Abstract: Observations have shown the existence of a diurnal oscillation of the wind profile in the springtime boundary layer of the central United States called the Great Plains low-level jet. This low-level jet is a mesoscale ...

Abstract: Thermally induced circulations, similar to sea breezes, may be established in the presence of horizontal gradients in soil moisture, soil type, vegetation, or snow cover. The expense of extensive observational networks and ...