01530nam1 22003131i 450 UON0002367320231205102030.73720020107g19291930 |0itac50 bafreFR|||| 1||||ˆLes ‰Civilisations de l'OrientRené GroussetParisLes Editions G. Crés1929-304 v.ill.21 cm001UON000236842001 ˆL' ‰OrientRené Grousset210 ParisLes Editions G. Crés et C.1929 ii360 p.ill. ; 20 cm1001UON000236862001 ˆL' ‰IndeRené Grousset210 ParisLes Editions G. Crés et C.1930 ii370 p.ill. ; 20 cm2001UON000236922001 ˆL' ‰IndeRené Grousset210 ParisEditions d'Histoire et d'Art1949 iii172 p.ill., tavole ; 22 cm2001UON000236872001 ˆLa ‰ChineRené Grousset210 ParisLes Editions G. Crés et C.1930 ii360 p.ill. ; 20 cm3001UON000236902001 ˆLe ‰JaponRené Grousset210 ParisLes Editions G. Crés et C.1930 viii319 p.ill. ; 20 cm4ARTE ORIENTALEUONC001004FIORIENTECULTURA E CIVILTA'UONC002364FIFRParisUONL002984GROUSSETRenéUONV005022376228Crés et C.UONV249694650ITSOL20240220RICAUON00023673ARTE - AsiaARTE ORIENTALEUONC002016Civilisations de l'Orient40334UNIOR05466nam 22007215 450 991029836530332120251117074619.03-319-00473-510.1007/978-3-319-00473-0(CKB)3710000000094966(EBL)1698104(OCoLC)881165909(SSID)ssj0001186807(PQKBManifestationID)11629596(PQKBTitleCode)TC0001186807(PQKBWorkID)11240601(PQKB)10512873(MiAaPQ)EBC1698104(DE-He213)978-3-319-00473-0(PPN)177825936(EXLCZ)99371000000009496620140326d2014 u| 0engur|n|---|||||txtccrPhysics of Lakes Volume 3: Methods of Understanding Lakes as Components of the Geophysical Environment /by Kolumban Hutter, Irina P. Chubarenko, Yongqi Wang1st ed. 2014.Cham :Springer International Publishing :Imprint: Springer,2014.1 online resource (660 p.)Advances in Geophysical and Environmental Mechanics and Mathematics,1866-8348Description based upon print version of record.3-319-00472-7 Includes bibliographical references at the end of each chapters and indexes.Barotropic Wind-induced Motions in a Shallow Lake -- Response of a Stratified Alpine Lake to External Wind Fields – Numerical Prediction and Comparison with Field Observations -- Comparing Numerical Methods for Convectively-Dominated Problems -- Comparing Different Numerical Treatments of Advection Terms for Wind-Induced Circulations in Lakes -- Subgrid-Scale Parameterization in Numerical Simulations of Lake Circulation -- Instruments and Sensors -- Measuring Methods and Techniques -- Dimensional Analysis, Similitude and Model Experiments -- Prograding and Retrograding Hypo- and Hyperpycnal Deltaic Formations into Quiescent Ambients -- Sediment Transport in Alluvial Systems.The ongoing thread in this volume of Physics of Lakes is the presentation of different methods of investigation for processes taking place in real lakes with a view to understanding lakes as components of the geophysical environment. It is divided into three parts. Part I is devoted to numerical modeling techniques and demonstrates that (i) wind-induced currents in depth-integrated models can only adequately predict current fields for extremely shallow lakes, and (ii) that classical multi-layered simulation models can only adequately reproduce current and temperature distributions when the lake is directly subjected to wind, but not the post-wind oscillating response. This makes shock capturing discretization techniques and Mellor-Yamada turbulence closure schemes necessary, as well as extremely high grid resolution to reduce the excessive numerical diffusion. Part II is devoted to the presentation of principles of observation and laboratory experimental procedures. It details the principles of operation for current, temperature, conductivity and other sensors applied in the field. It also discusses the advantages and limitations of common measuring methods like registration from stationary or drifting buoys, sounding and profiling from a boat, etc. Questions of data accuracy, quality, and reliability are also addressed. The use of laboratory experiments on a rotating platform is based on an exposition of dimensional analysis and model theory and illustrated using Lake Constance as an example. Part III gives an account of the dynamics of lake water as a particle-laden fluid, which, coupled with the transport of the bottom sediments, leads to morphodynamic changes of the bathymetry in estuarine and possibly whole lake regions. An elegant spatially one-dimensional theory makes it possible to derive analytic solutions of deltaic formations which are corroborated by laboratory experiments. A full three-dimensional description of the evolution of the alluvial bathymetry under prescribed tributary sediment input indicates a potential subject for future research.Advances in Geophysical and Environmental Mechanics and Mathematics,1866-8348GeophysicsOceanographyEnvironmental geologyEnvironmental geologyGeophysics/Geodesyhttps://scigraph.springernature.com/ontologies/product-market-codes/G18009Oceanographyhttps://scigraph.springernature.com/ontologies/product-market-codes/G25005Geoecology/Natural Processeshttps://scigraph.springernature.com/ontologies/product-market-codes/U21006Geophysics.Oceanography.Environmental geology.Environmental geology.Geophysics/Geodesy.Oceanography.Geoecology/Natural Processes.551.482Hutter Kolumbanauthttp://id.loc.gov/vocabulary/relators/aut47891Chubarenko Irina P.authttp://id.loc.gov/vocabulary/relators/autWang Yongqiauthttp://id.loc.gov/vocabulary/relators/autMiAaPQMiAaPQMiAaPQBOOK9910298365303321Physics of Lakes2520030UNINA