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標(biāo)題: Titlebook: Mathematics of the Weather; Polygonal Spline Loc Jürgen Steppeler,Jinxi Li Textbook 2022 Springer Nature Switzerland AG 2022 CFD.Finite Ele [打印本頁]

作者: 歸納    時間: 2025-3-21 17:11
書目名稱Mathematics of the Weather影響因子(影響力)




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作者: 桉樹    時間: 2025-3-21 23:51

作者: CHYME    時間: 2025-3-22 02:49

作者: NADIR    時間: 2025-3-22 06:07
Jürgen Steppeler,Jinxi Lil methods. With mat- matical developments in the ?elds of dynamic system’s theory, exempli?ed by Edward Lorenz’s pioneering work, and fractal theory, starting with the early fractal concepts inferred by Harold Edwin Hurst from the analysis of geoph- ical time series,nonlinear methods became availabl
作者: 落葉劑    時間: 2025-3-22 11:36

作者: Airtight    時間: 2025-3-22 13:14

作者: 厭惡    時間: 2025-3-22 18:22

作者: 煞費(fèi)苦心    時間: 2025-3-22 23:20

作者: Glaci冰    時間: 2025-3-23 04:14
978-3-031-07240-6Springer Nature Switzerland AG 2022
作者: 有常識    時間: 2025-3-23 06:46

作者: 啟發(fā)    時間: 2025-3-23 09:52
Platonic and Semi- Platonic Solids,ids and a simple non-conserving toy model. However, the tools and the example provided in Chapters “Finite Difference Schemes on Sparse and Full Grids” and “Full and Sparse Hexagonal Grids in the Plane” allow to create L-Galerkin sparse grids on the sphere. Further L-Galerkin methods will be presented in Chapter “Numerical Tests.”
作者: Cpap155    時間: 2025-3-23 13:53

作者: evince    時間: 2025-3-23 18:40

作者: 不利    時間: 2025-3-23 22:15

作者: EXUDE    時間: 2025-3-24 03:57

作者: 脫離    時間: 2025-3-24 08:26
Summary and Outlook,This section deals with potential applications and important research areas of numerical models of the atmosphere.
作者: Locale    時間: 2025-3-24 11:22

作者: Goblet-Cells    時間: 2025-3-24 15:49
2194-5217 appeal to researchers and industry specialists working on th."Mathematics of the Weather” details the mathematical techniques used to create numerical models of the atmosphere. It explains methods which are currently considered for practical use in models for the exaflop computers (10**19 operations
作者: subacute    時間: 2025-3-24 21:44

作者: 獸皮    時間: 2025-3-25 02:06
Simple Finite Difference Procedures, It is readable with basic knowledge of mathematics and without previous knowledge of numerics and this chapter is overlapping with Durran (Numerical methods for fluid dynamics: with applications to geophysics, 2nd edn. Springer, New York, pp. 35–146, 2010) for the convenience of the reader.
作者: 不開心    時間: 2025-3-25 06:52

作者: 兇猛    時間: 2025-3-25 08:16

作者: 灰姑娘    時間: 2025-3-25 12:26

作者: Ceremony    時間: 2025-3-25 16:18
2D Basis Functions for Triangular and Rectangular Meshes,, the meshes will be presented as structured. For research in new numerical methods, structured test models have the advantage of being easy to create. Unstructured programming is conveniently done by using a neighborhood management system, which is present in the MPAS, COSMO, and Fluidity models.
作者: 去掉    時間: 2025-3-25 22:43
Finite Difference Schemes on Sparse and Full Grids,ilities is too large. So just examples are presented to show how the schemes work. In particular, most examples are 2D. While the complexity of computer programs normally increases substantially when going to 3D, it is often obvious how to proceed from 2D to 3D.
作者: paroxysm    時間: 2025-3-26 02:39
Simple Finite Difference Procedures,rs. As this book is mainly about spatial discretization, the fourth-order Runge–Kutta scheme is used in tests for time discretization. A rather comprehensive set of possibilities is given in Durran (Numerical methods for fluid dynamics: with applications to geophysics, 2nd edn. Springer, New York, p
作者: Indurate    時間: 2025-3-26 07:48
Local- Galerkin Schemes in 1D,and therefore more practical on multiprocessing computers. A well-known example is the spectral element (SE) method, but there exist a large number of alternatives, named o.o. or the third-degree method. o.o. approximates the fields in order . and the fluxes in order .. All methods described here us
作者: 領(lǐng)先    時間: 2025-3-26 12:13

作者: SEED    時間: 2025-3-26 15:56
Finite Difference Schemes on Sparse and Full Grids,ty to make models more efficient for the same resolution. This section aims at transferring some of the 1D schemes defined in Chapter “Local-Galerkin Schemes in 1D” to two dimensions. There is no way the most general L-Galerkin scheme or a class of such schemes can be presented. The number of possib
作者: arousal    時間: 2025-3-26 19:14
Platonic and Semi- Platonic Solids,ids and a simple non-conserving toy model. However, the tools and the example provided in Chapters “Finite Difference Schemes on Sparse and Full Grids” and “Full and Sparse Hexagonal Grids in the Plane” allow to create L-Galerkin sparse grids on the sphere. Further L-Galerkin methods will be present
作者: 混合    時間: 2025-3-26 23:06

作者: 固執(zhí)點(diǎn)好    時間: 2025-3-27 02:48
Jürgen Steppeler,Jinxi Lialong seemingly unrelated paths. In spite of the fact that the - plication of nonparametric techniques in time series can be traced back to the 1940s at least, there still exists healthy and justi?ed skepticism about the capability of nonparametric methods in time series analysis. As - thusiastic ex
作者: mucous-membrane    時間: 2025-3-27 07:26

作者: Countermand    時間: 2025-3-27 13:11
Jürgen Steppeler,Jinxi Li availability of enlarged data sets and sophisticated methods for their analysis. Univariate as well as multivariate time series are a particular class of such data which are of special importance for studying the dynamical p- cesses in complex systems. Time series analysis theory and applications i
作者: 上下倒置    時間: 2025-3-27 17:08
Jürgen Steppeler,Jinxi Lial scales. In this contribution, we explicitly take the spatial dimension into account. Recent studies on this aspect have considered individual investigations of spatially distributed records from different stations, which form network structures with interesting statistical properties. However, th
作者: lanugo    時間: 2025-3-27 20:01
ed with all details. Considering the fact that the satellite altimetry technique can provide sea level observations at the global scale, spherical harmonics defined for the whole range of spherical coordinates (0 ≤ λ ≤ 2π, and ? π/2 ≤ ?≤ +π/2) could be among the possible choices for global ocean tid
作者: Esophagus    時間: 2025-3-28 01:11

作者: 確定無疑    時間: 2025-3-28 02:15
Robert E Barnhill,James H Brownomes causing QT prolongation (Vlachos et al. 2016). Sager and colleagues (2014) therefore observed that, given our advancing knowledge and understanding on multiple fronts, it is incumbent upon us to provide a more comprehensive evaluation of actual proarrhythmic risk. These advances are evident in
作者: FEAS    時間: 2025-3-28 06:20
Jean H. Overmeyer,Robert A. Erdman,William A. Maltese of introducing AT in relation, on the one hand, to user needs and, on the other, to the age, type and standard of property. However, the extent to which AT can narrow the gap between the home environment and individual capacity, depends upon the willingness of older people to use AT. If AT is to be
作者: CRAB    時間: 2025-3-28 12:15
Die Links-Rechts-Positionierung der Parteien bei den Bundestagswahlen 2005 bis 2013: Eine empirischezwei Lagern deutlich bestehen, insbesondere nachdem die Piraten 2013 im Vergleich zu 2009 weiter links verortet werden und weil die AfD sehr nahe an der Union und klar im bürgerlichen Lager liegt. Die Befunde sprechen überdies insgesamt nach wie vor für die Brauchbarkeit einer einfachen Links-Rechts
作者: Limpid    時間: 2025-3-28 15:30

作者: Stagger    時間: 2025-3-28 19:32
,The “Black Trinity” and the Cold War,ourse throughout the Cold War demonstrates the inherent appeal of heuristics under the conditions of uncertainty.. Furthermore, many scholars argued that the perceptions and interpretations of these events framed the political perspective toward the Soviet bloc and well beyond its borders.
作者: expansive    時間: 2025-3-29 02:36

作者: incarcerate    時間: 2025-3-29 06:37
ehend von einer Kl?rung des Kulturbegriffs bietet dieses Buch?eine umfassende?Studie?zu den?historischen Entwicklungen, zentralen Institutionen und Handlungsfelder?der Kulturpolitik in Deutschland.978-3-531-19402-8978-3-531-19403-5




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