Don ; Erosion ; European part of Russia ; Seasonal variation ; Stream ; Suspended load ; UralRiver ; Volga ; Watershed ; Years 1940-49 ; Years 1970-79 ; Zonality
Années 1940 ; Années 1970 ; Bassin-versant ; Charge en suspension ; Cours d'eau ; Don ; Erosion ; Russie d'Europe ; Ural fleuve ; Variation saisonnière ; Volga ; Zonalité
Climatic data ; European part of Russia ; Seasonal variation ; Twentieth Century ; UralRiver ; Volga ; Watershed ; Wind ; Wind speed ; Years 1930-39 ; Years 1990-99
Années 1930 ; Années 1990 ; Bassin-versant ; Donnée climatique ; Russie d'Europe ; Siècle 20 ; Ural fleuve ; Variation saisonnière ; Vent ; Vitesse du vent ; Volga
Caspienne Sea ; Fluvial geomorphology ; Human impact ; Hydrology ; Impact ; River mouth ; Russia ; Sea level ; Sedimentation ; Stream ; Stream flow ; UralRiver ; Volga ; Water management
Action anthropique ; Caspienne ; Cours d'eau ; Ecoulement fluvial ; Embouchure ; Gestion de l'eau ; Géomorphologie fluviale ; Hydrologie ; Impact ; Niveau marin ; Russie ; Sédimentation ; Ural fleuve ; Volga
Acción antrópica ; Corriente de agua ; Desembocadura ; Escorrentíafluvial ; Gestión del agua ; Hidrología ; Impacto ; Mar Caspio ; Nivel del mar ; Rio Ural ; Rusia ; Sedimentación ; Volga
Les zones d'embouchure des fleuves Volga, Terek, Sulak, Ural, et Kura se jetant dans la mer Caspienne subissent l'impact des fluctuations du niveau marin. Cet impact se manifeste par le changement du volume d’écoulement et de la sédimentation
Don ; European part of Russia ; Natural resources ; Runoff ; Spatial differentiation ; Surface water ; Underground flow ; Underground water ; UralRiver ; Volga ; Water balance ; Water supply ; Watershed
Approvisionnement en eau ; Bassin-versant ; Bilan hydrologique ; Différenciation spatiale ; Don ; Eau de surface ; Eau souterraine ; Ecoulement ; Ecoulement souterrain ; Ressource naturelle ; Russie d'Europe ; Ural fleuve ; Volga
Abastecimiento de agua ; Agua de superficie ; Agua subterránea ; Balance hidrológico ; Cuenca hidrográfica ; Diferenciación espacial ; Escorrentía ; Escorrentía subterránea ; Recursos naturales ; Rio Ural ; Rusia de Europa ; Volga
Asia ; Delimitation ; Don ; Eighteenth Century ; Eurasia ; Europe ; Frontier ; History of geography ; History of ideas ; Pechora River ; Russia ; Russian school ; Ural Mountains ; Volga
Asie ; Don ; Délimitation ; Ecole russe ; Eurasie ; Europe ; Frontière ; Histoire de la géographie ; Histoire des idées ; LOMONOSSOV (M.V.) ; Pečora fleuve ; Russie ; Siècle 18 ; Ural monts ; Volga
Asia ; Delimitación ; Escuela rusa ; Eurasia ; Europa ; Frontera ; Historia de la geografía ; Historia de las ideas ; Montes Ural ; Rusia ; Siglo 18 ; Volga
Caspienne Sea ; Eurasia ; Lake ; Lake level ; Precipitation ; Salt lake ; Statistics ; Temperature ; Thermal anomaly ; Time series ; UralRiver ; Volga ; Watershed
or their ancestors, had been trapped when the ice sheet advanced southwards across Siberian coastal water and, by blocking rivers, gave rise to an enormous lake system. Crossing the Urals and migrating westwards along ice-dammed waters, the relicts invaded Northern
Diatom ; Ecosystem ; European part of Russia ; Geological deposit ; Human impact ; Hydrobiology ; Hydrocarbon ; Hydrochemistry ; Impact study ; Industrial pollution ; River basin
When is a River not a River ? Consideration of the legal definition of a river for geomorphologists practising in New South Wales, Australia
Australia ; Concept ; Definition ; Environmental management ; Geomorphology ; Legislation ; New South Wales ; Perception ; River bed ; Stream ; Water resources
This paper examines why the definition of a river is an important and ongoing management issue, and outlines the development of legal definitions of river. Finally, the role of fluvial geomorphology is discussed with respect to the definition
of a river and its channel. This analysis will reveal whether the existing legislative framework adequately reflects the physical realities of rivers and watercourses so as to facilitate their conservation.
Sedimentatieverschijnselen nabij een rivier stuw op de Markrivier Sedimentation phenomena near a river dam on the river Mark
To alter the natural river behaviour, many regulation projects have been carried out on various river systems. However, until now very few studies on the reactions of the rivers to the imposed regulating systems have been undertaken. - (Author).
Channel geometry ; China ; Fluvial dynamics ; Fluvial processes ; Meander ; Model ; River bed ; Statistics ; Stream ; Stream flow
Since the anabranched river pattern is the most typical one in the middle and lower reaches of the Yangtze River (Changjiang) as well as in many other rivers in China, a systematic study on the formation cause of the anabranched river pattern has
been made in recent years, including field observations, modeling experiments in four river models under different boundary conditions, the analyses of river pattern formation and transformation etc. In this paper, some of the detailed results obtained
Some thermodynamic criteria for river channel changes
Fluvial dynamics ; Geosystem ; River bed ; Spatial variation ; Stream ; Stream flow
A theoretical model of river channel changes is presented, which shows some nonequilibrium thermodynamic criteria of a river channel to bedding and equilibrium.
Geometric properties of river cross sections and associated hydrodynamic implications in Wuhan-Jiujiang river reach, the Yangtze River
Based on measured hydrological data by using ship-mounted Acoustic Doppler Current Profiler (ADCP) instrument, the AA. analyzed shapes of river cross sections of the middle Yangtze River basin (mainly focusing on Makou and Tianjiazhen river reach
). The hydrologic data of 36 river cross sections have been successfully obtained. In this paper, the AA. try to characterize the hydrodynamic properties of river knots, associated backwater effects and their implications for flood mitigation in the middle and lower