Abstract
Abstract An actual three-dimensional analysis and the corresponding theoretical computation show that a cold cA air tongue intruding southward about the middle of January 1956 along the eastern side of the Rocky Mountains causes the overrunning warmer current to curve convexly toward the lower pressure side. The current behaves similarly to flow over terrestrial topography of the same shape. Moreover the results indicate that a cold air dome can produce perturbations as large as those produced by the Rocky Mountains.
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