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- W2083193895 abstract "Summer-time wind patterns have been monitored within and above a transverse valley of the Judaean Hills. Near surface anemograph records and pilot balloon observations have been analysed to identify three vertically separated wind regimes. Classical mountain/valley winds dominate the flow within the valley walls whereas the regional gradient flow is discerned above 400 m AGL or 700 m ASL. Sandwiched between these regimes is a breeze layer which reflects the diurnal rhythm of the coastal, mesoscale breezes which are driven by local sea-land temperature contrasts under the influence of the inland hills and the Coriolis force." @default.
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- W2083193895 date "1986-01-01" @default.
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- W2083193895 title "The interaction of valley/mountain winds with A diurnally veering sea/land breeze" @default.
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- W2083193895 doi "https://doi.org/10.1002/joc.3370060508" @default.
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