By using the portable 3-D rotating tank during the summer and fall semester 2007, we were able to supplement the theoretical treatment of fronts, Ekman layers, the Hadley circulation, baroclinic instability, western boundary currents, free convection, and thermohaline circulations. The 3-D tank was used to represent large-scale atmospheric circulation patterns that arose from density gradients influenced by rotation, as well as the evolution of patterns as rotation rate varied. Through the use of a 2-D wave tank, we were able to represent free convection and the development of secondary circulations which showed excellent visual examples of over-shooting tops of thunderstorms, the subsequent generation of gravity waves and how the anvil is produced. The 2-D tank also shows key concepts in the ocean as well as the atmosphere. Examples of ocean up-welling and return circulations from persistent wind forcing across a water surface.
By understanding the concepts and the theory behind these experiments, we were able to provide visual support to the professors that are lecturing in undergraduate oceanography and meteorology classes. Some of the senior level courses used to demonstrate these experiments are: climate dynamics, meso-and storm-scale meteorology, synoptic meteorology. Junior level courses consisted of atmospheric dynamics and thermodynamics.
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