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Artigos de revistas sobre o tema "River basin"

Autor: Grafiati

Publicado: 4 de junho de 2021

Última modificação: 26 de julho de 2025

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1

Filipovic, Ivan, Aleksandar Radivojevic, and Ljiljana Dimitrijevic. "Regularities of cartographic generalization of the density of river basin and proportion of the degree of generalization on the maps of different scales." Glasnik Srpskog geografskog drustva 91, no. 2 (2011): 113–21. http://dx.doi.org/10.2298/gsgd1102113f.

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Cartographic generalization of the rivers is a very complex process in cartography. Cartographic generalization involves reduction of water flows, their length, width and the density of river basin with the reducing of the map scale. In this study we analyzed the ratio of the density of river basin and the size of the degree of generalization of the maps of different scale. The example is the Velika Morava river basin. Based on the results given here we get to the basic regularities of proportion of the degree of generalization of the density of river basin.

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2

Aida, Korjenić, Temimović Emir, Banda Amra, and Sivac Amina. "BASIC CHARACTERISTICS OF THE PLUVIOMETRIC REGIME IN THE UNA RIVER BASIN." International Journal of Research -GRANTHAALAYAH 6, no. 2 (2018): 234–45. http://dx.doi.org/10.29121/granthaalayah.v6.i2.2018.1566.

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Intensity of action and frequency of high and low pressure barometric fields of large and medium scale have great influence on dynamics of pluviometric regime. On their action depend characteristics of thermic regime, relative humidity, cloudiness and windiness, which directly affect the precipitation. Concerning that the water balance is difference between the inflow and evaporation, it comes that precipitations do not have just special role, but they are also the most important factor of the Una river regime. Disposition and precipitation structure are the river regime's essential assumption

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3

Korjenić, Aida, Emir Temimović, Amra Banda, and Amina Sivac. "BASIC CHARACTERISTICS OF THE PLUVIOMETRIC REGIME IN THE UNA RIVER BASIN." International Journal of Research - Granthaalayah 6, no. 2 (2018): 234–45. https://doi.org/10.5281/zenodo.1194665.

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Intensity of action and frequency of high and low pressure barometric fields of large and medium scale have great influence on dynamics of pluviometric regime. On their action depend characteristics of thermic regime, relative humidity, cloudiness and windiness, which directly affect the precipitation. Concerning that the water balance is difference between the inflow and evaporation, it comes that precipitations do not have just special role, but they are also the most important factor of the Una river regime. Disposition and precipitation structure are the river regime's essential assump

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4

Bezgodova, O. V. "Structural and Morphometric Analysis of the Ihe-Ukhgun Small River Basin (Irkut River Basin)." Bulletin of Irkutsk State University. Series Earth Sciences 37 (2021): 3–16. http://dx.doi.org/10.26516/2073-3402.2021.37.3.

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The article is devoted to the structural and morphometric analysis of a small rivers using the example of the Ihe-Ukhgun river basin (left tributary of the Irkut river), which is based on a complex processing of a digital elevation model (DEM). The author has prepared a hydrologically correct DEM based on the ALOS Digital Surface Model (DSM) satellite data, carried out an automated calculation and mapping of the basin erosion network based on the DEM data, calculated the structural indicators of the third-order basins for analyzing the basin organization of the small rivers network. Structural

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5

Vera-Alcaraz, Héctor S., Carla S. Pavanelli, and Cláudio H. Zawadzki. "Taxonomic revision of the Rineloricaria species (Siluriformes: Loricariidae) from the Paraguay River basin." Neotropical Ichthyology 10, no. 2 (2012): 285–311. http://dx.doi.org/10.1590/s1679-62252012000200006.

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Species of the genus Rineloricaria from the Paraguay River basin were revised, the following species and geographic distributional patterns were found: R. aurata, Paraguay River basin in Brazil and Paraguay, rio Guaporé in Brazil; R. cacerensis, Paraguay River near Cáceres in Brazil; R. lanceolata, Paraguay River basin in Brazil and Paraguay, Guaporé, Ji-Paraná, Purus, Solimões, and Araguaia rivers in Brazil, Marañón and Madre de Dios rivers in Peru; R. parva, Paraguay River basin in Brazil and Paraguay, Paraná River in Argentina, Uruguay River in Brazil. Loricaria hoehnei is proposed as a new

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6

Boon, Philip J. "The catchment approach as the scientific basis of river basin management." River Systems 16, no. 1-2 (2005): 29–58. http://dx.doi.org/10.1127/lr/16/2005/29.

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7

Peng, Jing, Shaoming Li, and Lan Qi. "Study on river regulation measures of dried-up rivers of Haihe River basin, China." Water Science and Technology 67, no. 6 (2013): 1224–29. http://dx.doi.org/10.2166/wst.2013.680.

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In recent years, the ecological environment of plain rivers within Haihe River basin is questionable because of severe water shortages. Most of the rivers dry up regularly and it is therefore necessary to take measures to improve the river ecological environment. Meanwhile, flood control is the principal function for most of the dried-up rivers, so river regulation works for flood control also should be undertaken. In this paper, some measures of river regulation were selected applied to the Haihe River basin, taking these measures not only ensure the river security but also realize its ecolog

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8

Kurhanevych, L. P., and M. Z. Shipka. "GEOECOLOGICAL STATE OF THE FLOODPLAIN AND CHANNEL COMPLEX OF THE POLTVA RIVER BASIN (VISTULA RIVER BASIN REGION)." Hydrology, hydrochemistry and hydroecology, no. 1 (56) (2020): 64–70. http://dx.doi.org/10.17721/2306-5680.2020.1.7.

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In accordance with the water management zoning of the territory of Ukraine, the Poltva river basin belongs to the Vistula river basin region. The evaluation methodology of the channel and floodplain river complex state was proposed by Himko R. V. (2005). According to this methodology, the parameters (23 indicators), characterizing river state by points scale (5 quality classes), were defined. The research included three steps. During the preparatory stage cartographic materials were investigated and the coastal protection zones were highlighted. The fieldwork stage included: visual assessment

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9

Wang, Yichu, Danlu Liu, Enhang Liang, and Jinren Ni. "Structural Characteristics of Endorheic Rivers in the Tarim Basin." Remote Sensing 14, no. 18 (2022): 4502. http://dx.doi.org/10.3390/rs14184502.

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Endorheic rivers as landlocked systems with no hydrological connections to marine environments are suffering from water and ecosystem crisis worldwide, yet little is known about their structural characteristics with complex geomorphic and climatic dependence. Based on the river networks identified from 30 m resolution digital elevation models and surface water dynamic information derived from Landsat images, we investigate the hierarchical characteristics of 60 sub-basins in the Tarim Basin, the largest endorheic river basin in China. In the Tarim River basin, endorheic rivers exhibit a self-s

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10

Li, Yi, Jihai Yang, and Jing Zhang. "Assessing Environmental Performance of Water Infrastructure Based on an Attention-Enhanced Adaptive Neuro-Fuzzy Inference System and a Multi-Objective Optimization Model." Water 17, no. 6 (2025): 842. https://doi.org/10.3390/w17060842.

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This study aims to develop an integrated framework that combines an attention-enhanced adaptive neuro-fuzzy inference system (ANFIS) with multi-objective optimization to address the challenges of subjective indicator weight allocation and insufficient nonlinear relationship modeling in environmental performance evaluation of water infrastructure. Drawing on the tri-dimensional theory of performance evaluation—success, results, and actions—the framework organizes environmental performance indicators into five primary and nine secondary dimensions. Through empirical analysis across China’s five

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11

Tabunshchik, V. A. "MORPHOMETRIC CHARACTERISTICS OF RIVER BASINS OF THE NORTH-WESTERN SLOPE OF THE CRIMEAN MOUNTAINS (ZAPADNYY BULGANAK, ALMA, KACHA, BELBEK, CHERNAYA RIVER BASINS)." Scientific Notes of V.I. Vernadsky Crimean Federal University. Geography. Geology 7 (73), no. 3 (2021): 267–78. http://dx.doi.org/10.37279/2413-1717-2021-7-3-267-278.

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Zapadnyy Bulganak, Alma, Kacha, Belbek, Chernaya rivers belong to the rivers of the north-western slope of the Crimean Mountains. The sources of the rivers are located on the north-western slopes of the Main Ridge of the Crimean Mountains, then the rivers flow from east to west almost parallel to each other. Up to about the middle of their course, they have a character typical of mountain streams (except for the Zapadnyy Bulganak River). The river valleys in the upper reaches are V-shaped, narrow, their slopes are dissected by numerous gullies and tributaries. There are almost no tributaries i

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12

Tabunshchik, Vladimir, Roman Gorbunov, and Tatiana Gorbunova. "Anthropogenic Transformation of the River Basins of the Northwestern Slope of the Crimean Mountains (The Crimean Peninsula)." Land 11, no. 12 (2022): 2121. http://dx.doi.org/10.3390/land11122121.

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The territory of the Crimean Peninsula is extensively subject to economic activities. In this connection, there is an ever-increasing impact on the environment. The present paper presents an analysis of the transformation of the area of the largest river basins of the northwestern slope of the Crimean Mountains (basins of the Zapadnyy Bulganak, Alma, Kacha, Belbek, and Chernaya rivers). For this purpose, various indicators characterizing the transformation of the area were calculated: coefficient of anthropogenic transformation; land degradation index; urbanity index; level of anthropogenic tr

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13

Anonymous. "River basin administration." Eos, Transactions American Geophysical Union 70, no. 48 (1989): 1515. http://dx.doi.org/10.1029/89eo00374.

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14

Arkhawan J. Sh., R. N. Dara, M.A. Chnaray, A. R. Ahmed, and H.S. Khoshnaw. "HYDROCHEMICAL STUDY OF BALAK RIVER, ERBIL-IRAQ." IRAQI JOURNAL OF AGRICULTURAL SCIENCES 55, no. 5 (2024): 1743–55. http://dx.doi.org/10.36103/mrsdd983.

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This study was aimed to assess the water quality of different water resources (Surface water, subsurface in water, and groundwater) across the Balak river basin. Twenty two different water resource samples were collected and subjecting to a comprehensive physicochemical analysis. Balak river basin, situated in Erbil governorate, Iraq, it is located 10 km to the east from Bekhal Waterfall. Five attributers combine with Balak River within the basin areas which are: Rezanok Sub River, Balakiyan Sub River, Basan Sub River, Roste Sub River, and Alana Sub River. The hydro chemical study of all water

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15

Tambe, Devidas, and Rumana Khan. "Qualitative assessment of the Land surface parameters of Adula River Basin and Mahalungi River Basin." International Journal of Advance and Applied Research 6, no. 25 (2025): 108–13. https://doi.org/10.5281/zenodo.15293976.

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<strong>Abstract:</strong> Qualitative analyses of the land surface parameters give information on the development and evaluation of the landscape. It also provides understating on the hydrological behavior of the basing and the ruggedness of the terrain. Most of the land surface parameters are effective for quantitative assessment but some can be effective to the qualitative assessment. In this study contour, curvature and hillshade are selected as a qualitative description to Adula and Mahalungi river basin. A 30-meter spatial resolution Cartosat-1 freely available DEM data is used for the o

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16

Kyryliuk, Serhii. "The assessment algorithm for sustainable development goals in the Hukiv, Dereluy, and Vyzhenka river basin systems of Chernivtsi oblast." Present Environment and Sustainable Development 15, no. 2 (2021): 235–44. http://dx.doi.org/10.15551/pesd2021152019.

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The study deals with an integral assessment of hydromorphological and geoecological conditions of the Hukiv (flatland type of river), Dereluy (foothill type of river), and Vyzhenka (mountainous type of river) river basin systems (Figure 1). The indicators characterizing the river basin in the best way as a holistic system, the channel, floodplain, and watershed altogether, in natural reference conditions and in terms of human economic activity are addressed. The assessment hydromorphological test and geoecological monitoring of small rivers (SWOT-analysis) in accordance with the developed univ

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17

AL-Mahmood, Hassan K. H. "Hydrological changes in the lower part of Mesopotamian Basin." Iraqi Journal of Aquaculture 12, no. 1 (2021): 47–70. http://dx.doi.org/10.58629/ijaq.v12i1.128.

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This study was examined the hydrological changes in the water ways for the and the marshes associated with them in Southern part of lower Mesopotamian catchment area (Tigris and Euphrates Rivers and their branches in Amarah, Nasiriyah and Basra ) and the main tributaries of the Shatt al-Arab River( Swaib, Garmat Ali and Karun ), and the significant changes in the overall hydrological conditions of water discharge and water quality. Water discharge and water samples were collected quarterly for four sites during 2011, the laboratory analysis were performed to determine physical and chemical cha

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18

Zhukov, Ivan A., and Denis N. Aybulatov. "Changes in the annual runoff module of small rivers in the Russian part of the Ural River basin." Water Sector of Russia: Problems, Technologies, Management 2025, no. 2 (2025): 72–89. https://doi.org/10.35567/19994508-2025-2-72-89.

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Relevance. Currently, the main studies of the runoff modulus and the dynamics of its changes are conducted mainly on medium and large rivers of the Russian part of the Ural River basin, while the study of the runoff modulus of small rivers in this basin is extremely poor. Given the increasing deterioration of the ecological state of rivers, which primarily affects the annual water runoff modulus on small rivers, the study of the processes of runoff modulus formation, its variability and intra-annual changes are becoming the most important task of hydrology. Methods. The study is based on a com

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19

Tursunova, Aisulu Alashevna, S. K. Alimkulov, Akhan Bakhytovich Myrzakhmetov, M. A. Kanay, Aizhan Zh Dostaeva, and Gulmira Isakan. "Basic hydrographic information about the rivers and temporary watercourses of the Balkash-Alakol basin." Bulletin of the Karaganda University. “Biology, medicine, geography Series” 109, no. 1 (2023): 195–205. http://dx.doi.org/10.31489/2023bmg1/195-205.

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The article presents basic information about the state of the river network in the Balkash-Alakol basin. They consist of a list of rivers and temporary watercourses from 5 km in mountainous areas and from 10 km in lowland areas, and also include information on their main morphological and morphometric characteristics, which were presented only in the 1970s, after the 1970s such extensive research has not been done. The purpose of the study is to identify rivers and temporary streams, as well as to obtain basic hydrographic information through field surveys and with the help of modern GIS techn

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20

House, M. A. "River Basin Management in the UK." Water Science and Technology 23, no. 1-3 (1991): 57–64. http://dx.doi.org/10.2166/wst.1991.0401.

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The Water Act 1989 has resulted in the reorganisation of the system of River Basin Management which has operated in England and Wales since the establishment of the 10 Water Authorities in 1974. On 1st September 1989 the Water Authorities were re-structured to produce 10 Water Service Companies and a new regulatory body, the National Rivers Authority. This presentation will summarise the changes to River Basin Management in England and Wales resulting from this reorganisation.

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21

Devercelli, Melina, and Yolanda Zalocar de Domitrovic. "Phytoplankton of the Paraná River Basin." Advances in Limnology 65 (July 7, 2014): 39–65. http://dx.doi.org/10.1127/1612-166x/2014/0065-0033.

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22

Rios, Natalia Noemí, Carla Ginesta Torcivia, Maria Romina Onorato, Valeria Cortez Taillant, and María Yanina Esper Angillieri. "Morfometría de una cuenca de los Andes Centrales, San Juan, Argentina: evaluación de los factores condicionantes del terreno a la ocurrencia de aluviones." Andean Geology 51, no. 1 (2024): 194. http://dx.doi.org/10.5027/andgeov51n1-3441.

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The present work aims to determine flash flood occurrence prone areas, in the Jáchal river basin, San Juan Province, Argentina. The Jáchal river basin covers ~29,000 km2 and has a perimeter of ~2,400 km, while the eponymous river extends for nearly 570 km. It is a 7th order basin according to Strahler’s classification, subdivided into four 6th order sub-basins. Various morphometric basin characteristics are analysed and some basic and derived parameters are calculated. These calculations allow predicting the basin behaviour due to heavy rainfall, which translates into large volumes of water wi

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MAKAR'EVA, O. M., N. V. NESTEROVA, V. R. ALEKSEEV, A. N. SHIKHOV, A. A. ZEMLYANSKOVA, and A. A. OSTASHOV. "ESTIMATION OF AUFEIS RESOURCES IN THE INDIGIRKA RIVER BASIN." Meteorologiya i Gidrologiya, no. 3 (March 2022): 81–90. http://dx.doi.org/10.52002/0130-2906-2022-3-81-90.

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On the basis of corrected Landsat data for 2013-2017, a modern assessment of aufeis in the Indigirka River basin and its partial catchments with an area of 1830 to 305 000 km2 was conducted. The potential contribution of the aufeis flow to the formation of the water balance of rivers during various phases of hydrological regime was calculated. During the phase of the maximum development, the aufeis area of partial catchments ranges from 0.30 to 1.49%, reaching 0.54% of the total area of the Indigirka River basin. The aufeis resources (water content in aufeis) of the Indigirka River basin are 1

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24

Sim, Lay, Akio Onishi, Olivier Gervais, and Ngai Chan. "Comparative Research on River Basin Management in the Sagami River Basin (Japan) and the Muda River Basin (Malaysia)." Resources 7, no. 2 (2018): 33. http://dx.doi.org/10.3390/resources7020033.

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25

Zou, Yiqian, Ling Liu, Yanhua Jiang, and Chenjun Yang. "Research on the Gradient of Aquatic Ecological Integrity of Phytoplankton in Regional River Segments of Jiangsu Province and Its Driving Mechanism." Water 17, no. 11 (2025): 1645. https://doi.org/10.3390/w17111645.

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To study the structure and distribution characteristics of the phytoplankton community in the Huaihe River Basin, Yangtze River Basin, and Taihu Lake Basin in Jiangsu Province, 126 sampling sites were set up in 35 rivers in the region, and samples were collected during the wet season (August–September) in 2023. Based on the monitoring results of phytoplankton, the study selected 20 candidate indicators and conducted range screening, discriminative ability analysis, and correlation analysis. Finally, seven core indicators were determined to construct the Phytoplankton Biological Integrity Index

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26

Ahmadi, Jamshid. "Dynamic Geomorphology of the Amu Darya Basin in Afghanistan: A Study of Physiography, Basin Erosion, and Channel Development." Sprin Journal of Arts, Humanities and Social Sciences 3, no. 5 (2024): 48–52. http://dx.doi.org/10.55559/sjahss.v3i5.313.

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The morphological dynamics of rivers are motivated by way of a number of things, including floodplain sedimentation, channel migration, sediment transport, and hydrodynamics. A considerable information of the complicated dynamics of river structures is important to layout river initiatives which can be sustainable and environmentally conscious. Implementing thorough river control plans that include hydraulic infrastructure and ecological restoration projects is important to overcoming these boundaries. This solution will effectively manipulate competing needs for water resources whilst ensurin

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Yuriev, A. L., V. P. Samusenok, A. I. Vokin, G. B. Hludnev, and A. N. Matveev. "Biology of Perch in Upper Lena Basin." Bulletin of Irkutsk State University. Series Biology. Ecology 43 (2023): 16–38. http://dx.doi.org/10.26516/2073-3372.2023.43.16.

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Lena River is the largest watercourse in Eastern Siberia. The upper reaches of the river, 1600 km long, starts from the source to the mouth of the Vitim River. We collected data on perch biology in different seasons: in the Lena River in the section from the mouth of the Tutura River (right tributary 3,812 km from the mouth) to the mouth of the Ichora River (left tributary 2,973 km from the mouth) in different seasons from 2007 to 2022; in the Kuta 10-km section from 10 to 20 km from the river mouth in August 2011; Kirenga River from the mouth of the Marekta Brook (400 km from the mouth) to th

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BRAGA, B. P. F., and J. G. LOTUFO. "Integrated River Basin Plan in Practice: The São Francisco River Basin." International Journal of Water Resources Development 24, no. 1 (2008): 37–60. http://dx.doi.org/10.1080/07900620701722978.

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Boenigk, W. "The Pleistocene drainage pattern in the Lower Rhine Basin." Netherlands Journal of Geosciences - Geologie en Mijnbouw 81, no. 2 (2002): 201–9. http://dx.doi.org/10.1017/s0016774600022447.

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AbstractDuring the Pleistocene the drainage pattern in the Lower Rhine Basin changed twice, from a flooding of the whole basin by the river Rhine from SW to NE to an influence restricted to the NE only.The first dominance of the river Rhine is documented from the Reuverian to the Tiglian, the second one in the Cromerian. In between this time, the Meuse River drained the central Lower Rhine Basin in NE direction. For the sediments of that river, the term ‘Holzweiler Formation’ is introduced. Since the Late Cromerian, the influence of the Rhine is again restricted to the NE of the Lower Rhine Ba

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Bazarbayeva, T. A., B. D. Rakhyshova, and A. A. Oshakbay. "ECOLOGICAL STATE OF THE ILI BASIN GEOSYSTEMS." Chemical Journal of Kazakhstan 74, no. 2 (2021): 78–85. http://dx.doi.org/10.51580/2021-1/2710-1185.30.

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The article considers the geo-ecological situation of the Ili basin. The definition of the physical and geographical location, topography, soil and vegetation of the region was given. It was determined that the management of the efficient use of water resources in the Ili river basin depends primarily on the water resources of the rivers entering the basin and the level of Lake Balkhash. Factors determining the spring flow of the Ili River are shown. Due to the development of the middle reaches of the Ili River, the whole river ecosystem, rice fields and shangel massifs, excessive use of miner

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Vukić, Jasna, Kristýna Eliášová, Dario Marić, and Radek Šanda. "Occurrence of alien spirlin (Alburnoidessp.) in the Neretva river basin." Knowledge & Management of Aquatic Ecosystems, no. 420 (2019): 15. http://dx.doi.org/10.1051/kmae/2019007.

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Northern Mediterranean region is characterised by an exceptional richness of the freshwater ichthyofauna. Many fish species of this region are endemic to a single or a few river basins. This is also the case of the Neretva river basin (Adriatic Sea slope), where 17 out of 34 native species are endemic solely to this river basin. However, these unique Mediterranean freshwater ecosystems are fragile and are susceptible to human-induced changes, including introduction of alien fish species. We report here a finding of the 32ndalien fish species in the Neretva river basin, spirlinAlburnoidessp., w

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Mina, Hushyar Ibrahim, Pshtiwan Ali Mohmmed, Yadgar Mustafa Ibrahim, and Pshtiwan Shfeeq Ahmed. "The analysis Hydromorphometric Watershed Barsool Basin." Journal of University of Raparin 10, no. 2 (2023): 739–72. http://dx.doi.org/10.26750/vol(10).no(2).paper31.

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The Barsool River watershed is one of the branches of the lower Zab River in the Pishdar district. It flows into the lower Zab River about 100 meters southwest of Kawiya village. It is located between the latitudes (o36 07" 14'-o36 12" 00’) of North and longitudes (o45 "09 '51-o45 "19 '22) of East. The main source of this river is located in the Kurdistan Region, in the Pishdar district. The source of water for this river is located in the valley of Beklo, Gira, Dega, Badinbal, and Darashman villages. The main goal of the study is to introduce the environmental characteristics of the study are

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Suykens, Cathy. "Critical Success Factors in Transboundary Water Management: a US-EU Comparison." European Energy and Environmental Law Review 27, Issue 1 (2018): 2–14. http://dx.doi.org/10.54648/eelr2018001.

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In light of the increasing pressure on freshwater resources, good governance of rivers is key in meeting the challenges ahead. Integrated river basin management has been advocated both in the European Union and the United States. This paper will adopt a comparative approach to the analysis of river basin management by scrutinizing the legal regimes governing the Scheldt River in the EU and the Delaware River in the US. Based on these case studies, in combination with literature review, the article will set forth Critical Success Factors for integrated transboundary river basin management.

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Hu, Chenpeng, Ziqi Liu, Kangning Xiong, Xiaoxi Lyu, Yuan Li, and Renkai Zhang. "Characteristics of and Influencing Factors of Hydrochemistry and Carbon/Nitrogen Variation in the Huangzhouhe River Basin, a World Natural Heritage Site." International Journal of Environmental Research and Public Health 18, no. 24 (2021): 13169. http://dx.doi.org/10.3390/ijerph182413169.

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In karst areas, the characteristics of water chemistry and carbon and nitrogen are of great significance to basic research. The contents of Ca2+, Mg2+, K+, Na+, HCO3−, SO42−, NO3−, Cl−, dissolved organic carbon (DOC), and total nitrogen (TN) in water samples from 18 rivers and 14 springs in the Huangzhouhe River Basin were determined. The results showed that the water chemistry type in the Huangzhouhe River Basin is HCO3-Ca-Mg. The chemical composition is mainly affected by dolomite weathering and also by ion exchange and other human activities. The river and spring DIC remain at the same leve

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Rybak, Nazar, and Lidiya Dubis. "FEATURES OF RIVER CONFLUENCE NODE FUNCTIONING IN THE SUKIL RIVER BASIN." SCIENTIFIC ISSUES OF TERNOPIL VOLODYMYR HNATIUK NATIONAL PEDAGOGICAL UNIVERSITY. SERIES: GEOGRAPHY 57, no. 2 (2024): 37–46. https://doi.org/10.25128/2519-4577.24.2.5.

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The article studies three largest confluences of rivers in the Sukil basin for 1880-2021 period. The morphodynamic types of confluences have been determined, and the analysis of their displacements has been conducted; influence of the geological and geomorphological structure on the patterns of their functioning has been determined. Key words: river confluence, functioning, morphodynamics, the Sukil river, river channel.

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Bharati, Smt. Sangita Subhash. "A Geographical Study of Drainage Pattern in Chhatrapati Sambhajinagar District." International Journal of Advance and Applied Research 11, no. 5 (2024): 483–86. https://doi.org/10.5281/zenodo.14676848.

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<strong>Introduction:</strong> Chhatrapati Sambhajinagar district falls in the basin of Godavari and Tapi rivers and all the other rivers in Tapi basin of the district are small except Vaghur river.  River Godavari, also known as the South Ganga, is the largest major river in Maharashtra and Chhatrapati Sambhajinagar district.  The source of this river is at Brahmagiri near Trimbakeshwar in Nashik district.  This river enters Vaijapur taluka of Chhatrapati Sambhajinagar district from Nashik and Ahmednagar districts and flows across the border at most places in Vaijapur, Gangapur

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37

Bharati, Smt. Sangita Subhash. "A Geographical Study of Drainage Pattern in Chhatrapati Sambhajinagar District." International Journal of Advance and Applied Research 11, no. 5 (2024): 488–91. https://doi.org/10.5281/zenodo.14747705.

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<strong>Introduction:</strong> Chhatrapati Sambhajinagar district falls in the basin of Godavari and Tapi rivers and all the other rivers in Tapi basin of the district are small except Vaghur river.  River Godavari, also known as the South Ganga, is the largest major river in Maharashtra and Chhatrapati Sambhajinagar district.  The source of this river is at Brahmagiri near Trimbakeshwar in Nashik district.  This river enters Vaijapur taluka of Chhatrapati Sambhajinagar district from Nashik and Ahmednagar districts and flows across the border at most places in Vaijapur, Gangapur

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38

Dagosta, Fernando C. P., Murilo N. L. Pastana, and André L. H. Esguícero. "New records of fishes (Actinopterygii: Ostariophysi) from the Upper Tapajós River Basin." Check List 8, no. 3 (2012): 592. http://dx.doi.org/10.15560/8.3.592.

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The first report of Sartor (Anostomidae) and Tatia intermedia (Auchenipteridae) for the Upper Tapajós River Basin are presented here. Sartor is very rare on collections, and is reported only from the Trombetas, Tocantins and Upper Xingu river basins. Tatia intermedia is registered in the upper reaches of the Araguaia, Tocantins, Xingu, and Capim rivers, tributaries of the lower Amazon River in Brazil, northwards to the Suriname coastal rivers and the Essequibo River in Guyana.

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Li, Xiaoning, Chuanhai Wang, Gang Chen, Xing Fang, Pingnan Zhang, and Wenjuan Hua. "Distributed-Framework Basin Modeling System: Ⅲ. Hydraulic Modeling System." Water 13, no. 5 (2021): 649. http://dx.doi.org/10.3390/w13050649.

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A distributed-framework basin modeling system (DFBMS) was developed to simulate the runoff generation and movement on a basin scale. This study is part of a series of papers on DFBMS that focuses on the hydraulic calculation methods in runoff concentration on underlying surfaces and flow movement in river networks and lakes. This paper introduces the distributed-framework river modeling system (DF-RMS) that is a professional modeling system for hydraulic modeling. The DF-RMS contains different hydrological feature units (HFUs) to simulate the runoff movement through a system of rivers, storage

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40

Lombardo, Umberto. "Alluvial plain dynamics in the southern Amazonian foreland basin." Earth System Dynamics 7, no. 2 (2016): 453–67. http://dx.doi.org/10.5194/esd-7-453-2016.

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Abstract. Alluvial plains are formed with sediments that rivers deposit on the adjacent flood-basin, mainly through crevasse splays and avulsions. These result from a combination of processes, some of which push the river towards the crevasse threshold, while others act as triggers. Based on the floodplain sedimentation patterns of large rivers in the southern Amazonian foreland basin, it has been suggested that alluvial plain sediment accumulation is primarily the result of river crevasse splays and sheet sands triggered by above-normal precipitation events due to La Niña. However, more than

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41

Lombardo, U. "Alluvial plain dynamics in the southern Amazonian foreland basin." Earth System Dynamics Discussions 6, no. 2 (2015): 2063–100. http://dx.doi.org/10.5194/esdd-6-2063-2015.

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Abstract. Alluvial plains are formed with sediments that rivers deposit on the adjacent flood-basin, mainly through crevasse splays and avulsions. These result from a combination of processes, some of which push the river towards the crevasse threshold, while others act as triggers. Based on the floodplain sedimentation patterns of large rivers in the southern Amazonian foreland basin, it has been suggested that alluvial plain sediment accumulation is primarily the result of river crevasse splays triggered by above normal precipitation events due to La Niña. However, more than 90 % of the Amaz

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42

Sukhyj, P., and I. Berezka. "The climatic conditions of the drainage and surface water regime Upper Siret river basin." Visnyk of the Lviv University. Series Geography, no. 46 (December 26, 2013): 348–55. http://dx.doi.org/10.30970/vgg.2013.46.1501.

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A study of climate Siret River Basin within the Chernivtsi region. Designated hydrographic and hydrometric characteristics of rivers. The relationship between climatic conditions and the hydrographic network and the regime of surface water basin of the Upper Siret. Key words: river basin; climate; surface water; hydrological regime.

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43

Alfaro, Aldi, SB Soeryamassoeka, Danang Gunarto, Umar Umar, and Eko Yulianto. "FLOOD MANAGEMENT STRATEGY IN THE LANDAK SUB-RIVER BASIN USING SWOT ANALYSIS." Jurnal Teknik Sipil 23, no. 1 (2023): 93. http://dx.doi.org/10.26418/jtst.v23i1.61790.

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The Landak sub-River Basin is part of the Kapuas River Basin which is drained by the Landak River with an area of approximately 7,921 km2. Flooding in the Landak sub-River Basin occurs every year with the number of cases tending to increase. Flooding in the Landak sub-River Basin inundates about 20 villages, which means that flood-prone areas dominate. The causes of flooding in the Landak sub-River Basin are very complex, basically caused by natural and non-natural factors. Specifically, there are many problems in the Landak sub-River Basin that are thought to trigger flooding such as land use

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44

Petersen-Perlman, Jacob D. "Projecting River Basin Resilience in the Zambezi River Basin through Global Analyses and Basin Realities." Water Resources Management 30, no. 6 (2016): 1987–2003. http://dx.doi.org/10.1007/s11269-016-1264-3.

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45

Dagosta, Fernando, Murilo Pastana, and André Esguícero. "New records of fishes (Actinopterygii: Ostariophysi) from the Upper Tapajós River Basin." Check List 8, no. (3) (2012): 592–94. https://doi.org/10.15560/8.3.592.

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The first report of <em>Sartor </em>(Anostomidae) and <em>Tatia intermedia </em>(Auchenipteridae) for the Upper Tapajós River Basin are presented here. <em>Sartor </em>is very rare on collections, and is reported only from the Trombetas, Tocantins and Upper Xingu river basins. <em>Tatia intermedia </em>is registered in the upper reaches of the Araguaia, Tocantins, Xingu, and Capim rivers, tributaries of the lower Amazon River in Brazil, northwards to the Suriname coastal rivers and the Essequibo River in Guyana.

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46

Bukovskiy, Mikhail, Kirill Kuzmin, Maria Chernova, and Elena Vishniakova. "The structure of the Karay river basin by the longitudinal slopes of the river beds and the average gradients of water catchments slopes." E3S Web of Conferences 163 (2020): 06002. http://dx.doi.org/10.1051/e3sconf/202016306002.

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The problems of water lag time during flood forecasting, the rate of pollution spreading over the basin area in the event of industrial accidents, the transport of suspended and dissolved substances by rivers, and planning of erosion control measures are very relevant today. Within the framework of the basin approach, an elementary water catchment can be adopted as an elementary unit for the analysis of a particular territory. At the same time, river bed slopes determine the power of the water flow, and the average slopes of water catchments significantly affect the formation of river flow, th

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47

Zhovnir, V., and Vasyl Grebin. "Estimation of hydro-hydrochemical exploration of the basin Southern Bug." Physical Geography and Geomorphology 90, no. 2 (2018): 50–58. http://dx.doi.org/10.17721/phgg.2018.2.05.

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The history of the development of the hydrometric network within the basin of the Southern Bug from the end of the nineteenth century to today is considered. The Southern Bug basin is among the well-studied hydrologically, although instrumental hydrological observations on the river began later than other large Ukrainian rivers. The interest of scientists and practitioners for a long time was limited only to the study of the lower section of the river, suitable for navigation. The presence of thresholds and fluctuations along the river and its inflows, on the one hand, prevented the developmen

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48

Sekine, M., M. Ukita, and H. Nakanishi. "Systematic Pollutegraph Simulation for Real Scale River Basin." Water Science and Technology 23, no. 1-3 (1991): 141–50. http://dx.doi.org/10.2166/wst.1991.0410.

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This study describes the model for predicting the run-off load of pollutants through rivers into eutrophic lakes and inner sea areas. The model is composed of three stages: discharged load prediction; flow-rate prediction; and run-off load prediction. The discharged load in the river basin is estimated by using a pollutant loading factor method. The flow-rate which is necessary for the formula to predict the run-off load, was obtained by a tank model method. The run-off load prediction process consists of two stages: flow-out stage and flow-down stage. The flow-out stage represents the process

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49

Volchak, Alexander, Sergey Parfomuk, and Svetlana Sidak. "Intra-annual Runoff Distribution in the Pripyat River Basin." E3S Web of Conferences 212 (2020): 01016. http://dx.doi.org/10.1051/e3sconf/202021201016.

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The time variability features of the intra-annual runoff distribution in the Pripyat River basin at the present stage are considered. The study used data from 10 active gauging-stations at the basin area for the period of enabled observations. Changes in the nature of natural runoff regulation of rivers are shown. An increase in the coefficient of natural runoff regulation after the period 1970-1983 for the rivers of the Pripyat River basin was revealed. The relationship between the coefficient of uneven runoff and the share of spring flood was established.

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Сидорчук, А. Ю., О. К. Борисова, and А. В. Панин. "PALEOHYDROLOGY OF RIVERS IN THE DON RIVER BASIN." Гидросфера. Опасные процессы и явления 2, no. 5 (2024): 172–90. http://dx.doi.org/10.34753/hs.2023.5.2.172.

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На основе морфометрии палеорусел реконструирован гидрологический режим крупных меандрирующих рек, существовавших в бассейне реки Дон 18–14 тыс. лет назад. Для палеогидрологических реконструкций применялся метод морфометрических зависимостей, полученных на основе гидравлической геометрии речных русел – связи между шириной русла и средним максимальным расходом воды и отношения между максимальным расходом половодья и площадью водосбора. Реконструированные палеовеличины максимального суточного слоя поверхностного стока в период снеготаяния составили на севере бассейна р. Дон, в перигляциальной лес

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