作者: 捕鯨魚(yú)叉 時(shí)間: 2025-3-21 22:54
https://doi.org/10.1007/978-3-642-23450-7Environmental Physics; Geophysical Fluid Dynamics; Physical Oceanography作者: 接合 時(shí)間: 2025-3-22 04:09 作者: 咽下 時(shí)間: 2025-3-22 06:57 作者: outer-ear 時(shí)間: 2025-3-22 12:40 作者: Indent 時(shí)間: 2025-3-22 15:02
Gravity Wavesg to mixing processes in the ocean interior, especially to diapycnal mixing. Surface gravity waves are effective in the exchange of momentum, heat, water, and gases between the ocean and the atmosphere, in addition to their practical significance for shipping.作者: 感激小女 時(shí)間: 2025-3-22 17:02
PreliminariesIn this chapter some aspects of the kinematical description of oceanic flows are discussed. Furthermore, the equilibrium thermodynamics of seawater is reviewed. The results are prerequisites for the derivation of conservation laws in Chapter 2.作者: galley 時(shí)間: 2025-3-23 00:57
Book 2012d developments of fluid mechanics and theoretical oceanography. The last part covers the theory of the global wind-driven circulation in homogeneous and stratified regimes, the circulation and overturning in the Southern Ocean, and the global meridional overturning and thermohaline-driven circulatio作者: 使虛弱 時(shí)間: 2025-3-23 01:21 作者: Stress-Fracture 時(shí)間: 2025-3-23 09:03 作者: Condense 時(shí)間: 2025-3-23 11:36
Dirk Olbers,Jürgen Willebrand,Carsten Edenntlicher Bedeutung sind. Dies gilt namentlich für das Handels- und Gesellschaftsrecht, um handelsrechtliche Besonderheiten im Gesch?ftsverkehr und die rechtliche Struktur von Gesellschaften erkennen zu k?nnen.Bei allen Themenfeldern wird die Fragestellung stets aus Sicht des Unternehmers beleuchtet.作者: FLEET 時(shí)間: 2025-3-23 15:54 作者: 權(quán)宜之計(jì) 時(shí)間: 2025-3-23 18:11
Dirk Olbers,Jürgen Willebrand,Carsten Eden Ver?nderung der Leistung ist nur inRichtung geringeren Energieumsatzes m?glich. Somit wird das Netz nicht nur durchSchwankungen auf der Energieabnehmerseite, sondern bei unkoordinierter Speisungaus Windkraftanlagen auch durch die Witterung bedingt in der Energiezufuhr beeinflusst.作者: 鑲嵌細(xì)工 時(shí)間: 2025-3-24 01:18
Dirk Olbers,Jürgen Willebrand,Carsten Eden Ver?nderung der Leistung ist nur inRichtung geringeren Energieumsatzes m?glich. Somit wird das Netz nicht nur durchSchwankungen auf der Energieabnehmerseite, sondern bei unkoordinierter Speisungaus Windkraftanlagen auch durch die Witterung bedingt in der Energiezufuhr beeinflusst.作者: OWL 時(shí)間: 2025-3-24 04:21 作者: Epidural-Space 時(shí)間: 2025-3-24 08:35
beizuziehenden Rechtsanw?lten ein sorgf?ltig aufbereitetes Problem zur L?sung vorzulegen. Solche Grundlagen im Vertragsrecht sind unumg?nglich, um am Wirtschaftsleben erfolgreich teilnehmen zu k?nnen.Der Aufbau des Lehrbuches folgt der gesetzlichen Systematik. Zun?chst wird der Allgemeine Teil des 作者: apiary 時(shí)間: 2025-3-24 11:58 作者: BIDE 時(shí)間: 2025-3-24 16:21
Dirk Olbers,Jürgen Willebrand,Carsten Eden beizuziehenden Rechtsanw?lten ein sorgf?ltig aufbereitetes Problem zur L?sung vorzulegen. Solche Grundlagen im Vertragsrecht sind unumg?nglich, um am Wirtschaftsleben erfolgreich teilnehmen zu k?nnen.Der Aufbau des Lehrbuches folgt der gesetzlichen Systematik. Zun?chst wird der Allgemeine Teil des 作者: 大門在匯總 時(shí)間: 2025-3-24 21:49 作者: backdrop 時(shí)間: 2025-3-25 01:37 作者: Expostulate 時(shí)間: 2025-3-25 06:36 作者: collagen 時(shí)間: 2025-3-25 08:26 作者: Emasculate 時(shí)間: 2025-3-25 15:17 作者: 地殼 時(shí)間: 2025-3-25 19:16 作者: 秘傳 時(shí)間: 2025-3-25 22:02
Geostrophic and Quasi-Geostrophic Motionsed by a small Rossby number. Geostrophic balance is assumed to dominate for lateral scales comparable to the Rossby radius – leading to the quasi-geostrophic approximation – or on scales comparable to Earth’s radius – the planetary geostrophic approximation. The latter set of equations can be reform作者: 名詞 時(shí)間: 2025-3-26 01:40 作者: 使困惑 時(shí)間: 2025-3-26 05:13
Gravity Wavesg to mixing processes in the ocean interior, especially to diapycnal mixing. Surface gravity waves are effective in the exchange of momentum, heat, water, and gases between the ocean and the atmosphere, in addition to their practical significance for shipping.作者: Sleep-Paralysis 時(shí)間: 2025-3-26 10:44
Long Wavesenerally called long waves) are of particular importance in the ocean. We have already encountered the hydrostatic limit for gravity waves in Sections 7.4.1 and 7.5. In addition to long gravity waves, planetary and topographic waves are in hydrostatic balance and hence also are long waves. Near the 作者: 熱心助人 時(shí)間: 2025-3-26 15:04
Lagrangian Theory of Ocean Wavesfor incompressible flow, for isentropic compressible flow and for a rotating stratified fluid system. Some of the wave equations, derived and analyzed in the previous chapters, may be transferred into this Lagrangian framework, including Rossby waves and gravity waves. The present chapter is devoted作者: Pantry 時(shí)間: 2025-3-26 19:21 作者: tackle 時(shí)間: 2025-3-26 22:18 作者: 評(píng)論性 時(shí)間: 2025-3-27 03:23
Geostrophic Turbulencebiquitous and important for many aspects of the large-scale ocean circulation and often are referred to as mesoscale ocean eddies. As discussed in Section 5.1, motions on these scales are strongly constrained by rotation and stratification and have a very small aspect ratio and hence are nearly two-作者: 啤酒 時(shí)間: 2025-3-27 06:11
The Wind-Driven Circulationconstant density, followed by a consideration of the effects of stratification and topography. Important concepts and results are the Ekman layers, Ekman spiral and Ekman transport, the Sverdrup transport and the Stommel/Munk gyre models of the large-scale circulation. The impact of topography and s作者: Omnipotent 時(shí)間: 2025-3-27 12:05 作者: 植物學(xué) 時(shí)間: 2025-3-27 17:13
Approximations Derived from Mode Filteringmore advanced reader and not meant to be studied in detail since many of the issues, which are only touched here, are covered in more detail later. References to the more detailed discussions are given in the respective context.作者: SEEK 時(shí)間: 2025-3-27 19:22 作者: flaggy 時(shí)間: 2025-3-28 00:32 作者: Mutter 時(shí)間: 2025-3-28 02:59 作者: braggadocio 時(shí)間: 2025-3-28 07:55 作者: DOSE 時(shí)間: 2025-3-28 13:30 作者: 完整 時(shí)間: 2025-3-28 16:30 作者: archenemy 時(shí)間: 2025-3-28 19:57
Forced Wavesct and can be created by other waves. We have discussed a general treatment in Section 9.6, using a Lagrangian framework. We expand the treatment to a situation where a random ensemble of waves is an adequate representation for the wave field.作者: brassy 時(shí)間: 2025-3-29 00:00
Geostrophic Turbulencection 12.2 is devoted to the more realistic inhomogeneous situation of the real ocean. In Section 12.3 we discuss alternative averaging frameworks to differentiate between advective and diffusive effects of turbulent mixing.作者: 不規(guī)則 時(shí)間: 2025-3-29 03:42
Small-Scale Turbulenceiscussed in Section 11.1, while basic concepts of turbulent mixing are described in Section 11.2. The application to the real, i. e. inhomogeneous, ocean in the presence of density stratification and large gravity force and the development of basic turbulence closure schemes can be found in Section 11.3.作者: strdulate 時(shí)間: 2025-3-29 11:15
The Wind-Driven Circulationstigated using the model BARBI. This model represents the interaction of barotropic and baroclinic fields in a minimal way. The spin-up of the wind-driven circulation by wave processes was presented in Section 8.2.6.作者: Constant 時(shí)間: 2025-3-29 14:37
Physics of Heat Exchange with the Environment,t temperature difference (. .C.). In the case of evaporation on the skin, the water vapour pressure difference (.) between the body surface and the ambient air substitutes for the temperature difference.作者: Apogee 時(shí)間: 2025-3-29 17:37 作者: CHURL 時(shí)間: 2025-3-29 22:01 作者: 類人猿 時(shí)間: 2025-3-30 01:45 作者: 分散 時(shí)間: 2025-3-30 05:22 作者: Lymphocyte 時(shí)間: 2025-3-30 12:00
IGEC Transactions, Volume 1: Energy Conversion and Management978-3-031-48902-0Series ISSN 2352-2534 Series E-ISSN 2352-2542 作者: NOVA 時(shí)間: 2025-3-30 15:19 作者: Condescending 時(shí)間: 2025-3-30 19:57
