We first demonstrate that the central pressure deficit is highly predictable from the low-level wind field via gradient wind balance. We then show that this relationship reduces to a dependence on two ...

The value of the constant K in the pressure velocity relation P = KV2 was found to be 0-0027, a result some what smaller than those found by Dines, Frowde, and Langley.

MANY years ago an investigation was begun by me to determine the relative velocity of wind and wave in deep water when the former has operated for a sufficient time to produce a constant condition ...