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Walter Munk and Bruce Bills

) and has a maximum near p = 1. Fig . 4. (top) Sketch of proposed radiative balance. (bottom) The assumed radiative flux density relative to a mean radiation, with a zero crossing at 36° latitude; in a steady state the integrated tropical excess equals the polar deficit, and the poleward transport of heat across the zero latitude: F Tropics = F polar = F . A variable obliquity modulates the incoming radiation by δF Tropics , δF polar and independently modulates the poleward transport by

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