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- W1998352803 abstract "Observations of a drainage flow event on a high-altitude simple slope were made for a few hours during a five-day field study that was otherwise characterized by high and gusty winds blowing across the face of the slope believed due to the presence of a nocturnal jet. A simple slope in the Jemez Mountains of north-central New Mexico was instrumented with meteorological surface stations and 10 m masts. Data collected during the drainage flow event indicate a depth ranging from greater than 10 m at the bottom of the slope to near zero at the top. At the bottom of the slope, the wind speed varied from 2.5 m s−1 at 1.5 m above ground to 0.5 m s−1 at a height of 10 m." @default.
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- W1998352803 date "1983-02-01" @default.
- W1998352803 modified "2023-09-25" @default.
- W1998352803 title "Observations of a Drainage Flow Event on a High-Altitude Simple Slope" @default.
- W1998352803 doi "https://doi.org/10.1175/1520-0450(1983)022<0331:ooadfe>2.0.co;2" @default.
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