Oke, T. R., 1987: Boundary layer climates. 2nd ed. London Routledge, 435 pp.Oke T R.Boundary Layer Climates[M].London:Routledge, 1987.Oke, T. R.,Boundary Layer Climates, Methuen & Co., Ltd., London, 1978.Oke, T. R. "Boundary Layer Climates". 2 ed. London: Methuen, 1987....
出版者:Routledge 作者:Oke, T. R. 出品人: 页数:435 译者: 出版时间:1988-1 价格:802.00元 装帧:Pap isbn号码:9780415043199 丛书系列: 图书标签:建筑学习 Boundary Layer Climates 2024 pdf epub mobi 电子书 图书描述 This modern climatology textbook explains those climates formed near the ground in terms...
Boundary layer climates Oke, T. R.: Boundary Layer Climates, 2nd edn., Routledge, New York, 435 pp., 1987. Paterson, W. S. B.: The Physics of Glaciers, 3rd edn.,... SB Idso 被引量: 13发表: 1980年 Experimental Urban Heat Island Research of Four Biggest Polar Cities in Northern ...
Oke TR (1988) Boundary layer climates, 2nd edn. Routledge, London, p 435 Google Scholar Oke TR, Mills G, Christen A, Voogt JA (2017) Urban climates. Cambridge University Press. https://doi.org/10.1017/9781139016476 Book Google Scholar Park S, Shin J (2019) Heuristic estimation of low...
Roll vortices are a very common phenomenon in the daytime convective boundary layer. In the presence of such large-scale organized structures, single-tower measurement must be biased, because the associated vertical energy transport is inherently not captured (Etling and Brown1993). Under strongly uns...
Correspondence toJ. B. R. Loureiro. Rights and permissions Reprints and permissions About this article Cite this article Loureiro, J.B.R., Monteiro, A.S., Pinho, F.T.et al.Water-Tank Studies of Separating Flow Over Rough Hills.Boundary-Layer Meteorol129, 289–308 (2008). https://doi....
Time-lapse photography and its teaching usefulness in planetary boundary layer meteorology Abstract In this paper, the author shares her experiences in producing time-lapse movies dedicated to teaching introductory level meteorology and micro-meteorology, intended as dynamical phenomena unfolding in time. ...
A theoretical background has been developed using MOST to estimate the vertical turbulent fluxes within the surface layer with non-dimensional parameters. Indeed, the theory relates the turbulent flux of a quantity with its mean vertical gradient through a so-called universal function\(\phi \)that...
Oke, T.R. Boundary Layer Climates, 2nd ed.; Routledge: London, UK, 1992. [Google Scholar] Hogan, R.J.; Grant, A.L.M.; Illingworth, A.J.; Pearson, G.N.; O’Connor, E.J. Vertical velocity variance and skewness in clear and cloud-topped boundary layers as revealed by Doppler lid...