Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN: 9780134746241
Author: Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher: PEARSON
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Question

where ε = 0.622 (unitless) and yields w in g/kg. This reveals that w is partially dependent on atmospheric pressure, p. What does this formula suggest about the effect of pressure on the actual moisture content at higher elevations?

In the equation presented: \[ w = \varepsilon \times \frac{e}{p} \] - \(w\) represents a variable or a rated quantity. - \(\varepsilon\) (epsilon) is another variable or a parameter in the equation. - \(e\) is the numerator of the fraction. - \(p\) is the denominator of the fraction. - The fraction \(\frac{e}{p}\) indicates division of \(e\) by \(p\). - The symbol \(\times\) denotes multiplication. This equation might be used in a context such as physics, engineering, or economics where \(w\) could be a result of some combination of \(\varepsilon\) and the ratio of \(e\) to \(p\).
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Transcribed Image Text:In the equation presented: \[ w = \varepsilon \times \frac{e}{p} \] - \(w\) represents a variable or a rated quantity. - \(\varepsilon\) (epsilon) is another variable or a parameter in the equation. - \(e\) is the numerator of the fraction. - \(p\) is the denominator of the fraction. - The fraction \(\frac{e}{p}\) indicates division of \(e\) by \(p\). - The symbol \(\times\) denotes multiplication. This equation might be used in a context such as physics, engineering, or economics where \(w\) could be a result of some combination of \(\varepsilon\) and the ratio of \(e\) to \(p\).
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