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Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions

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Blackadar, Alfred K.·1957·Bulletin of the American Meteorological Society

Abstract

A sharp maximum is frequently observed at night in the wind speed profile below 3000 ft. The wind speed maximum is usually at the top of the nocturnal inversion, is supergeostrophic, and is often associated with extremely large values of wind shear at low levels. It is shown that the characteristic velocity profile tends to promote an orderly growth of the nocturnal inversion. The supergeostrophic wind speeds suggest that an inertia oscillation is induced when the constraint imposed by the daytime mixing is released by the initiation of an inversion at about the time of sunset.

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Metadata

Authors
Blackadar, A. K.
Venue
Bulletin of the American Meteorological Society
Published
1957-05
Volume
38
Issue
5
Pages
283-290
ISSN
  • 0003-0007 (ISSN-L)
  • 1520-0477
OpenAlex
W2888504372
Cited by
1,089
References
0
FWCI
13.85
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions. https://app.cochat.ai/papers/10.1175/1520-0477-38.5.283
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Blackadar, A. K. (1957). Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions. Bulletin of the American Meteorological Society. https://doi.org/10.1175/1520-0477-38.5.283

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.