Flux‐gradient relationships in the constant flux layer
Abstract An analysis is made of the Monin‐Obukhov function Φ M in the familiar wind profile equation, using data from two recent expeditions to Gurley (New South Wales) and Hay ...
Abstract An analysis is made of the Monin‐Obukhov function Φ M in the familiar wind profile equation, using data from two recent expeditions to Gurley (New South Wales) and Hay ...
Abstract The diabatic mean profile forms in the surface layer are studied, by applying analysis methods having high resolving power to data from O'Neill, U.S.A. (heights up to 6...
An extension of the Tahiti minus Darwin Southern Oscillation Index (SOI) from 1882 back to 1876 is reported following the recovery of early Darwin mean sea-level pressure data s...
A general method for calibrating Sun photometers that relaxes the constraints on atmospheric conditions is described. Instead of requiring constant extinction conditions the met...
The availability of GODAE Oceanview-type ocean forecast systems provides the opportunity to develop high-resolution, short- to medium-range coupled prediction systems. Several g...