影响带来
发表于 2025-3-26 21:56:22
Childhood, Youth and University Studies,es is possible. The horizontal sizes of the most rapidly growing modes, as a rule, are an order of magnitude larger than the vertical sizes. The possibility of observing this instability under natural conditions is discussed.
assent
发表于 2025-3-27 03:20:25
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转换
发表于 2025-3-27 08:42:34
Ground-Based Remote Sensing of the Atmospheric Boundary Layer: 25 Years of Progress,then discussed, including the sea breeze, convergence boundaries, dispersion, and boundary-layer cloud systems. The review concludes with a discussion of the likely future role of remote sensors in boundary-layer research.
开头
发表于 2025-3-27 12:44:23
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Bouquet
发表于 2025-3-27 13:44:12
Book 1996R.E. Munn served as Editor-in-Chiefuntil recently. The special 25th Anniversary volume, on which thisbook is based, was compiled from review and other articles solicitedand selected as a `Festschrift‘ to honour Ted Munn‘s achievement aseditor of the journal over that time. .Articles by leading contr
GULP
发表于 2025-3-27 18:42:57
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BYRE
发表于 2025-3-27 22:34:02
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适宜
发表于 2025-3-28 04:00:29
https://doi.org/10.1007/978-3-031-66123-5 evaporation coefficient at wind speeds above 15 m s. have not been substantiated. Wind stress measurements showed a relationship with wave age. New methods were developed for coping with flow distortion.
LATER
发表于 2025-3-28 06:16:24
https://doi.org/10.1007/978-94-017-0489-2f and is related to similar studies conducted in the early 1980s. Data limitations are discussed and applications of numerical and wind-tunnel models to Askervein are outlined. Problems associated with model simulations are noted and model results are compared with the field measurements.
臆断
发表于 2025-3-28 10:52:10
,The Atmospheric Boundary Layer — Advances in Knowledge and Application,odelling of selected phenomena; (ii) numerical weather prediction; and (iii) climate simulations. Future trends are identified, including the incorporation into models of advanced cloud schemes and interactive canopy schemes, and the nesting of high resolution boundary-layer schemes in global climate models.