Atmosphere, Ocean and Climate Dynamics: An Introductory Text by John Marshall

By John Marshall

For complicated undergraduate and starting graduate scholars in atmospheric, oceanic, and weather technological know-how, surroundings, Ocean and weather Dynamics is an introductory textbook at the circulations of the ambience and ocean and their interplay, with an emphasis on worldwide scales. it's going to provide scholars a superb snatch of what the ambience and oceans seem like at the large-scale and why they appear that approach. The position of the oceans in weather and paleoclimate can be mentioned. the combo of observations, thought and accompanying illustrative laboratory experiments units this article aside through making it obtainable to scholars without earlier education in meteorology or oceanography. * Written at a mathematical point that's beautiful for undergraduates andbeginning graduate scholars* presents an invaluable academic instrument via a mix of observations andlaboratory demonstrations which are seen over the net* includes directions on the best way to reproduce the easy yet informativelaboratory experiments* comprises copious difficulties (with pattern solutions) to assist scholars study thematerial.

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Additional info for Atmosphere, Ocean and Climate Dynamics: An Introductory Text

Sample text

In this chapter, we discuss the nature of the convective process and its role in determining the radiative-convective balance of the troposphere. 31 32 4. 1. Solar radiation warms the Earth’s surface, triggering convection, which carries heat vertically to the emission level from which, because the atmosphere above this level is transparent in the IR spectrum, energy can be radiated out to space. The surface temperature of about 288 K is significantly higher than the temperature at the emission level, 255 K, because the energy flux from the surface must balance not just the incoming solar radiation but also downwelling IR radiation from the atmosphere above.

This is closer to the actual mean surface temperature of 288 K but is now an overestimate! The model we have discussed is clearly an oversimplification: • For one thing, not all the solar flux incident on the top of the atmosphere reaches the surface; typically, 20%–25% is absorbed within the atmosphere (including by clouds). 2 that IR absorption by the atmosphere is incomplete. The greenhouse effect is actually less strong than in the model assumed previously, and so Ts will be less than the value implied by Eq.

Using the hot and cold water supply we can achieve a temperature difference of 20◦ C over the depth of the tank. The temperature profile is measured and recorded using thermometers attached to the side of the tank.

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