標(biāo)題: Titlebook: Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields; Albert Gyr,Franz-S. Rys Book 1995 Springer Science+Business Me [打印本頁(yè)] 作者: Traction 時(shí)間: 2025-3-21 19:48
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields影響因子(影響力)
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields影響因子(影響力)學(xué)科排名
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields被引頻次
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields被引頻次學(xué)科排名
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields年度引用
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields年度引用學(xué)科排名
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields讀者反饋
書(shū)目名稱Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields讀者反饋學(xué)科排名
作者: 外表讀作 時(shí)間: 2025-3-21 23:10
Boundary Conditions and Treatment of Topography in Limited-Area Models,s of conserved integrals — are conveniently cast into differential form, the hydrodynamical equations. Depending on the application, these equations are altered to a variety of different forms with different mathematical properties and different requirements on initial and/or boundary conditions in 作者: OCTO 時(shí)間: 2025-3-22 01:48
Thermodynamic and Radiative Processes in the Atmosphere, and thermal characteristics of the atmosphere. Air flow will determine the speed and direction with which a meteorological variable will be transported and dispersed, while the thermal structure of the atmosphere will control the nature of the dispersion through local stability or instability, such作者: RENAL 時(shí)間: 2025-3-22 05:23 作者: ILEUM 時(shí)間: 2025-3-22 12:33 作者: 免費(fèi) 時(shí)間: 2025-3-22 15:41
Inversion layers,ace within so-called atmospheric inversion layers, namely the layers characterized by the increase of the absolute temperature with height. In the course of the diurnal evolution of the atmospheric planetary boundary layer the two most typical examples of the sublayers with the inverse temperature g作者: 免費(fèi) 時(shí)間: 2025-3-22 18:07
Reflexive Practice for the Times We Live In as the presence of inversion layers which act as a “l(fā)id” and strongly inhibit vertical motion. Inversion situations are especially important for air quality problems, as poor dispersion and trapping of pollutants beneath the inversion will inevitably lead to poor local and regional air quality.作者: 不利 時(shí)間: 2025-3-22 23:51 作者: Accessible 時(shí)間: 2025-3-23 04:47 作者: 門(mén)閂 時(shí)間: 2025-3-23 06:40
Book 1995amage in the case of accidents, and to evaluate thepossible influence of existing or planned sources. In most cases, suchpredictions depend on high-speed computation. .The present textbook presents a mathematically explicit introductionin eight chapters: 1: An introduction to the basics of fluid dyn作者: ANN 時(shí)間: 2025-3-23 12:20
Thermodynamic and Radiative Processes in the Atmosphere, as the presence of inversion layers which act as a “l(fā)id” and strongly inhibit vertical motion. Inversion situations are especially important for air quality problems, as poor dispersion and trapping of pollutants beneath the inversion will inevitably lead to poor local and regional air quality.作者: 多骨 時(shí)間: 2025-3-23 14:29
Atmospheric Boundary-Layer Processes and Influence of Inhomogeneous Terrain,ofiles of these meteorological variables and their fluxes. It will be clear these profiles will depend strongly on the process that determines vertical transport in the boundary layer. This process is turbulence. Therefore, the study of the atmospheric boundary layer is almost synonym with a study of atmospheric turbulence.作者: muscle-fibers 時(shí)間: 2025-3-23 18:29
Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields978-94-015-8547-7Series ISSN 1382-4309 Series E-ISSN 2215-1826 作者: Dignant 時(shí)間: 2025-3-24 00:49 作者: Coma704 時(shí)間: 2025-3-24 03:38
Ein Zeitalter radikaler Ungewissheith scales of atmospheric motion according to:.In spatial extension, the surface layer extends from the ground and up to a few hundred meters in the vertical. It is characterized by approximately constant fluxes of heat and momentum which can be determined by measurements near the surface.作者: Outspoken 時(shí)間: 2025-3-24 06:38
Phil C. Langer,Angela Kühner,Panja Schwederace within so-called atmospheric inversion layers, namely the layers characterized by the increase of the absolute temperature with height. In the course of the diurnal evolution of the atmospheric planetary boundary layer the two most typical examples of the sublayers with the inverse temperature gradient can be observed.作者: 突變 時(shí)間: 2025-3-24 13:02 作者: Arthritis 時(shí)間: 2025-3-24 18:28
Panja Schweder,Phil C. Langer,Angela KühnerThere is no generally-accepted theory of the climatology of cities, yet. The urban climate is altogether an old subject of investigations, since the book of Howard (1833), and a new one because of this lack of generally-accepted framework: new techniques and new approaches are likely to produce new breakthroughs.作者: 教育學(xué) 時(shí)間: 2025-3-24 23:02 作者: Femine 時(shí)間: 2025-3-24 23:25 作者: frozen-shoulder 時(shí)間: 2025-3-25 06:20 作者: 鋪?zhàn)?nbsp; 時(shí)間: 2025-3-25 10:23
Modelling Diffusion and Dispersion of Pollutants,h scales of atmospheric motion according to:.In spatial extension, the surface layer extends from the ground and up to a few hundred meters in the vertical. It is characterized by approximately constant fluxes of heat and momentum which can be determined by measurements near the surface.作者: 靦腆 時(shí)間: 2025-3-25 13:55
Inversion layers,ace within so-called atmospheric inversion layers, namely the layers characterized by the increase of the absolute temperature with height. In the course of the diurnal evolution of the atmospheric planetary boundary layer the two most typical examples of the sublayers with the inverse temperature gradient can be observed.作者: 轎車 時(shí)間: 2025-3-25 18:47
https://doi.org/10.1007/978-94-015-8547-7Climatology; Inversion; Large Eddy Simulation; Scale; fluid dynamics; fluid mechanics; air pollution and a作者: Kindle 時(shí)間: 2025-3-25 20:13 作者: CAND 時(shí)間: 2025-3-26 02:34
ERCOFTAC Serieshttp://image.papertrans.cn/d/image/279029.jpg作者: 叫喊 時(shí)間: 2025-3-26 04:46
https://doi.org/10.1007/978-3-658-16365-5ance to the distribution of pollutants, are relatively shallow (a few kilometres at most) and are significantly influenced by the nature of the underlying earth’s surface. This chapter is concerned with clarifying the term ‘meso-scale’ and presenting the basic fluid mechanics of meso-scale airflows,作者: Nonporous 時(shí)間: 2025-3-26 11:40 作者: 失望昨天 時(shí)間: 2025-3-26 16:32 作者: 豎琴 時(shí)間: 2025-3-26 19:26
https://doi.org/10.1007/978-3-658-20005-3djust from their values in the free-atmosphere to the boundary conditions at the earth’s surface. These boundary conditions are the no-slip condition for the velocity and for heat and humidity imposed surface fluxes. The theory of the atmospheric boundary layer should provide us with the vertical pr作者: 不連貫 時(shí)間: 2025-3-26 22:04 作者: FEAS 時(shí)間: 2025-3-27 03:41
Phil C. Langer,Angela Kühner,Panja Schwederace within so-called atmospheric inversion layers, namely the layers characterized by the increase of the absolute temperature with height. In the course of the diurnal evolution of the atmospheric planetary boundary layer the two most typical examples of the sublayers with the inverse temperature g作者: Oscillate 時(shí)間: 2025-3-27 09:06
Book 1995heric boundary layers andthe influence of inhomogeneous terrain on the advection and thevertical dispersion, and the method of large eddy simulation. 5:Statistical processes in turbulent dispersion, turbulent diffusion andchemical reactions in fluxes. 6: Theoretical modelling of diffusionand dispers作者: 使閉塞 時(shí)間: 2025-3-27 12:39
https://doi.org/10.1007/978-3-658-16365-5ximations that may be made in the momentum and continuity equations, identifying those of most importance to meso-scale airflows. The need for and procedures involved in specifying turbulence closure follows. Much of the analysis of meso-scale airflows now involves solution of the momentum and other作者: vascular 時(shí)間: 2025-3-27 16:08
Introduction to the fluid mechanics of meso-scale flow fields,ximations that may be made in the momentum and continuity equations, identifying those of most importance to meso-scale airflows. The need for and procedures involved in specifying turbulence closure follows. Much of the analysis of meso-scale airflows now involves solution of the momentum and other作者: GRACE 時(shí)間: 2025-3-27 18:10
Diffusion and Transport of Pollutants in Atmospheric Mesoscale Flow Fields作者: 有角 時(shí)間: 2025-3-28 01:10
1382-4309 mulation. 5:Statistical processes in turbulent dispersion, turbulent diffusion andchemical reactions in fluxes. 6: Theoretical modelling of diffusionand dispers978-90-481-4501-0978-94-015-8547-7Series ISSN 1382-4309 Series E-ISSN 2215-1826 作者: Substitution 時(shí)間: 2025-3-28 03:55 作者: HEW 時(shí)間: 2025-3-28 08:25 作者: Interdict 時(shí)間: 2025-3-28 12:53 作者: 過(guò)度 時(shí)間: 2025-3-28 15:53 作者: Schlemms-Canal 時(shí)間: 2025-3-28 20:25
