作者: wall-stress 時(shí)間: 2025-3-21 21:56
ions.The main theme is understanding how turbulence effects .At a time when the polar regions are undergoing rapid and unprecedented change, understanding exchanges of momentum, heat and salt at the ice-ocean interface is critical for realistically predicting the future state of sea ice. By offering作者: 倫理學(xué) 時(shí)間: 2025-3-22 02:39 作者: cumber 時(shí)間: 2025-3-22 06:31 作者: 自愛 時(shí)間: 2025-3-22 09:34
Musikpublikum und Musikpublikumsforschung,ns between time-series covariances and ensemble averages of turbulent fluctuation products. Simplified forms of the turbulent kinetic energy and scalar variance equations are described, and related to spectral characteristics including a length scale proportional to the inverse wave number at the peak in the vertical velocity spectrum.作者: Nonflammable 時(shí)間: 2025-3-22 14:41
Turbulence Basics,ns between time-series covariances and ensemble averages of turbulent fluctuation products. Simplified forms of the turbulent kinetic energy and scalar variance equations are described, and related to spectral characteristics including a length scale proportional to the inverse wave number at the peak in the vertical velocity spectrum.作者: sundowning 時(shí)間: 2025-3-22 17:10 作者: 刪除 時(shí)間: 2025-3-22 22:54
http://image.papertrans.cn/a/image/151860.jpg作者: 寄生蟲 時(shí)間: 2025-3-23 05:11 作者: CHAR 時(shí)間: 2025-3-23 07:02
978-1-4419-2685-2Springer-Verlag New York 2008作者: 泄露 時(shí)間: 2025-3-23 10:52
https://doi.org/10.1007/978-3-662-67084-2binger of climate change. Central to this impact is a thin layer of sea ice that is predominantly seasonal, and at maximum extent (at the end of austral winter) covers roughly 8% of the world ocean area. Sea ice affects climate in several important ways. It effectively insulates the ocean from the c作者: 熟練 時(shí)間: 2025-3-23 17:23 作者: 遺忘 時(shí)間: 2025-3-23 18:17 作者: defibrillator 時(shí)間: 2025-3-23 22:55 作者: neoplasm 時(shí)間: 2025-3-24 03:40 作者: 星球的光亮度 時(shí)間: 2025-3-24 09:53 作者: BARGE 時(shí)間: 2025-3-24 11:34
https://doi.org/10.1007/978-3-8349-8383-1sely on techniques I learned while collaborating with George Mellor when we were both occupying visiting research chairs at the Naval Postgraduate School in Monterey, California. They were first used to model the IOBL with the Mellor-Yamada “l(fā)evel 2.” second-moment closure (Mellor and Yamada 1982; M作者: 相符 時(shí)間: 2025-3-24 15:03
Forum Produkt- und Produktionsmanagementin Chapter 7. The intent is to elucidate certain features of the response of the upper ocean to variations in forcing that require consideration of the time dependence of the physical conservation equations..First, we show that an interesting series of upper ocean measurements at the SHEBA site near作者: 易受刺激 時(shí)間: 2025-3-24 20:16
Vom Bergbau und Hüttenwesen bei den Altenies, along with their Reynolds fluxes including values at the immediate boundary. For the atmospheric surface layer, extensive research has been devoted to methods relating relatively simple measurements to fluxes. Central to this approach is characterizing surface roughness for momentum and scalar 作者: Aprope 時(shí)間: 2025-3-24 23:45 作者: hypnogram 時(shí)間: 2025-3-25 06:05
affect mixing in the Weddell Sea...The book’s content, developed from a series of lectures, may be appropriate additional material for upper-level undergraduates and first-year graduate students studying the g978-1-4419-2685-2978-0-387-78335-2作者: CUR 時(shí)間: 2025-3-25 10:22 作者: 大罵 時(shí)間: 2025-3-25 14:26 作者: Grating 時(shí)間: 2025-3-25 19:35 作者: Receive 時(shí)間: 2025-3-25 20:12 作者: Gobble 時(shí)間: 2025-3-26 00:15
A Numerical Model for the Ice/Ocean Boundary Layer,rd and Baumert 1995) models in that the length scales are based on a combination of measurements and similarity theory, rather than derived from separate TKE and master length scale conservation equations. A practical impact is that the LTC model eliminates the need to carry these equations in the s作者: AGATE 時(shí)間: 2025-3-26 05:36
LTC Modeling Examples,rgetic inertial motion of the ice and upper ocean. Inertial oscillation nearly always implies strong shear in the upper part of the pycnocline, and early models of mixed-layer evolution (e.g., Pollard et al. 1973; Niiler and Kraus 1977) related the rate of mixed-layer deepening (“entrainment velocit作者: 易改變 時(shí)間: 2025-3-26 11:17 作者: lambaste 時(shí)間: 2025-3-26 15:45
https://doi.org/10.1007/978-3-662-67084-2mosphereocean exchanges and how studies of turbulent exchange in the ice-ocean boundary layer have revealed much about how planetary boundary layers (where rotation is important) work in general. It briefly describes pertinent ice-station exercises, and lays out the framework for subsequent chapters作者: Gentry 時(shí)間: 2025-3-26 18:34
Patrick Glogner-Pilz,Patrick S. F?hlilarity theory for the IOBL stabilized by positive buoyancy flux at the surface (melting). The crucial parameters identified in the exercise, including important turbulence scales, then provide the rationale for development of the local turbulence closure model described in subsequent chapters.作者: Anterior 時(shí)間: 2025-3-26 22:43
Musikpublikum und Musikpublikumsforschung,r suggested by Busch and Panofsky (1968), and compared with calculations from one of the first attempts at large eddy simulation for the atmospheric boundary layer (Deardorff 1972). This was far from conclusive; however, later measurements tended to confirm that basic approach.作者: VAN 時(shí)間: 2025-3-27 04:31 作者: sultry 時(shí)間: 2025-3-27 08:19
https://doi.org/10.1007/978-3-8349-8383-1rd and Baumert 1995) models in that the length scales are based on a combination of measurements and similarity theory, rather than derived from separate TKE and master length scale conservation equations. A practical impact is that the LTC model eliminates the need to carry these equations in the s作者: 使苦惱 時(shí)間: 2025-3-27 11:10
Forum Produkt- und Produktionsmanagementrgetic inertial motion of the ice and upper ocean. Inertial oscillation nearly always implies strong shear in the upper part of the pycnocline, and early models of mixed-layer evolution (e.g., Pollard et al. 1973; Niiler and Kraus 1977) related the rate of mixed-layer deepening (“entrainment velocit作者: 小教堂 時(shí)間: 2025-3-27 16:37
Vom Bergbau und Hüttenwesen bei den Altens is much less straightforward for a variety of reasons. First, in contrast to the upper sea-ice surface, variation in the underice morphology often occupies a significant fraction of the entire boundary layer. If the IOBL scales with about 1/30 of the atmospheric boundary layer, a pressure ridge wi作者: terazosin 時(shí)間: 2025-3-27 18:41 作者: cluster 時(shí)間: 2025-3-27 23:08
Basic Physical Concepts, elsewhere; and second, the combination of cold temperature and salt injection inherent in the freezing process produces very dense water, so that the polar and subpolar regions provide the main conduit by which the abyssal ocean communicates with the remainder of the climate system. A cursory revie作者: Calculus 時(shí)間: 2025-3-28 03:41
Turbulence Basics,mass balance at the ice-ocean interface dictates ice growth or ablation, the turbulence will also transport heat and salt. This chapter introduces basic features of turbulence in natural flows, by describing general characteristics of turbulence; how it is measured in the somewhat unique under-ice e作者: 分離 時(shí)間: 2025-3-28 09:20 作者: PACT 時(shí)間: 2025-3-28 13:45
Turbulence Scales for the Ice/Ocean Boundary Layer,er and the underlying ocean. This chapter presents several examples from field observations that shed light on the impact of both stress and buoyancy on turbulence in the IOBL, and use them to develop a heuristic approach to specifying the mixing length. A key in this development is the apparent con作者: acclimate 時(shí)間: 2025-3-28 16:17
The Ice/Ocean Interface, law of thermodynamics. There are essentially only three important factors in the enthalpy balance: (i) upward (or downward) heat conduction within the ice column; (ii) heat flux from or to the underlying ocean; and (iii) latent heat associated with the phase change as ice grows or melts. However, s作者: 扔掉掐死你 時(shí)間: 2025-3-28 19:48
A Numerical Model for the Ice/Ocean Boundary Layer,sely on techniques I learned while collaborating with George Mellor when we were both occupying visiting research chairs at the Naval Postgraduate School in Monterey, California. They were first used to model the IOBL with the Mellor-Yamada “l(fā)evel 2.” second-moment closure (Mellor and Yamada 1982; M作者: 肥料 時(shí)間: 2025-3-29 00:31
LTC Modeling Examples,in Chapter 7. The intent is to elucidate certain features of the response of the upper ocean to variations in forcing that require consideration of the time dependence of the physical conservation equations..First, we show that an interesting series of upper ocean measurements at the SHEBA site near作者: 敘述 時(shí)間: 2025-3-29 06:24 作者: Antioxidant 時(shí)間: 2025-3-29 08:05
History of Mechanism and Machine ScienceA slit lamp is a combination of a light source and a microscope.?The slit lamp is currently the most important instrument one needs for a proper clinical examination of the eye. If we understand this biomicroscope?and its working, one will be able to put it to optimal use and improvise along the way for our clinical examination.
