標(biāo)題: Titlebook: Buoyant Convection in Geophysical Flows; E. J. Plate,E. E. Fedorovich,J. C. Wyngaard Book 1998 Springer Science+Business Media Dordrecht 1 [打印本頁(yè)] 作者: FERN 時(shí)間: 2025-3-21 17:38
書目名稱Buoyant Convection in Geophysical Flows影響因子(影響力)
書目名稱Buoyant Convection in Geophysical Flows影響因子(影響力)學(xué)科排名
書目名稱Buoyant Convection in Geophysical Flows網(wǎng)絡(luò)公開(kāi)度
書目名稱Buoyant Convection in Geophysical Flows網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書目名稱Buoyant Convection in Geophysical Flows被引頻次
書目名稱Buoyant Convection in Geophysical Flows被引頻次學(xué)科排名
書目名稱Buoyant Convection in Geophysical Flows年度引用
書目名稱Buoyant Convection in Geophysical Flows年度引用學(xué)科排名
書目名稱Buoyant Convection in Geophysical Flows讀者反饋
書目名稱Buoyant Convection in Geophysical Flows讀者反饋學(xué)科排名
作者: 蚊帳 時(shí)間: 2025-3-22 00:17
Matrices with Real or Complex Entries,ated as internal boundary layers of radial geometry strongly affected by the buoyancy forces. Generally, convergence flows superimpose on mean wind. In calm weather they yield their own velocity shears characterised by the “minimum friction velocity”. As a result, turbulent mixing and heat/mass tran作者: GRACE 時(shí)間: 2025-3-22 00:25 作者: 單調(diào)性 時(shí)間: 2025-3-22 04:42
Theory and Application of Mixed Matrices,opriate information on the fluxes at the air-sea interface. Most coupled models with simplified fluxes do not represent the surface temperature well enough and water mass characteristics drift away from the initial state. Restoring conditions at the sea surface are needed to force the model back to 作者: 情感 時(shí)間: 2025-3-22 10:39 作者: embolus 時(shí)間: 2025-3-22 14:37
The Search for a Feasible Solutionumptions of the zero-order representation of the CBL vertical structure. The developed theory is generalized for the case of the CBL over an irregular terrain..The second model considered is the general-structure CBL bulk model, which incorporates a self-similar representation of the buoyancy profil作者: 搬運(yùn)工 時(shí)間: 2025-3-22 20:03 作者: 充氣女 時(shí)間: 2025-3-23 00:21
Matrices, Statistics and Big Dataenhanced surface evaporation upstream in the trade-wind region can be regarded as a fuel supply for this circulation. It is in this context that the presence of shallow cumuli, though small in individual size and non-precipitating, intensifies the large-scale circulation. Locally, the vertical trans作者: Trigger-Point 時(shí)間: 2025-3-23 05:16
Surface Frictional Processes and Non-Local Heat/Mass Transfer in the Shear-Free Convective Boundaryated as internal boundary layers of radial geometry strongly affected by the buoyancy forces. Generally, convergence flows superimpose on mean wind. In calm weather they yield their own velocity shears characterised by the “minimum friction velocity”. As a result, turbulent mixing and heat/mass tran作者: 抵制 時(shí)間: 2025-3-23 05:57
Convection in Viscous and Rotating Fluids from the Viewpoint of the Forced Flow Theory,the statement that the characteristic velocity of the flow is the applied force times the minimum time scale typical of the flow..Results of the application of the proposed principle are compared with the predictions of the similarity theory. Neither of the two enables dimensionless coefficients to 作者: OGLE 時(shí)間: 2025-3-23 10:59
Modeling the Oceanic Mixed-Layer and Effects of Deep Convection,opriate information on the fluxes at the air-sea interface. Most coupled models with simplified fluxes do not represent the surface temperature well enough and water mass characteristics drift away from the initial state. Restoring conditions at the sea surface are needed to force the model back to 作者: Intruder 時(shí)間: 2025-3-23 14:37
Observations of Clear and Cloud-Capped Convective Boundary Layers, and Techniques for Probing Them,lecting and absorbing solar radiation (globally they reflect about 20% of the total incoming radiation), and, if deep enough, by generating their own secondary circulations through the release of latent heat by condensation. In this way, clouds are a mechanism for releasing latent heat emitted from 作者: 亞當(dāng)心理陰影 時(shí)間: 2025-3-23 22:02
Bulk Models of the Atmospheric Convective Boundary Layer,umptions of the zero-order representation of the CBL vertical structure. The developed theory is generalized for the case of the CBL over an irregular terrain..The second model considered is the general-structure CBL bulk model, which incorporates a self-similar representation of the buoyancy profil作者: 浪費(fèi)物質(zhì) 時(shí)間: 2025-3-24 01:33 作者: 美學(xué) 時(shí)間: 2025-3-24 02:50 作者: 金哥占卜者 時(shí)間: 2025-3-24 06:46
Book 1998 andmicrophysics. New theoretical concepts and approaches have beenoutlined regarding scaling and parameterization of physical processesin buoyancy-driven geophysical flows. .The book summarizes interdisciplinary studies of buoyancy effects indifferent media (atmosphere and hydrosphere) over a wide 作者: Delude 時(shí)間: 2025-3-24 10:55 作者: 憂傷 時(shí)間: 2025-3-24 17:35
Experiment, Numerical Modeling, Numerical Simulation, and Their Roles in the Study of Convection,A casual observer of a turbulent flow, say a cigarette plume or the eddying motion downstream of a waterfall, can easily get the impression that turbulence behaves as it pleases locally in space and time. Any constraints on its behavior seem to come with a long leash.作者: 集合 時(shí)間: 2025-3-24 21:39 作者: Arbitrary 時(shí)間: 2025-3-25 02:59
Matrices with Real or Complex Entries,te “The scientific study of turbulent flow spans approximately one hundred years; during that time some of the greatest names in physics, mechanics, and engineering have at one time or another taken a crack at the problem. Progress in many directions has been made, indeed significant progress. Howev作者: 共和國(guó) 時(shí)間: 2025-3-25 04:28 作者: Psychogenic 時(shí)間: 2025-3-25 08:40
Matrices with Real or Complex Entries,dtl [49] theory of free convection, implying the concepts of (i) universal chaotic turbulence and (ii) local correspondence between turbulent fluxes and mean gradients. Accordingly the fluxes of heat and water vapour in the atmospheric surface layer are parameterized disregarding gross features of t作者: 柏樹(shù) 時(shí)間: 2025-3-25 14:19 作者: 存在主義 時(shí)間: 2025-3-25 16:28
Polynomial Matrix and Valuated Matroid,tic time scales. In this paper, a principle of the fastest response is proposed. It states that quadratic characteristics of the physical fields, .. variances and other second-order moments, can be estimated as the product of their generation rate and a minimum time scale inherent in the system cons作者: Obverse 時(shí)間: 2025-3-25 20:16 作者: senile-dementia 時(shí)間: 2025-3-26 03:57 作者: atopic 時(shí)間: 2025-3-26 06:49 作者: dysphagia 時(shí)間: 2025-3-26 08:35 作者: Conflagration 時(shí)間: 2025-3-26 13:32
The Search for a Feasible Solutionthe layer. Such parameterizations are constructed based on empirical knowledge about vertical distributions of meteorological variables in the CBL..Two main types of CBL bulk models are presented and discussed. The first model considered is the so-called zero-order jump model, which implies a vertic作者: llibretto 時(shí)間: 2025-3-26 17:57 作者: 撫育 時(shí)間: 2025-3-26 22:28 作者: lethal 時(shí)間: 2025-3-27 04:18
Powers of Nonnegative Matrices,thermally stratified wind tunnel of the Institute of Hydrology and Water Resources Planning (IHW), University of Karlsruhe. Design of the wind tunnel, and the technique employed for velocity and temperature measurements are described. The performed experiments reproduce convective conditions in the 作者: FLINT 時(shí)間: 2025-3-27 05:36
Powers of Nonnegative Matrices, and stable boundary layer. For a review of the meteorological characteristics of the three prototypes we refer to Nieuwstadt and Duynkerke [10]. Here we shall concentrate on the CBL. Convection or rather the term free convection is used to describe the process whereby turbulence is produced by buoy作者: Barrister 時(shí)間: 2025-3-27 11:32 作者: painkillers 時(shí)間: 2025-3-27 16:04
Matrices in Engineering Problemsn the large-scale subsiding motion is strong and the ocean surface is cold. This large-scale condition leads to a very moist, shallow planetary boundary layer (PBL). The lifting condensation level is below the top of the mixed layer, so an uniform layer of cloud can form in the upper part of the PBL作者: 拾落穗 時(shí)間: 2025-3-27 18:06 作者: 苦笑 時(shí)間: 2025-3-28 00:15
Nato Science Series C:http://image.papertrans.cn/b/image/191960.jpg作者: 不怕任性 時(shí)間: 2025-3-28 03:21 作者: 幼稚 時(shí)間: 2025-3-28 06:16
Eddy Dynamics and Kinematics of Convective Turbulence, these are related to the interactions of the turbulence with the rigid surfaces and other regions of fluid motion bounding the convective layer. The effects of weak cross winds and non-uniformity in surface conditions are also discussed.作者: Precursor 時(shí)間: 2025-3-28 11:21 作者: 綠州 時(shí)間: 2025-3-28 17:56 作者: 安撫 時(shí)間: 2025-3-28 22:41 作者: 舊式步槍 時(shí)間: 2025-3-29 02:04 作者: 花費(fèi) 時(shí)間: 2025-3-29 06:41 作者: 莎草 時(shí)間: 2025-3-29 10:54
https://doi.org/10.1007/978-94-011-5058-3Absorption; Cloud; Ocean; Scale; Weather forecasting; Wind; convection作者: Aspiration 時(shí)間: 2025-3-29 12:22
978-94-010-6125-4Springer Science+Business Media Dordrecht 1998作者: exacerbate 時(shí)間: 2025-3-29 17:39 作者: conscribe 時(shí)間: 2025-3-29 19:48
Matrices with Real or Complex Entries,te “The scientific study of turbulent flow spans approximately one hundred years; during that time some of the greatest names in physics, mechanics, and engineering have at one time or another taken a crack at the problem. Progress in many directions has been made, indeed significant progress. However, the ‘turbulence problem’ …remains. ”作者: 簡(jiǎn)略 時(shí)間: 2025-3-30 00:40 作者: 愉快嗎 時(shí)間: 2025-3-30 04:52
Matrices with Real or Complex Entries,e rate of convective transport defines a buoyancy velocity, which is used to parameterize surface heat, moisture, and momentum fluxes (drag). Vertical profiles of wind and potential temperature are found for the radix layer, the bottom fifth of the boundary layer, which work better than classical surface-layer similarity theories.作者: uncertain 時(shí)間: 2025-3-30 09:21
Mixed Systems, Upper and Lower Bounds dilution. This nonlocal mixing can be described by a transilient matrix, where each element indicates what fraction of air at a destination height comes from any source height. Parameterization of this matrix allows transilient turbulence theory to be used to forecast boundary-layer evolution.作者: 和平主義者 時(shí)間: 2025-3-30 13:23 作者: characteristic 時(shí)間: 2025-3-30 18:46 作者: Epidural-Space 時(shí)間: 2025-3-30 22:32 作者: 節(jié)約 時(shí)間: 2025-3-31 03:19 作者: oracle 時(shí)間: 2025-3-31 07:10 作者: sorbitol 時(shí)間: 2025-3-31 11:26 作者: outrage 時(shí)間: 2025-3-31 16:45
Parameterizations of the Convective Boundary Layer in Atmospheric Models,an ensemble-mean turbulence model. There exist many PBL parameterization schemes. Based on a survey Wyngaard and Moeng performed in 1990 (Taylor and Wyngaard [24]), we found these PBL schemes can be categorized into six generic types:作者: Halfhearted 時(shí)間: 2025-3-31 18:17 作者: 聰明 時(shí)間: 2025-3-31 23:53
Airborne Water Vapor Differential Absorption Lidar Studies of the Convective Boundary Layer,iance water vapor profiles using a set of empirically derived equations. Such measurements are of high climatological interest, since they enable to evaluate and monitor evaporation and biosphere—atmosphere exchange processes over land surfaces.作者: craving 時(shí)間: 2025-4-1 02:01
