2 edition of Morphological and hydrological regularities of the structure of the river net found in the catalog.
Morphological and hydrological regularities of the structure of the river net
N. A. Rzhanitsyn
|LC Classifications||GB1205 .R963|
|The Physical Object|
|Pagination||xi, 380 p.|
|Number of Pages||380|
river morphology. The study of the channel pattern and the channel geometry at several points along a river channel, including the network of tributaries within the drainage basin. Also known as channel morphology; fluviomorphology; stream morphology. Morphology may be defined as the science of structure or form "and fluvial may be defined as produced by the action of flowing water." Since rivers can hardly be said to have structure, fluvial morphology is therefore the science of the form as produced by the action of flowing water.
Wood falling from the forest canopy is an important element in the structure of these streams. The middle river represents a balance between deposition and erosion. Much of the heavier material is deposited but lighter silts and sands can still be picked up by . Lakes: Lake Morphological Impact Assessment Tool (MImAS) since GIS, remote sensing and groundtruthing over last 3 years for lakes 19 pressure metrics relating to the water levels, shoreline, structures and land use Photo: W. Trodd Transitional and Coastal: Hydromorphological Quality Index (HQI; developed in-house) 13 metrics 4 GIS.
International Journal of Sediment Research 23 () Erosion, sediment transportation and accumulation in rivers N. I. ALEKSEEVSKIY 1, K. M. BERKOVICH 2, and R. S. CHALOV 3 Abstract The present paper analyses the interrelation between erosion, sediment transportation and accumulation proposed by N. I. Makkaveyev () and its further development in modern studies of river Cited by: The terms river morphology and its synonym stream morphology are used to describe the shapes of river channels and how they change in shape and direction over time. The morphology of a river channel is a function of a number of processes and environmental conditions, including the composition and erodibility of the bed and banks (e.g., sand, clay, bedrock); erosion comes from the power and Bedforms: Ait, Antidune, Dune, Current ripple.
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Get this from a library. Morphological and hydrological regularities of the structure of the river net. [N A Rzhanitsyn]. The problem of assessment of sea level rise impact on the hydrological regime and morphological structure of river deltas is discussed.
Studies of the response of river deltas, which are among the most vulnerable natural objects. Rzhanitsyn, N.A. () Morphological and hydrological regularities of the structure of the river net, translated by Krimgold for USDA, original Gidrometeoizdat, Leningrad.
Google Scholar Shaw, E.M. () Engineering hydrology techniques in practice, Series in Cited by: 4. Regularities in sea level rise impact on the hydrological regime and morphological structure of river deltas.
Abstract. The problem of assessment of sea level rise impact on the hydrological regime and morphological structure of river deltas is by: The major hydrological and geographic characteristics of the Godavari River and the coastal zone of the Bay of Bengal that have their effect on the hydrological regime and the morphological structure of the river delta are considered.
The hydrographic, climatic, and environmental conditions in the Godavari delta are by: 3. The main regularities of hydrological and hydrological-environmental processes occurring within the complex estuary, the Chesapeake Bay and the mouths of its tributaries, are discussed.
The peculiarities of the estuary morphological structure, including the structures of tidal and net currents, salinity and water turbidity fields and their variability, the environmental conditions, and their Cited by: 2.
Morphological, hydrological, biogeochemical and ecological changes surroundings in structure or function; known as functional process zones (FPZ)) (Thorp et al., ). Patches on which Because increased morphological variability in the river bed enhances hyporheic exchange, river Cited by: Analysis of morphological and hydrological changes in the Correntes river The morphological changes were identified between and using LANDSAT TM 5 (/72) satellite images from September and the recently launched CBERS 4, (/), Maya panchromatic camera with m spatial resolution.
HYDROLOGICAL CYCLE CONTENTS VOLUME I The Hydrological Cycle 1 Igor Alekseevich Shiklomanov, Director, State Hydrological Institute, St.
Petersburg, Russia 1. Introduction: Definitions of Hydrosphere and Hydrological Cycle 2. Composition of the Hydrosphere Distribution of Water Water in Oceans and Seas Subsurface Water The characteristic hydrological feature of all IRES is intermittence (Chapter 1), often followed by drying of part or all of the channel (Fig.
).Rewetting usually coincides with the onset of sustained flow although in some IRES, there may be several “false starts” where surface water is present or pools fill and then dry for several weeks or even months before streamflow begins in.
We provide an example of analyzing the hydrographic network of the Komarovka river basin in order to develop the technique of objective digitizing and correct determination of a first-order water stream. Keywords: hydrological modeling, hydrographic network, structure of river systems, digital models of the by: 7.
As part of an hierarchical, multi-scale, hydro- morphological framework for European rivers that has been developed within the REFORM project, a procedure for classifying rivers has been devised.
The procedure includes components that categorise river channel mor. river, and a river may meander continuously for hundreds of kilometers through a flood plain. The term is derived from the River Meanderes in Turkey. If a meandering channel has been rejuvenated, a channel begins to under-cut a river bed while keeping a meandering course.
As a result, a meandering valley is formed, and the river runningFile Size: KB. FRESH SURFACE WATER – Vol. I -River Morphology and Channel Processes - Iware Matsuda ©Encyclopedia of Life Support Systems (EOLSS) The higher the water velocity, the more capacity a river has for transporting sediment load.
There are three different processes in transporting sediment load. They are corrosion, suspension and traction. UNESCO – EOLSS SAMPLE CHAPTERS FRESH SURFACE WATER – Vol. I - Types of River Ecosystems - G.
van der Velde, R.S.E.W. Leuven, I. Nagelkerken ©Encyclopedia of Life Support Systems (EOLSS) Flow The most obvious characteristic of rivers is that they flow, which distinguishes theseFile Size: KB.
The peculiarities of river and sea hydrological factors responsible for the regime of the Thames River mouth area are described in detail. Characteristics of the river water runoff were specified and supplemented by the data on the river inundations in the area of by: 4.
The main marine hydrological factors that influence the regime and structure of river mouths, including the mean (background) sea level, waves, tides, and storm surges, are : Maria Mikhailova. The main marine hydrological factors that influence the regime and structure of river mouths, including the mean (background) sea level, waves, tides, and storm surges, are discussed.
Regularities in the response of the mouths of major rivers, flowing into the Caspian Sea, to large-scale variations in its level and river water runoff and sediment yield are considered. Part Two Other hydraulic structures 8 River engineering Introduction Some basic principles of open-channel ﬂow River morphology and régime River surveys Flow-measuring structures River ﬂood routing River improvement Worked examples References 9 Diversion works.
Applied River Morphology is not the only river morphology book you will need, but it is the only one you will refer to again and again, on every project. This book is even enjoyable to read through and look at the photos and sketches during non-work by: Applied River Morphology.
Luna Leopold best describes Dave Rosgen’s new book, Applied River Morphology, as “a generous and detailed explanation of the classification system and how it might be used to incorporate the observed processes of river mechanics into restoration design.” Applied River Morphology is the product of Dave Rosgen, a File Size: KB.Inﬂuence of catchment processes on ﬂuvial morphology and river habitats Askoa Ibisate1,∗, Alfredo Ollero2 and Elena D´ıaz1 1 Section of Physical Geography, Dept.
of Geography, Prehistory and Archaeology, University of Basque Country, Tom´as y Valiente s/n, Vitoria-Gasteiz.