標(biāo)題: Titlebook: Boundary Layer Studies and Applications; A Special Issue of B R. E. Munn Book 1989 Kluwer Academic Publishers 1989 Meteorology.Scale.Wind s [打印本頁] 作者: Stenosis 時(shí)間: 2025-3-21 19:54
書目名稱Boundary Layer Studies and Applications影響因子(影響力)
書目名稱Boundary Layer Studies and Applications影響因子(影響力)學(xué)科排名
書目名稱Boundary Layer Studies and Applications網(wǎng)絡(luò)公開度
書目名稱Boundary Layer Studies and Applications網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Boundary Layer Studies and Applications被引頻次
書目名稱Boundary Layer Studies and Applications被引頻次學(xué)科排名
書目名稱Boundary Layer Studies and Applications年度引用
書目名稱Boundary Layer Studies and Applications年度引用學(xué)科排名
書目名稱Boundary Layer Studies and Applications讀者反饋
書目名稱Boundary Layer Studies and Applications讀者反饋學(xué)科排名
作者: 秘傳 時(shí)間: 2025-3-21 20:20
An Evaluation of Aircraft Flux Measurements of CO2, Water Vapor and Sensible Heat,x. Cospectral analyses showed no significant high frequency losses for the data from flight levels of 25 and 50 m, but an underestimation of approximately 10% resulted at 10 m. Flight direction with respect to wind direction was relatively unimportant at 10 and 25 m but some effects were observed at作者: 肌肉 時(shí)間: 2025-3-22 01:59
Spectra of Surface Wind Speed and Air Temperature over the Ocean in the Mesoscale Frequency Range in buoys. Significant mesoscale peaks in spectra appear in relatively strong winds and unstable or near-neutral atmospheric conditions, and none in stable atmospheric conditions. A criterion of wind speed and atmospheric stability is found for the mesoscale spectral peak appearance.作者: Outshine 時(shí)間: 2025-3-22 07:42
The Spectral Velocity Tensor for Homogeneous Boundary-Layer Turbulence,n the transition domain from the inertial subrange towards lower wave numbers. When the three sets of parameters are the same, the three spectra correspond to isotropic turbulence and they are all interrelated and related to the energy spectrum. We show how it is possible to obtain these spectral fo作者: Abutment 時(shí)間: 2025-3-22 09:05
Spatial Correlation Functions of Surface-Layer Atmospheric Turbulence in Neutral Stratification,turbulence. In Section 3 it is shown that the correlation equations of Section 2 agree satisfactorily with some recent measurements of the longitudinal correlation functions in the range of distances from 3 m to 100 m. Some measurements of the lateral correlation functions of atmospheric turbulence 作者: 奴才 時(shí)間: 2025-3-22 16:14 作者: 烤架 時(shí)間: 2025-3-22 17:14 作者: 弄皺 時(shí)間: 2025-3-23 01:03 作者: motor-unit 時(shí)間: 2025-3-23 01:31 作者: electrolyte 時(shí)間: 2025-3-23 05:37 作者: Arresting 時(shí)間: 2025-3-23 12:40
https://doi.org/10.1007/978-3-642-84857-5turbulence. In Section 3 it is shown that the correlation equations of Section 2 agree satisfactorily with some recent measurements of the longitudinal correlation functions in the range of distances from 3 m to 100 m. Some measurements of the lateral correlation functions of atmospheric turbulence 作者: 颶風(fēng) 時(shí)間: 2025-3-23 13:54
Low-Dimensional Functional Materialslation results in less bias than a constant one. For the ship synoptic data available via GTS for the North Atlantic Ocean, spatial resolution, as expressed by an equivalent filter half-width, is 220 km, considerably improved compared to typical data assimilation schemes used in numerical forecast m作者: Increment 時(shí)間: 2025-3-23 20:45 作者: oncologist 時(shí)間: 2025-3-23 23:56
https://doi.org/10.1007/978-94-007-6618-1rease at high wind speeds, but no direct observations of this are found. Recently it has become possible to estimate water vapor flux in tropical regions from satellite data, opening the possiblity of studying large-scale evaporative events as a function of both time and space.作者: 內(nèi)部 時(shí)間: 2025-3-24 05:47 作者: 小畫像 時(shí)間: 2025-3-24 06:45 作者: 手術(shù)刀 時(shí)間: 2025-3-24 11:35
Water Vapor Flux at the Sea Surface,rease at high wind speeds, but no direct observations of this are found. Recently it has become possible to estimate water vapor flux in tropical regions from satellite data, opening the possiblity of studying large-scale evaporative events as a function of both time and space.作者: fatuity 時(shí)間: 2025-3-24 18:32
Velocity and Temperature Spectra and Cospectra in an Unstable Suburban Atmosphere,lux cospectra are in good agreement with reference data from smoother surfaces. Recommendations are made concerning site requirements, height of measurement and averaging times for the study of turbulence and turbulent fluxes over suburban terrain.作者: anesthesia 時(shí)間: 2025-3-24 22:00
Springer Series in Solid-State Sciencesatmospheric data summarized by Jackson (1976) as well as neutral-stratification data presented by Peterson .. (1979) and new data measured at Cherrywood, Ontario. It is found that the Panofsky-Dutton formulation gives the least root-mean-square (RMS) absolute errors for atmospheric applications.作者: Cantankerous 時(shí)間: 2025-3-25 01:44
,Internal Boundary-Layer Height Formulae — A Comparison with Atmospheric Data,atmospheric data summarized by Jackson (1976) as well as neutral-stratification data presented by Peterson .. (1979) and new data measured at Cherrywood, Ontario. It is found that the Panofsky-Dutton formulation gives the least root-mean-square (RMS) absolute errors for atmospheric applications.作者: Migratory 時(shí)間: 2025-3-25 05:44
F. Creuzet,G. Creuzet,B. Hamzic,D. Jéromece, small-scale turbulence and vertical fluxes seem to be concentrated. Zones of horizontal divergence appear to be associated with ejection of cold air from the underlying surface inversion while the convergent zones might be due to random “collisions” between horizontal modes.作者: Vasoconstrictor 時(shí)間: 2025-3-25 09:39 作者: 包裹 時(shí)間: 2025-3-25 12:17
Coherent Structures in the Very Stable Atmospheric Boundary Layer,ce, small-scale turbulence and vertical fluxes seem to be concentrated. Zones of horizontal divergence appear to be associated with ejection of cold air from the underlying surface inversion while the convergent zones might be due to random “collisions” between horizontal modes.作者: 特別容易碎 時(shí)間: 2025-3-25 17:16
Shapes of Annual Frequency Distributions of Wind Speed Observed on High Meteorological Masts,tribution shape from surface data is possible in the surface layer. In the upper PBL, however, such estimation is not very feasible, because no simple methods are available to estimate the reversal height from routine surface observations.作者: 噴油井 時(shí)間: 2025-3-26 00:03
https://doi.org/10.1007/978-1-4899-7031-2strophic wind show the development of a maximum of .. at about three quarters of the NBL. From the comparison with the models, we conclude that the observed profiles are most satisfactorily described by the model of Duynkerke and Driedonks.作者: insolence 時(shí)間: 2025-3-26 00:41
Huguette Launois,Halina Niedobaov constant in the inertial subrange is estimated from a set of averaged spectra. Cross-spectra indicate little relation between concentration and wind fluctuations. However, most of the correlation that exists is due to periods larger than about 10 or 20 s.作者: Amplify 時(shí)間: 2025-3-26 05:29
https://doi.org/10.1007/978-94-009-0447-7 a few to 20 min. This additional energy may be ascribed to gravity waves..The models cannot be applied in cases with trends in the data. The model tends to underestimate the dependence of variances on sampling time in cases when systems, such as longitudinal vortices or gravity waves exist.作者: 遣返回國 時(shí)間: 2025-3-26 12:10 作者: 口訣 時(shí)間: 2025-3-26 13:41 作者: 貪婪的人 時(shí)間: 2025-3-26 20:52
Dependence of Velocity Variance on Sampling Time, a few to 20 min. This additional energy may be ascribed to gravity waves..The models cannot be applied in cases with trends in the data. The model tends to underestimate the dependence of variances on sampling time in cases when systems, such as longitudinal vortices or gravity waves exist.作者: facetious 時(shí)間: 2025-3-26 23:03 作者: 庇護(hù) 時(shí)間: 2025-3-27 03:42
F. Creuzet,G. Creuzet,B. Hamzic,D. Jéromeg at the top of a strongly stratified nocturnal inversion layer as observed by fast response aircraft data. The spatial variation of the coefficients of the principal components identify regular coherent structures with mainly horizontal motions. Conditional sampling is formulated in terms of this s作者: ATOPY 時(shí)間: 2025-3-27 07:18
Low-Dimensional Cooperative Phenomenaements have recently been undertaken to attempt to widen the scope of applicability of such measurements. However, because of the intermittency of turbulent transfer, flux measurements must be averaged over long periods of time or long distances to give reproducible results. This requirement makes i作者: 使虛弱 時(shí)間: 2025-3-27 13:15
Huguette Launois,Halina Niedobapeed and air temperature over the ocean in the mesoscale frequency range were studied. The averaged composite spectrum of wind speed for the whole period shows the existence of a spectral gap in the frequency range from 10. to 5 × 10. Hz. However, significant peaks in this range are often seen in pa作者: ALERT 時(shí)間: 2025-3-27 17:27 作者: 鴿子 時(shí)間: 2025-3-27 19:16
https://doi.org/10.1007/978-1-4899-7031-2ls described by Nieuwstadt (1984, 1985) and Sorbjan (1986) and the numerical model of Duynkerke and Driedonks (1987). These theoretical profiles are compared with observed profiles from the meteorological mast at Cabauw, The Netherlands. From the observations, it is found that .. is large in the sur作者: BABY 時(shí)間: 2025-3-27 22:02
Huguette Launois,Halina Niedobaese experiments generally exhibit an inertial subrange at high frequencies with a slope of ?5/3 and indicate peak energy at a time period of about 50 to 100s. These periods of peak energy are a factor of two to five less than those for the peak of the wind speed fluctuation (.’ or .’) spectra. A gen作者: 作繭自縛 時(shí)間: 2025-3-28 03:13
Exciton Mechanism of Superconductivity,tion of the spectral tensor Φ.(.) for isotropic turbulence and we show how in the limit of isotropy, Φ.(.) becomes equal to Φ.(.). Whereas Φ.(.) is determined entirely by one scalar function of . = |.|, namely the energy spectrum, we need three independent scalar functions of . to specify Φ.(.). We 作者: Somber 時(shí)間: 2025-3-28 08:50 作者: FIS 時(shí)間: 2025-3-28 13:09 作者: 強(qiáng)制令 時(shí)間: 2025-3-28 14:37
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作者: flaunt 時(shí)間: 2025-3-28 19:02
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作者: 隼鷹 時(shí)間: 2025-3-29 02:45 作者: ALTER 時(shí)間: 2025-3-29 05:01 作者: irreparable 時(shí)間: 2025-3-29 09:29 作者: OPINE 時(shí)間: 2025-3-29 13:38
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作者: Debate 時(shí)間: 2025-3-29 16:02
https://doi.org/10.1007/978-94-009-0975-5Meteorology; Scale; Wind speed; temperature; wind作者: 機(jī)構(gòu) 時(shí)間: 2025-3-29 21:08 作者: Coterminous 時(shí)間: 2025-3-30 01:47
Overview: 978-94-010-6928-1978-94-009-0975-5作者: Androgen 時(shí)間: 2025-3-30 06:42
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.作者: 好色 時(shí)間: 2025-3-30 11:53 作者: 放縱 時(shí)間: 2025-3-30 13:32 作者: lavish 時(shí)間: 2025-3-30 19:13
,Hans Panofsky, 1917–1988,The editor of ., R. E. Munn, asked me to write a dedication for a special memorial volume for Hans A. Panofsky. Having known Hans and his beloved wife and companion Nancy for nearly 25 years, having fallen victim to their charm and joy of life, and having witnessed first hand Hans’ constructive influence on our discipline, I could not but agree.作者: Synapse 時(shí)間: 2025-3-30 21:21 作者: vitreous-humor 時(shí)間: 2025-3-31 01:59
http://image.papertrans.cn/b/image/190022.jpg作者: 混合 時(shí)間: 2025-3-31 06:52
Wave Drag in the Planetary Boundary Layer Over Complex Terrain,eynolds 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.作者: 暴發(fā)戶 時(shí)間: 2025-3-31 12:40
The Structure of the Stably Stratified Internal Boundary Layer in Offshore Flow over the Sea,er (IBL) over the sea formed by warm air advection from land to sea. The potential temperature and humidity fields reveal the vertical extent of the IBL, for fetches out to several hundred of kilometres, geostrophic winds of 20–25 m s., and potential temperature differences between undisturbed conti作者: Ondines-curse 時(shí)間: 2025-3-31 15:51
