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- W2090885370 abstract "Abstract Temporal and spatial variations in the structure of the lower atmosphere off Oregon's central coast are studied. The response of the wind and thermal fields to a synoptic-scale realignment aloft that causes a rapid shift from surface southerly to northerly winds is detailed. The effects and importance of the infrequent southerlies on the marine inversion, sea breezes and upwelling is also investigated. A vast array of meteorological and oceanographic observations were measured by aircraft, land stations, buoys and ships during the first Coastal Upwelling Experiment I (CUE-I). The winds, air and water temperature, and currents from the surface ocean layer to 1.5 km are compared during 16–29 August 1972. The period of southerly surface winds created a warm moist lower atmosphere, weak sea breezes, and brought about a cessation to previous upwelling. In contrast, northerlies and ridging aloft produced a distinct marine inversion, strong sea breezes, and an upwelling event. The marked changes reveal ..." @default.
- W2090885370 created "2016-06-24" @default.
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- W2090885370 date "1980-07-01" @default.
- W2090885370 modified "2023-09-23" @default.
- W2090885370 title "Low-Level Atmospheric Changes over Oregon's Coastal Upweliing Region" @default.
- W2090885370 doi "https://doi.org/10.1175/1520-0493(1980)108<1029:llacoo>2.0.co;2" @default.
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