Tellus · 1976 · 12 citations · 4 references
Natural SciencesEarth SciencesMeteorologyAir-sea InteractionAtmospheric SciencePhysical OceanographySea BreezesSea-breeze CirculationsWind StressLand-sea Breeze InteractionSea Breeze ObservationSea Breeze VariabilitySea-breeze Circulation StructureSea-breeze PropagationSea-breeze Return FlowSea-breeze TimingUpper-level Wind Analysis
Using surface and upper wind observations on three days at each of three sites in north-western Saudi Arabia it was found that the sea breeze could extend at least 225 km inland at an average speed of 6.7 m sec-l between 1445 and 2300. At 25 km inland both the on-shore component and the off-shore return flow above it were about 1.2 km deep. At this site two increases in dew point, separated by about two hours, fol-lowed the arrival of the sea breeze and may have represented the arrival of air with a mostly land track followed by air with a mostly sea track. An unexplained fall in dew point immediately preceded the arrival of the sea breeze on six out of 11 days.
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D. E. Pedgley · Weather · 1966 · 26 citations
Tetroon Trajectories in an Urban Atmosphere
J. K. Angell, Donald H. Pack, George C. Holzworth et al. · Journal of applied meteorology · 1966 · 22 citations · Full text