperturbed ) Hamiltonian H 0 , the eigenvalue problem for which is solved and the spectrum is discrete and non-degenerate :

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315 views • 31 slides
MET 61 Introduction to Meteorology - Lecture 12

MET 61 Introduction to Meteorology - Lecture 12

MET 61 Introduction to Meteorology - Lecture 12. Midlatitude Cyclones Dr. Eugene Cordero San Jose State University Reading: Chapter 13 (Ahrens); Pg. 313-320 (W&H) Class Outline: Polar front theory Cyclone development QG Theory. Scale Time Scale Distance Scale Examples Macroscale

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699 views • 26 slides
Singular Value Decomposition of images from scanned photographic plates

Singular Value Decomposition of images from scanned photographic plates

Singular Value Decomposition of images from scanned photographic plates. Vasil Kolev Institute of Computer and Communications Systems Bulgarian Academy of Sciences Milcho Tsvetkov, Katya Tsvetkova, Ana Borisova Institute of Astronomy, Bulgarian Academy of Sciences

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308 views • 17 slides
Controlling Chaos!

Controlling Chaos!

Controlling Chaos!. Dylan Thomas and Alex Yang. Why control chaos?. One may want a system to be used for different purposes at different times Chaos offers flexibility (ability to switch between behaviors as circumstances change) Small changes produce large effects. How is it done?.

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361 views • 14 slides
Supersonic Potential Flow

Supersonic Potential Flow

Supersonic Potential Flow. For supersonic flow, we write the small perturbation potential equation as: Writing the equation in this form highlights the difference from the subsonic equation.

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946 views • 11 slides
Approximate Analytical/Numerical Solutions to the Groundwater Flow Problem

Approximate Analytical/Numerical Solutions to the Groundwater Flow Problem

Approximate Analytical/Numerical Solutions to the Groundwater Flow Problem. CWR 6536 Stochastic Subsurface Hydrology. 3-D Saturated Groundwater Flow. K(x,y,z) random hydraulic conductivity field f (x,y,z) random hydraulic head field No analytic solution exists to this problem

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237 views • 11 slides

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