By Sam Miller

ISBN-10: 1107100712

ISBN-13: 9781107100718

This textbook on atmospheric thermodynamics is for college kids of meteorology or atmospheric technological know-how. It additionally serves as a reference textual content for operating execs in meteorology and climate forecasting. it truly is distinct since it presents entire, calculus-based derivations of simple physics from first ideas, and connects mathematical relationships to real-world, useful climate forecasting purposes. labored examples and perform difficulties are integrated all through.

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Extra resources for Applied Thermodynamics for Meteorologists

Example text

Using this convention, locations to the north of the origin would correspond to positive y values, and locations south of the origin would correspond to negative values of y. 5. Two-dimensional hill. A positive slope implies that the height of the hill is increasing as you go north, or decreasing as you go south. A negative slope implies that the height of the hill is decreasing as you go north, or increasing as you go south. 6. Three-dimensional hill. 13a), the expression means the partial derivative of z with respect to x, with the subscript y indicating that the operation is performed with y treated as a constant.

That’s the province of the First Law of Thermodynamics, which we’ll return to in Chapter 4. In this section we’ll derive four of them. Forms involving density and specific volume. 39) Form involving number of moles. 42) R* is also the product of two constants, Avogadro’s Number (NA) and Boltzmann’s Constant11 (k), and is computed by: which we’ll return to a bit later. 46) where n is the number of kmols of substance in the sample of gas. This form of the Ideal Gas Law is probably more familiar to meteorology undergraduates who have taken a twoor three-semester sequence in basic university physics.

Using this convention, locations to the north of the origin would correspond to positive y values, and locations south of the origin would correspond to negative values of y. 5. Two-dimensional hill. A positive slope implies that the height of the hill is increasing as you go north, or decreasing as you go south. A negative slope implies that the height of the hill is decreasing as you go north, or increasing as you go south. 6. Three-dimensional hill. 13a), the expression means the partial derivative of z with respect to x, with the subscript y indicating that the operation is performed with y treated as a constant.

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Applied Thermodynamics for Meteorologists by Sam Miller


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