Kelvin waves and internal bores in the marine boundary layer inversion andtheir relationship to coastally trapped wind reversals

Detailed observations of a coastally trapped disturbance, or wind reversal, on 10-11 June 1994 along the California coast provide comprehensive docume ntation of its structure, based on aircraft, wind profiler, radio acoustic sounding system, and buoy measurements. Unlike the expectations from earlie r studies based on limited data, which concluded that the deepening of the marine boundary layer (MBL) was a key factor, the 1994 data show that the p erturbation was better characterized as an upward thickening of the inversi on capping the MEL. As the event propagated over a site, the reversal in th e alongshore wind direction occurred first within the inversion and then 3- 4 h later at the surface. A node in the vertical structure (defined here as the altitude of zero vertical displacement) is found just above the invers ion base, with up to 200-m upward displacements of isentropic surfaces abov e the node, and 70-m downward displacements below. Although this is a single event, it is shown that the vertical structure ob served is representative of most other coastally trapped wind reversals. Th is is determined by comparing a composite of the 10-11 June 1994 event, bas ed on measurements at seven buoys, with surface pressure perturbations calc ulated from aircraft data. These results are compared to the composite of m any events. In each case a weak pressure trough occurred between 2.4 and 4. 0 h ahead of the surface wind reversal, and the pressure rose by 0.32-0.48 mb between the trough and the wind reversal. The pressure rise results from the cooling caused by the inversion's upward expansion. The propagation and structure of the event are shown to be best characteriz ed as a mixed Kelvin wave-bore propagating within the inversion above the M EL, with the MBL acting as a quasi-rigid lower boundary. If the MBL is inst ead assumed to respond in unison with the inversion, then the theoretically predicted intrinsic phase speeds significantly exceed the observed intrins ic phase speed. The hybrid nature of the event is indicated by two primary characteristics: 1) the disturbance had a much shallower slope than expecte d for an internal bore, while at the same time the upward perturbation with in the inversion was quasi-permanent rather than sinusoidal, which more clo sely resembles a bore; and 2) the predicted phase speeds for the "solitary" form of nonlinear Kelvin wave and for an internal bore are both close to t he observed intrinsic phase speed.