作者: 人類學(xué)家 時(shí)間: 2025-3-21 21:52
978-90-481-4740-3Springer Science+Business Media Dordrecht 1996作者: Scintillations 時(shí)間: 2025-3-22 04:23
http://image.papertrans.cn/b/image/190051.jpg作者: Nmda-Receptor 時(shí)間: 2025-3-22 04:36
Ludovico Agostini’s ‘Imaginary Republic‘the Atmospheric Environment Service (of Canada), the International Institute for Applied Systems Analysis in Austria and with the Institute of Environmental Studies at the University of Toronto, and as editor of this journal.作者: 連詞 時(shí)間: 2025-3-22 12:36 作者: dysphagia 時(shí)間: 2025-3-22 14:14
https://doi.org/10.1007/978-3-030-97016-1x budgets, surface-exchange relations, and the universal functions of Monin—Obukhov similarity within the “constant-flux” layer. More recently, the growth in supercomputers and computational fluid dynamics has stimulated micrometeorological applications of large-eddy simulation (LES). LES uses a dif作者: 翻布尋找 時(shí)間: 2025-3-22 17:49
https://doi.org/10.1007/978-3-031-66123-5s surfaces. This task is approached by tying together concepts from a diverse range of recent studies on subgrid parameterization, the roughness sublayer, the roll of large “inactive” boundary-layer eddies, internal boundary-layer growth, the equilibrium sublayer, footprint theory and the blending h作者: RUPT 時(shí)間: 2025-3-22 22:10
https://doi.org/10.1007/978-3-031-66123-5s of evaporation from the sea and has investigated the role of droplets in the transfer of water to the atmosphere. Predictions of a rapid rise in the evaporation coefficient at wind speeds above 15 m s. have not been substantiated. Wind stress measurements showed a relationship with wave age. New m作者: detach 時(shí)間: 2025-3-23 03:43 作者: 增減字母法 時(shí)間: 2025-3-23 05:54
Notizenaus den Ietzten Lebensjahren,e of the Planetary Boundary Layer (PBL) for the development and the substructures of two different types of cold fronts. The effects of turbulent friction, large-scale (geostrophic) forcing and the diurnal variation of the terms of the surface energy balance (SEB) equation on the frontal development作者: 描述 時(shí)間: 2025-3-23 12:12 作者: Generosity 時(shí)間: 2025-3-23 16:55 作者: 燒烤 時(shí)間: 2025-3-23 20:25
Notizenaus den Ietzten Lebensjahren,.32 to 0.65 have been reported. Most of the data are, however, found in a rather narrow range between 0.39 and 0.41. Plotting all available atmospheric data against the so-called roughness Reynolds number, Reo = ..../. or against the surface Rossby number, Ro. = ./... gives no clear indication of sy作者: PHON 時(shí)間: 2025-3-23 22:17
https://doi.org/10.1007/978-94-017-0489-2ling of the coupled system of ocean and atmosphere. Knowledge of air- sea fluxes has grown, based on Monin-Obukhov similarity theory for surface boundary layers and on direct and indirect techniques of measuring the fluxes. This has been the basis for providing boundary conditions needed to couple a作者: GOAD 時(shí)間: 2025-3-24 03:19 作者: malign 時(shí)間: 2025-3-24 07:50 作者: motor-unit 時(shí)間: 2025-3-24 12:28
https://doi.org/10.1007/978-3-642-46886-5f instabilities associated with the characteristic strong inflection in the mean velocity profile. Mixing-layer turbulence, formed around the inflectional mean velocity profile which develops between two coflowing streams of different velocities, differs in several ways from turbulence in a surface 作者: lattice 時(shí)間: 2025-3-24 17:08 作者: Celiac-Plexus 時(shí)間: 2025-3-24 21:03
A Professor with Industrial Experience, the ease with which the vertical flux contribution from surface area sources can be calculated. The flux contribution at an observation point . is found by summing the ratio of the particle vertical velocity at . to the “touchdown” velocity for particles which impact the ground within the source bo作者: Cougar 時(shí)間: 2025-3-25 02:44
Ludwig Prandtl Gesammelte Abhandlungenon the analytical model of the boundary-layer height proposed by Gryning and Batchvarova (1990) and Batchvarova and Gryning (1991). The model accounts for the temperature jump and the mean vertical air motion at the top of the internal boundary-layer. Four cases from experiments in Nanticoke and Van作者: 著名 時(shí)間: 2025-3-25 06:03
Searching for Italian Renaissance UtopiasAt Cabauw, The Netherlands, a 213 m high mast specifically built for meteorological research has been operational since 1973. Its site, construction, instrumentation and observation programs are reviewed. Regarding analysis of the boundary layer at Cabauw, the following subjects are discussed:作者: 功多汁水 時(shí)間: 2025-3-25 08:34 作者: 動機(jī) 時(shí)間: 2025-3-25 12:26 作者: Coronation 時(shí)間: 2025-3-25 17:15 作者: 豐滿有漂亮 時(shí)間: 2025-3-25 23:11 作者: 柔聲地說 時(shí)間: 2025-3-26 02:54
,R. E. (Ted) Munn — Founding Editor; A Mini-Biography,the Atmospheric Environment Service (of Canada), the International Institute for Applied Systems Analysis in Austria and with the Institute of Environmental Studies at the University of Toronto, and as editor of this journal.作者: 移植 時(shí)間: 2025-3-26 07:04
Review of Lagrangian Stochastic Models for Trajectories in the Turbulent Atmosphere,y their application to calculate dispersion in the principal types of atmospheric turbulence (stratified, vertically-inhomogeneous, Gaussian or non-Gaussian turbulence in the surface layer and above), and show that they are especially suitable for some problems (e.g., quantifying ground emissions).作者: 偏狂癥 時(shí)間: 2025-3-26 08:37
The Footprint for Flux Measurements, from Backward Lagrangian Stochastic Models, the ease with which the vertical flux contribution from surface area sources can be calculated. The flux contribution at an observation point . is found by summing the ratio of the particle vertical velocity at . to the “touchdown” velocity for particles which impact the ground within the source boundary.作者: tariff 時(shí)間: 2025-3-26 15:00 作者: 灰姑娘 時(shí)間: 2025-3-26 20:31
https://doi.org/10.1007/978-3-642-46886-5then 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.作者: 影響帶來 時(shí)間: 2025-3-26 21:56
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.作者: assent 時(shí)間: 2025-3-27 03:20 作者: 轉(zhuǎn)換 時(shí)間: 2025-3-27 08:42
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.作者: 開頭 時(shí)間: 2025-3-27 12:44 作者: Bouquet 時(shí)間: 2025-3-27 13:44
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作者: GULP 時(shí)間: 2025-3-27 18:42 作者: BYRE 時(shí)間: 2025-3-27 22:34 作者: 適宜 時(shí)間: 2025-3-28 04:00
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.作者: LATER 時(shí)間: 2025-3-28 06:16
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.作者: 臆斷 時(shí)間: 2025-3-28 10:52
,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.作者: Gustatory 時(shí)間: 2025-3-28 17:01
The Impact of the Hexos Programme, 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.作者: mercenary 時(shí)間: 2025-3-28 20:47 作者: 萬神殿 時(shí)間: 2025-3-28 23:02 作者: Ventilator 時(shí)間: 2025-3-29 03:58 作者: PAEAN 時(shí)間: 2025-3-29 11:08
Book Review,I painfully recall mistaking . (blossom) for the plural of . (sap of a tree) and completely misinterpreting the rest of the paragraph. I’m happy to see that these few lines in the original German edition remain in the 1995 English version.作者: Prognosis 時(shí)間: 2025-3-29 14:11 作者: 自作多情 時(shí)間: 2025-3-29 18:37 作者: fledged 時(shí)間: 2025-3-29 22:07
Experimental Micrometeorology in an Era of Turbulence Simulation,ong coupling between experimental and computational work in micrometeorology. A challenge for experimentalists today is to address problems posed in the language of the resolvable, subgrid-scale decomposition. We illustrate by discussing measurement strategies for resolvable-scale turbulence fields and for local surface-exchange coefficients.作者: 誰在削木頭 時(shí)間: 2025-3-30 03:55 作者: 大洪水 時(shí)間: 2025-3-30 04:13 作者: 消息靈通 時(shí)間: 2025-3-30 08:39
Experimental Micrometeorology in an Era of Turbulence Simulation,x budgets, surface-exchange relations, and the universal functions of Monin—Obukhov similarity within the “constant-flux” layer. More recently, the growth in supercomputers and computational fluid dynamics has stimulated micrometeorological applications of large-eddy simulation (LES). LES uses a dif作者: 整潔 時(shí)間: 2025-3-30 15:37 作者: 產(chǎn)生 時(shí)間: 2025-3-30 18:58 作者: Deference 時(shí)間: 2025-3-31 00:43 作者: 大吃大喝 時(shí)間: 2025-3-31 04:40
Frontal Substructures Within the Planetary Boundary Layer,e of the Planetary Boundary Layer (PBL) for the development and the substructures of two different types of cold fronts. The effects of turbulent friction, large-scale (geostrophic) forcing and the diurnal variation of the terms of the surface energy balance (SEB) equation on the frontal development作者: CLAMP 時(shí)間: 2025-3-31 08:09
Review of Lagrangian Stochastic Models for Trajectories in the Turbulent Atmosphere,y their application to calculate dispersion in the principal types of atmospheric turbulence (stratified, vertically-inhomogeneous, Gaussian or non-Gaussian turbulence in the surface layer and above), and show that they are especially suitable for some problems (e.g., quantifying ground emissions).作者: 洞察力 時(shí)間: 2025-3-31 11:12 作者: figment 時(shí)間: 2025-3-31 14:01
Review of Some Basic Characteristics of the Atmospheric Surface Layer,.32 to 0.65 have been reported. Most of the data are, however, found in a rather narrow range between 0.39 and 0.41. Plotting all available atmospheric data against the so-called roughness Reynolds number, Reo = ..../. or against the surface Rossby number, Ro. = ./... gives no clear indication of sy作者: 商談 時(shí)間: 2025-3-31 20:36 作者: malign 時(shí)間: 2025-3-31 23:33 作者: AGOG 時(shí)間: 2025-4-1 02:43
Ground-Based Remote Sensing of the Atmospheric Boundary Layer: 25 Years of Progress,w begins with a brief comparison of the state of remote sensors in boundary-layer research 25 years ago with its present-day status. Next, a summary of the current capabilities of remote sensors for boundary-layer studies demonstrates that for boundary-layer depth and for profiles of many mean quant作者: 咽下 時(shí)間: 2025-4-1 06:57 作者: Monocle 時(shí)間: 2025-4-1 11:51 作者: 審問 時(shí)間: 2025-4-1 17:16
The Footprint for Flux Measurements, from Backward Lagrangian Stochastic Models, the ease with which the vertical flux contribution from surface area sources can be calculated. The flux contribution at an observation point . is found by summing the ratio of the particle vertical velocity at . to the “touchdown” velocity for particles which impact the ground within the source bo作者: 敬禮 時(shí)間: 2025-4-1 18:42
A Model for the Height of the Internal Boundary Layer over an Area with an Irregular Coastline,on the analytical model of the boundary-layer height proposed by Gryning and Batchvarova (1990) and Batchvarova and Gryning (1991). The model accounts for the temperature jump and the mean vertical air motion at the top of the internal boundary-layer. Four cases from experiments in Nanticoke and Van作者: 水土 時(shí)間: 2025-4-2 01:56
