
In order to progress from Part 1 to Part 2, a student must achieve a threshold performance. The achievement of a threshold performance at Part 1 qualifies a student for a Certificate of Higher …
2. Additional information: Include any additional information about the reassessment here (e.g. how the reassessment relates to the module learning outcomes or rationale for the choice and …
2.2 1-D Conservation Law ...........................................................................................................12 2.2.1 Non-Conservative Schemes............................................................................................12
Modules completed at Part 2 and Part 3 regardless of place of study, will contribute to the classification of degrees. For further information about your Programme please refer to the …
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Dimensional Analysis
Since E is an energy it has dimensions M L2T−2. The right hand side of the equation can also be seen to have this dimension, if we recall that m is a mass and c is the speed of light (with …
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Maths for Science
Everybody is familiar with the counting numbers (1, 2, 3, etc.), but scientists also make use of other kinds of numbers, so it is appropriate to begin this course with some revision of numbers …
2 Fourier Transform The Fourier Transform transforms a function f which is defined over space (or time) into the frequency domain, so that it is defined in terms of Fourier coefficients.
particle 2 is at 0.2 of the Ny independent observations of the Ny independent observations is the standard deviation of the observation errors These are two almost perfect particles, what more …
2.2 Useful References Some books and www sites on doing a PhD that students have found useful are given below:
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Chapter 7: Vorticity
The locally vertical component of planetary vorticity is the Coriolis parameter: f = 2 W sin f x is the relative vorticity , the vorticity relative to the earth surface.