Academic literature on the topic 'Sharp River Bends'

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Journal articles on the topic "Sharp River Bends"

1

Ottevanger, W., K. Blanckaert, and W. S. J. Uijttewaal. "Processes governing the flow redistribution in sharp river bends." Geomorphology 163-164 (August 2012): 45–55. http://dx.doi.org/10.1016/j.geomorph.2011.04.049.

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2

Tritthart, M., and D. Gutknecht. "3-D computation of flood processes in sharp river bends." Proceedings of the Institution of Civil Engineers - Water Management 160, no. 4 (2007): 233–47. http://dx.doi.org/10.1680/wama.2007.160.4.233.

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3

Zhao, Shui-Xia, Wen-Jun Wang, Xiao-Hong Shi, et al. "Freeze-Up Ice Jam Formation in the River Bend, a Case Study on the Inner Mongolia Reach of Yellow River." Crystals 11, no. 6 (2021): 631. http://dx.doi.org/10.3390/cryst11060631.

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Concern has been expressed regarding the impacts of climate change on river ice and ice jam formation in cold regions. Ice jams are easily initiated in bends and narrow channels and cause disasters. In this study, observations and remote sensing monitoring are used to study the freeze-up ice jam formation of bends. Sediment transport and freezing process of the river interact, influencing bed changes profile and sedimentary budget. River ice processes, channel evolution, ice hydro-thermodynamics, and ice jam accumulation are explored. The results show that the channel topography determines the
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4

Kranenburg, Wouter M., W. Rockwell Geyer, Adrian Mikhail P. Garcia, and David K. Ralston. "Reversed Lateral Circulation in a Sharp Estuarine Bend with Weak Stratification." Journal of Physical Oceanography 49, no. 6 (2019): 1619–37. http://dx.doi.org/10.1175/jpo-d-18-0175.1.

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AbstractAlthough the hydrodynamics of river meanders are well studied, the influence of curvature on flow in estuaries, with alternating tidal flow and varying water levels and salinity gradients, is less well understood. This paper describes a field study on curvature effects in a narrow salt-marsh creek with sharp bends. The key observations, obtained during times of negligible stratification, are 1) distinct differences between secondary flow during ebb and flood, with helical circulation as in rivers during ebb and a reversed circulation during flood, and 2) maximum (ebb and flood) streamw
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5

Vermeulen, B., A. J. F. Hoitink, S. W. van Berkum, and H. Hidayat. "Sharp bends associated with deep scours in a tropical river: The river Mahakam (East Kalimantan, Indonesia)." Journal of Geophysical Research: Earth Surface 119, no. 7 (2014): 1441–54. http://dx.doi.org/10.1002/2013jf002923.

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6

Xia, Junqiang, Qingrong Jiang, Shanshan Deng, et al. "Morphological characteristics and evolution processes of sharp bends in the Lower Yellow River." CATENA 210 (March 2022): 105936. http://dx.doi.org/10.1016/j.catena.2021.105936.

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7

Hamidifar, Hossein, Alireza Keshavarzi, and Paweł M. Rowiński. "Influence of Rigid Emerged Vegetation in a Channel Bend on Bed Topography and Flow Velocity Field: Laboratory Experiments." Water 12, no. 1 (2019): 118. http://dx.doi.org/10.3390/w12010118.

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Trees have been used extensively by river managers for improving the river environment and ecology. The link between flow hydraulics, bed topography, habitat availability, and organic matters is influenced by vegetation. In this study, the effect of trees on the mean flow, bed topography, and bed shear stress were tested under different flow conditions. It was found that each configuration of trees produced particular flow characteristics and bed topography patterns. The SR (single row of trees) model appeared to deflect the maximum velocity downstream of the bend apex toward the inner bank, w
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8

KANG, Taeun, Ichiro KIMURA, and Yasuyuki SHIMIZU. "STUDIES ON RIVER FLOWS AT SHARP BENDS WITH A WEAK SECONDARY FLOW USING 2D AND 3D CFD MODELS." Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) 73, no. 4 (2017): I_613—I_618. http://dx.doi.org/10.2208/jscejhe.73.i_613.

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9

Spicer, Preston, and Kimberly Huguenard. "Observations of Near-Surface Mixing Behind a Headland." Journal of Marine Science and Engineering 8, no. 2 (2020): 68. http://dx.doi.org/10.3390/jmse8020068.

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Field observations were collected near the mouth of the Bagaduce River, Maine, in order to understand how complex features affect the intratidal and lateral variability of turbulence and vertical mixing. The Bagaduce River is a low-inflow, macrotidal estuary that features tidal islands, tidal flats and sharp channel bends. Profiles of salinity, temperature, and turbulent kinetic energy dissipation (ε) were collected for a tidal cycle across the estuary with a microstructure profiler. Lateral distributions of current velocities were obtained with an acoustic doppler current profiler. Results sh
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10

Mayomi, Ikusemoran, John Abdullahi, and Anthony Dami. "Terrain Analysis of Biu Plateau, for Road Transport Development, Borno State, Nigeria." Journal of Geography and Geology 6, no. 2 (2014): 28. http://dx.doi.org/10.5539/jgg.v6n2p28.

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Among all the means of transportation, road has been described as the most important, probably because of its flexibility and its low cost in terms of construction, maintenance and usage. However, in Nigeria, road is considered to be the most dangerous means of transportation because of their bad nature such as sharp bends, narrow bridges, steep slopes and other related problems which are associated with the terrain where these roads are constructed. Road transportation therefore needs proper planning and development through the use of geo-information technologies that would ease accessibility
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