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- W2283504408 abstract "Mean wind and turbulence data collected using an array of micrometeorological flux towers during the October 2006 METCRAX field campaign in Arizona’s Meteor Crater were analyzed to investigate the relationship between regional-scale ambient flows and the characteristics of temperature inversions inside the crater. Five micrometeorological towers were located along an east-west cross section through the center of the crater. The analyses of 5-min mean data from all the towers showed that a strong temperature inversion formed inside the crater when ambient regional-scale flows were weak. Under these conditions, the temperature inversion was confined to the lowest 10-20 m above the basin floor, with the bulk of the basin atmosphere being nearly isothermal. Turbulence was intermittent within the temperature inversion, but was often nearly continuous in the isothermal layer above the shallow surface-based inversion. When the regional scale flows exceeded approximately 5 m/s, the basin atmosphere became fully coupled with the atmosphere above and little or no temperature inversion formed inside the crater. A regionalscale drainage flow from the southwest often formed on clear nights, producing winds of 2-7 m/s at the crater rim. Because these winds were near the threshold speed, the crater atmosphere exhibited a range of behaviours on individual nights." @default.
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- W2283504408 date "2007-01-01" @default.
- W2283504408 modified "2023-09-23" @default.
- W2283504408 title "The development and characteristics of a cold air pool in a small, enclosed basin and its relationship with regional and large-scale forcing [presentation]" @default.
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