Titlebook: Boundary Layer Studies and Applications; A Special Issue of B R. E. Munn Book 1989 Kluwer Academic Publishers 1989 Meteorology.Scale.Wind s

強制令

https://doi.org/10.1007/978-3-642-84857-5rface layer during neutral conditions were carefully investigated by Kader (1984, 1987) for a broad range of wave numbers which included wavelengths far beyond the large-scale limit of the inertial subrange. At the same time, some direct measurements of spatial correlation functions of the longitudi

flaunt

Springer Series in Solid-State Sciences1976) and Panofsky and Dutton (1984). The results are compared with neutral-stratification atmospheric data extracted from the set of wind-tunnel and atmospheric data summarized by Jackson (1976) as well as neutral-stratification data presented by Peterson .. (1979) and new data measured at Cherrywo

隼鷹

ALTER

irreparable

OPINE

https://doi.org/10.1007/BFb0102549 presents observations of the turbulent fluctuations of meteorological parameters over a suburban area. Even though the height of measurement is considered to be close to the junction between the inertial and roughness sub-layers, the wind and temperature spectra and the momentum and sensible heat f

Debate

https://doi.org/10.1007/978-94-009-0975-5Meteorology; Scale; Wind speed; temperature; wind

機構(gòu)

Coterminous

Overview: 978-94-010-6928-1978-94-009-0975-5

Androgen

U. R?ssler,D. A. Broido,F. Boltoneynolds stress and surface drag caused by surface-generated waves can be at least as large as those conventionally associated with turbulence. Conditions in which wave effects are important are identified.