標題: Titlebook: An Introduction to Boundary Layer Meteorology; Roland B. Stull Textbook 1988 Kluwer Academic Publishers 1988 Cloud.Fog.Meteorology.Profil. [打印本頁] 作者: digestive-tract 時間: 2025-3-21 16:54
書目名稱An Introduction to Boundary Layer Meteorology影響因子(影響力)
書目名稱An Introduction to Boundary Layer Meteorology影響因子(影響力)學科排名
書目名稱An Introduction to Boundary Layer Meteorology網(wǎng)絡公開度
書目名稱An Introduction to Boundary Layer Meteorology網(wǎng)絡公開度學科排名
書目名稱An Introduction to Boundary Layer Meteorology被引頻次
書目名稱An Introduction to Boundary Layer Meteorology被引頻次學科排名
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書目名稱An Introduction to Boundary Layer Meteorology讀者反饋
書目名稱An Introduction to Boundary Layer Meteorology讀者反饋學科排名
作者: Accord 時間: 2025-3-21 20:35
1383-8601 sical physics. An additional attraction of the filed is the rich diversity of topics and research methods that are collected under the umbrella-term of boundary-layer meteorology. The flavor of the challenges and the excitement associated with the study of the atmospheric boundary layer are captured作者: Ordeal 時間: 2025-3-22 02:31 作者: 2否定 時間: 2025-3-22 08:13
Die Salvarsanbehandlung der Syphilis,n order end up with a useful description of turbulence that can be applied to real situations. In this Chapter, the unknowns are identified, and methods to parameterize them are reviewed. Simulation techniques such as large-eddy simulation are discussed in Chapter 10.作者: 寵愛 時間: 2025-3-22 12:21
Zeitliche Verteilung der Sal abscheidungen,r the variables of interest. Similarity theory provides a way to organize and group the variables to our maximum advantage, and in turn provides guidelines on how to design experiments to gain the most information.作者: 粗野 時間: 2025-3-22 14:20 作者: 廣大 時間: 2025-3-22 20:25 作者: 設施 時間: 2025-3-22 22:42 作者: collagenase 時間: 2025-3-23 04:44
Turbulence Closure Techniques,n order end up with a useful description of turbulence that can be applied to real situations. In this Chapter, the unknowns are identified, and methods to parameterize them are reviewed. Simulation techniques such as large-eddy simulation are discussed in Chapter 10.作者: Ambiguous 時間: 2025-3-23 08:56 作者: 可以任性 時間: 2025-3-23 12:26
Convective Mixed Layer,eddies into the sides of thermals, and vertical entertainment on the thermal scale into the whole mixed layer. In this chapter we examine the structure and evolution of the convective boundary layer, and study the forcings acting on it.作者: 法律的瑕疵 時間: 2025-3-23 16:50 作者: assail 時間: 2025-3-23 20:23 作者: 逃避現(xiàn)實 時間: 2025-3-24 00:15
Textbook 1988of conditions. It is assumed that the work will be used at the beginning graduate level for students with an undergraduate background in meteorology, but the author envisions, and has catered for, a heterogeneity in the background and experience of his readers..作者: 和平主義者 時間: 2025-3-24 05:16 作者: Supplement 時間: 2025-3-24 06:57
Some Mathematical & Conceptual Tools: Part 1. Statistics,erministic description difficult. Instead, we are forced to retreat to the use of statistics, where we are limited to average or expected measures of turbulence. In this chapter we review some basic statistical methods and show how measurements of turbulence can be put into a statistical framework. 作者: Interstellar 時間: 2025-3-24 14:05 作者: carotenoids 時間: 2025-3-24 18:41 作者: 豐滿中國 時間: 2025-3-24 22:11
Turbulence Kinetic Energy, Stability and Scaling, is directly related to the momentum, heat, and moisture transport through the boundary layer. Turbulence kinetic energy is also sometimes used as a starting point for approximations of turbulent diffusion.作者: anticipate 時間: 2025-3-25 01:00 作者: 埋葬 時間: 2025-3-25 07:12
Boundary Conditions and Surface Forcings,m the surface modify the state of the boundary layer. The heat and moisture fluxes are driven, in turn, by the external forcings such as radiation from the sun or transpiration from plants. Forcings across the top of the boundary layer also alter mean characteristics within it.作者: Resection 時間: 2025-3-25 07:58 作者: POWER 時間: 2025-3-25 12:16
Convective Mixed Layer, into identifiable structures such as thermals and plumes (Young, 1988). Entertainment happens at a variety of scales: lateral entertainment by small eddies into the sides of thermals, and vertical entertainment on the thermal scale into the whole mixed layer. In this chapter we examine the structur作者: incite 時間: 2025-3-25 15:52
Boundary Layer Clouds,flux divergence in the boundary layer are altered by clouds, and these effects are emerging as important aspects of the climate-change problem. In addition, the radiative effects combine with latent heating to modulate BL dynamics, turbulence generation, and evolution. This chapter provides a brief 作者: Obscure 時間: 2025-3-25 20:22
Geographic Effects,ographic variations can modify the boundary-layer flow, and in some cases generate circulations in conjunction with diurnal heating cycles. We have already touched on a few such flows, such as the drainage winds at night within a stable boundary layer. In this chapter we examine both geographically-作者: 商議 時間: 2025-3-26 01:51 作者: savage 時間: 2025-3-26 05:09 作者: 秘密會議 時間: 2025-3-26 08:53
Zeitliche Verteilung der Sal abscheidungen,Spectrum analysis is a statistical tool that we can employ to probe further into the workings of turbulence. By decomposing a series of measurements into frequency or wavenumber components, we can discover how eddies of different time and space scales contribute to the overall turbulence state.作者: lobster 時間: 2025-3-26 15:02 作者: 危機 時間: 2025-3-26 18:01 作者: Admonish 時間: 2025-3-26 20:59 作者: 荒唐 時間: 2025-3-27 01:41 作者: Missile 時間: 2025-3-27 09:10
Stable Boundary Layer,The boundary layer can become stably stratified whenever the surface is cooler than the air. This stable boundary layer (SBL) often forms at night over land, where it is known as a nocturnal boundary layer (NBL). It can also form by advection of warmer air over a cooler surface.作者: appall 時間: 2025-3-27 09:55 作者: ablate 時間: 2025-3-27 15:17
An Introduction to Boundary Layer Meteorology978-94-009-3027-8Series ISSN 1383-8601 Series E-ISSN 2215-162X 作者: CLOT 時間: 2025-3-27 21:20 作者: 讓步 時間: 2025-3-27 23:36 作者: Inkling 時間: 2025-3-28 02:54 作者: Calibrate 時間: 2025-3-28 06:55 作者: BORE 時間: 2025-3-28 14:23 作者: 態(tài)學 時間: 2025-3-28 16:12
Zusammenfassung der Untersuchung in Thesen,ographic variations can modify the boundary-layer flow, and in some cases generate circulations in conjunction with diurnal heating cycles. We have already touched on a few such flows, such as the drainage winds at night within a stable boundary layer. In this chapter we examine both geographically-generated and geographically-modified flows.作者: agitate 時間: 2025-3-28 22:16
Juridicum – Schriftenreihe zum StrafrechtIt is here where our crops are grown, our dwellings are constructed, and much of our commerce takes place. We grow familiar with our local breezes and microclimates, and we sense the contrasts when we travel to other places.作者: seruting 時間: 2025-3-29 02:50 作者: geometrician 時間: 2025-3-29 03:55
https://doi.org/10.1007/978-3-642-86354-7ermodynamics of the gases in our atmosphere. Motions in the boundary layer are slow enough compared to the speed of light that the Galilean/Newtonian paradigm of classical physics applies. These equations, collectively known as the ., contain time and space derivatives that require initial and bound作者: HUMP 時間: 2025-3-29 07:49
https://doi.org/10.1007/978-3-642-86354-7ations (3.5.3c) through (3.5.3g) contains a covariance like . or .. In order to use those previous equations, we can either evaluate the covariances experimentally, or we can derive additional equations to forecast the covariances.作者: FLAG 時間: 2025-3-29 13:33
https://doi.org/10.1007/978-3-662-33122-4 is directly related to the momentum, heat, and moisture transport through the boundary layer. Turbulence kinetic energy is also sometimes used as a starting point for approximations of turbulent diffusion.作者: bizarre 時間: 2025-3-29 16:59 作者: 搖曳的微光 時間: 2025-3-29 22:59 作者: 記憶法 時間: 2025-3-30 00:01
Zeitliche Verteilung der Sal abscheidungen,ss, boundary layer observations frequently show consistent and repeatable characteristics, suggesting that we could develop empirical relationships for the variables of interest. Similarity theory provides a way to organize and group the variables to our maximum advantage, and in turn provides guide作者: 種屬關(guān)系 時間: 2025-3-30 05:03
https://doi.org/10.1007/978-3-662-34054-7 into identifiable structures such as thermals and plumes (Young, 1988). Entertainment happens at a variety of scales: lateral entertainment by small eddies into the sides of thermals, and vertical entertainment on the thermal scale into the whole mixed layer. In this chapter we examine the structur作者: 闡釋 時間: 2025-3-30 08:40
Zusammenfassung der Untersuchung in Thesen,flux divergence in the boundary layer are altered by clouds, and these effects are emerging as important aspects of the climate-change problem. In addition, the radiative effects combine with latent heating to modulate BL dynamics, turbulence generation, and evolution. This chapter provides a brief