nach oben

Sustainable Water Resources Management

Erschienen in:

01.02.2024 | Original Article

Decreasing trends of downstream channel width: a comprehensive review of the scientific literature

verfasst von: Sadhan Malik, Subodh Chandra Pal, Abu Reza Md. Towfiqul Islam

Erschienen in: Sustainable Water Resources Management | Ausgabe 1/2024

Einloggen

Aktivieren Sie unsere intelligente Suche, um passende Fachinhalte oder Patente zu finden.

search-config

KI-gestützte Suche

Aus

Abstract

Reduction of channel width and area without major anthropogenic intervention has been a topic of interest in geomorphology as identified by some earlier studies, indicating contradictory phenomena in relation to the widely accepted downstream increases in channel width and area. However, there is limited knowledge regarding the downstream reduction of bankfull channel area and width (DRBCWA) in the absence of major anthropogenic factors in the existing scientific literature. Therefore, the current study presents a comprehensive review of downstream decreasing channel width and channel area in response to natural factors. In this study, synthesis methods were followed to achieve our goal. A significant amount of literature was systematically surveyed, and data related to downstream variations in channel size were compared and analyzed to fulfil our objective. This study found that DRBCWA is not limited to a particular climatic and geo-environmental setup; rather, it has been observed across a range of climates, including temperate maritime climates, arid zones, semiarid climates, and hyper-arid areas and over monsoon-dominated regions. Here, the loss of water from the channel in wide floodplain regions with cohesive bank materials and the lowering of sea level are found to be the key driving factors responsible for the reduction of channel width and capacity downstream.

Vorheriger Artikel Water market auctioning method in the Sultanate of Oman: Islamic principles of three aflaj case study in Northern Oman

Nächster Artikel Groundwater potential identification in Temcha catchment, Upper Blue Nile Basin, Ethiopia

Sie haben noch keine Lizenz? Dann Informieren Sie sich jetzt über unsere Produkte:

Springer Professional "Wirtschaft+Technik"

Online-Abonnement

Mit Springer Professional "Wirtschaft+Technik" erhalten Sie Zugriff auf:

über 102.000 Bücher
über 537 Zeitschriften

aus folgenden Fachgebieten:

Automobil + Motoren
Bauwesen + Immobilien
Business IT + Informatik
Elektrotechnik + Elektronik
Energie + Nachhaltigkeit
Finance + Banking
Management + Führung
Marketing + Vertrieb
Maschinenbau + Werkstoffe
Versicherung + Risiko

Jetzt Wissensvorsprung sichern!

Jetzt informieren

Springer Professional "Technik"

Online-Abonnement

Mit Springer Professional "Technik" erhalten Sie Zugriff auf:

über 67.000 Bücher
über 390 Zeitschriften

aus folgenden Fachgebieten:

Automobil + Motoren
Bauwesen + Immobilien
Business IT + Informatik
Elektrotechnik + Elektronik
Energie + Nachhaltigkeit
Maschinenbau + Werkstoffe

Jetzt Wissensvorsprung sichern!

Jetzt informieren

Akhter S, Eibek KU, Islam S, Islam ARMT, Shen S, Chu R (2019) Predicting spatiotemporal changes of channel morphology in the reach of Teesta River Bangladesh Using GIS and ARIMA Modeling. Quat Int 513:80–94. https://doi.org/10.1016/j.quaint.2019.01.022CrossRef

Allen JRL (1965) A review of the origin and characteristics of recent alluvial sediments. Sedimentology 5:89–191. https://doi.org/10.1111/j.1365-3091.1965.tb01561.xADSCrossRef

Allison MA, Demas CR, Ebersole BA, Kleiss BA et al (2012) A water and sediment budget for the lower Mississippi-Atchafalaya River in flood years 2008–2010: implications for sediment discharge to the oceans and coastal restoration in Louisiana. J Hydrol 432:84–97CrossRef

Allmendinger NE, Pizzuto JE, Potter N et al (2005) The influence of riparian vegetation on stream width, eastern Pennsylvania, USA. Bull Geol Soc Am. https://doi.org/10.1130/B25447.1CrossRef

Andrews ED (1984) Bed-material entrainment and hydraulic geometry of gravel-bed rivers in colorado. Bull Geol Soc Am 95:371–378. https://doi.org/10.1130/0016-7606(1984)95%3c371:BEAHGO%3e2.0.CO;2CrossRef

Anderson RJ, Bledsoe BP, Hession WC (2004) Width of streams and rivers in response to vegetation, bank material, and other factors. J Am Water Resour Assoc 40:1159–1172. https://doi.org/10.1111/j.1752-1688.2004.tb01576.xCrossRef

Annayat W, Sil BS (2020) Assessing channel morphology and prediction of centerline channel migration of the Barak River using geospatial techniques. Bull Eng Geol Env. https://doi.org/10.1007/s10064-020-01894-9CrossRef

ASCE Task Committee (1998) River width adjustment. J Hydraul Eng 124:881–902CrossRef

Bandyopadhyay S, Kar NS, Das S, Sen J (2014) River systems and water resources of west bengal : a review. Geol Soc India Spec Publ 3:63–84. https://doi.org/10.17491/cgsi/0/v0i0/62893CrossRef

Benson MA, Thomas DM (1966) A definition of dominant discharge. Int Assoc Sci Hydrol Bull 11:76–80. https://doi.org/10.1080/02626666609493460CrossRef

Bhattacharyya A (2013) Evaluation of hydro-geonomic characteristics of flood in the Mayurakshi river basin of eastern India. Department of Geography, Visva-Bharati

Blum MD, Törnqvist TE (2000) Fluvial responses to climate and sea-level change: a review and look forward. Sedimentology 47:2–48CrossRef

Bowman D, Svoray T, Devora S et al (2010) Extreme rates of channel incision and shape evolution in response to a continuous, rapid base-level fall, the Dead Sea, Israel. Geomorphology 114:227–237. https://doi.org/10.1016/J.GEOMORPH.2009.07.004ADSCrossRef

Boyd R, Dalrymple R, Zaitlin BA (1992) Classification of clastic coastal depositional environments. Sediment Geol 80:139–150. https://doi.org/10.1016/0037-0738(92)90037-RADSCrossRef

Bradley C, Smith DG (1984) Meandering channel response to altered flow regime: Milk River, Alberta and Montana. Water Resour Res 20:1913–1920. https://doi.org/10.1029/WR020i012p01913ADSCrossRef

Bridge JS (2003) Rivers and floodplains: forms, processes, and sedimentary record: rivers and floodplains: forms, processes, and sedimentary record. Blackwell Publication, Oxford, Malden

Bridge JS, Smith ND, Trent F, Gabel SL, Bernstein P (1986) Sedimentology and morphology of a low-sinuosity river: calamus River, Nebraska Sand Hills. Sedimentology 33:851–870. https://doi.org/10.1111/j.1365-3091.1986.tb00987.xADSCrossRef

Burnett AW, Schumm SA (1983) Alluvial-River response to neotectonic deformation in Louisiana and Mississippi. Science (80–) 222:49–50. https://doi.org/10.1126/science.222.4619.49ADSCrossRef

Cadol D, Rathburn SL, Cooper DJ (2011) Aerial photographic analysis of channel narrowing and vegetation expansion in Canyon De Chelly National Monument, Arizona, USA, 1935–2004. River Res Appl 27:841–856. https://doi.org/10.1002/rra.1399CrossRef

Cattaneo A, Steel RJ (2003) Transgressive deposits: a review of their variability. Earth Sci Rev 62:187–228. https://doi.org/10.1016/S0012-8252(02)00134-4ADSCrossRef

Chakrabarti B (1985) A Geomorphological analysis of mayurakshi river basin. Department of Geography, The University of Burdwan, Shodhganga@INFLIBNET

Chakraborty A (2010) Suffering with the river: floods, social transition and local communities in the Ajoy river basin in West Bengal, India. Ritsumeikan J Asia Pacific Stud 27:125–138

Chapman GP, Rudra K (2007) Water as Foe, Water as friend: lessons from bengal’s millennium flood. J South Asian Dev 2:19–49. https://doi.org/10.1177/097317410600200102CrossRef

Chapman PG, Rudra K (2016) Time streams : history and rivers in bengal. member secretary centre for archaeological studies and training, Eastern India (An Autonomous Institution of the Govternment of West Bengal), Kolkata

Charlton FG, Brown PM, Benson RW (1978) The hydraulic geometry of some gravel rivers in Britain

D’Alpaos A, Lanzoni S, Mudd SM, Fagherazzi S (2006) Modeling the influence of hydroperiod and vegetation on the cross-sectional formation of tidal channels. Estuar Coast Shelf Sci. https://doi.org/10.1016/j.ecss.2006.05.002CrossRef

De Rose RC, Stewardson MJ, Harman C (2008) Downstream hydraulic geometry of rivers in Victoria, Australia. Geomorphology 99:302–316. https://doi.org/10.1016/j.geomorph.2007.11.008ADSCrossRef

DoIW-GoWB (2014) Annual flood report, 2013: irrigation and waterways directorate Govt. of West Bengal, india. Kolkata

DoIW-GoWB (2015) Annual flood report, 2014: irrigation and Waterways Directorate Govt. of West Bengal, India. Kolkata

DoIW-GoWB (2016) Annual flood report, 2015: irrigation and waterways directorate Govt. of West Bengal, india. Kolkata

Dunaway D, Swanson SR, Wendel J, Clary W (1994) The effect of herbaceous plant communities and soil textures on particle erosion of alluvial streambanks. Geomorphology 9:47–56. https://doi.org/10.1016/0169-555X(94)90030-2ADSCrossRef

Dunkerley D (1992) Channel geometry, bed material and inferred flow conditions in ephemeral stream systems, Barrier Range, Western NSW. Aust Hydrol Process 6:417–433ADSCrossRef

Dunkerly DL (2008) Bank permeability in an Australian ephemeral dry-land stream: variation with stage resulting from mud deposition and sediment clogging. Earth Surf Process Landforms 33:226–2443ADSCrossRef

Dury GH (1958) Tests of a general theory of misfit streams. Trans Pap Institute Br Geogr. https://doi.org/10.2307/621181CrossRef

Dury GH (1965) Principles of underfit streams: general Theories of Meandering Valleys. United States Government Printing Office, Washington, DC

Dury GH (1976) Discharge prediction, present and former, from channel dimensions. J Hydrol 30:219–245. https://doi.org/10.1016/0022-1694(76)90102-5CrossRef

Dury GH (1984) Abrupt variation in channel width along part of the River Severn, near Shrewsbury, Shropshire, England. Earth Surf Process Landforms 9:485–492. https://doi.org/10.1002/esp.3290090509ADSCrossRef

Eaton BC, Giles TR (2009) Assessing the effect of vegetation-related bank strength on channel morphology and stability in gravel-bed streams using numerical models. Earth Surf Process Landforms 34:712–724. https://doi.org/10.1002/esp.1768ADSCrossRef

Egger G, Ferreira MT, Rivaes R, et al (2013) Riparian vegetation responses to altered flow regimes driven by climate change in Mediterranean rivers Riparian vegetation responses to altered fl ow regimes driven by climate change in Mediterranean rivers.https://doi.org/10.1002/eco.1287

Fashae O, Olusola AO (2017) Landuse types within channel corridor and river channel morphology of River Ona, Ibadan, Nigeria. Indones J Geogr. https://doi.org/10.22146/IJG.12738CrossRef

Fashae O, Olusola A, Faniran A (2018) Environmental factors and pattern of riparian vegetation along the downstream sections of the Lower Ogun River, Nigeria. Singap J Trop Geogr 39:215–223. https://doi.org/10.1111/sjtg.12235CrossRef

Ferguson R, Ashworth P (1991) Slope-induced changes in channel character along a gravel-bed stream: the Allt Dubhaig, Scotland. Earth Surf Process Landforms 16:65–82. https://doi.org/10.1002/esp.3290160108ADSCrossRef

Finnegan NJ, Roe G, Montgomery DR, Hallet B (2005) Controls on the channel width of rivers: implications for modeling fluvial incision of bedrock. Geology 33:229–232. https://doi.org/10.1130/G21171.1ADSCrossRef

Frederikse T, Landerer F, Caron L, Adhikari S et al (2020) The causes of sea-level rise since 1900. Nature 584(7821):393–397CrossRefPubMed

Friedman GM, Osterkamp W, Lewis WJ (1996a) The role of vegetation and bed-level fluctuation in the process of channel narrowing. Geomorphology 14:341–351ADSCrossRef

Friedman JM, Osterkamp WR, William M, Lewis J (1996b) Channel narrowing and vegetation development following a great plains flood. Ecology 77:2167–2181CrossRef

Gaurav K, Tandon SK, Devauchelle O et al (2017) A single width–discharge regime relationship for individual threads of braided and meandering rivers from the Himalayan Foreland. Geomorphology 295:126–133. https://doi.org/10.1016/j.geomorph.2017.07.004ADSCrossRef

Ghosh S, Guchhait SK (2014a) Analyzing fluvial hydrological estimates and flood geomorphology from channel dimensions using ASTER DEM, GIS and statistics in the controlled Damodar river, India. J Geom 8:232–245

Ghosh S, Guchhait SK (2014b) Hydrogeomorphic variability due to dam constructions and emerging problems: a case study of Damodar River, West Bengal, India. Environ Dev Sustain 16:769–796. https://doi.org/10.1007/s10668-013-9494-5CrossRef

Ghosh S, Mistri B (2012) Hydrogeomorphic Significance of Sinuosity Index in relation to River Instability: a Case Study of Damodar River, West Bengal, India. Int J Adv Earth Sci 1:49–57

Graf WL (1978) Fluvial adjustments to the spread of tamarisk in the Colorado Plateau region. Geol Soc Am Bull 89:1491–1501. https://doi.org/10.1130/0016-7606(1979)90%3c1183:FATTSB%3e2.0.CO;2CrossRef

Gugliotta M, Saito Y (2019) Matching trends in channel width, sinuosity, and depth along the fluvial to marine transition zone of tide-dominated river deltas: the need for a revision of depositional and hydraulic models. Earth Sci Rev 191:93–113ADSCrossRef

Hammer TR (1972) Stream channel enlargement due to urbanization. Water Resour Res 8:1530–1540. https://doi.org/10.1029/WR008i006p01530ADSCrossRef

Hargitai H, Kereszturi Á, Stouthamer E (2014) Avulsion channel. Encyclopedia of planetary landforms. Springer, New York, pp 1–10

Hereford R (1984) Climate and ephemeral-stream processes: twentieth-century geomorphology and alluvial stratigraphy of the Little Colorado River, Arizona. Bull Geol Soc Am 95:654–668. https://doi.org/10.1130/0016-7606(1984)95%3c654:CAEPTG%3e2.0.CO;2CrossRef

Hession WC, Pizzuto JE, Johnson TE, Horwitz RJ (2003) Influence of bank vegetation on channel morphology in rural and urban watersheds. Geology 31:147–150. https://doi.org/10.1130/0091-7613(2003)031%3c0147:IOBVOC%3e2.0.CO;2ADSCrossRef

Hey RD, Thorne CR (1986) Stable channels with mobile gravel beds. J Hydraul Eng 112:671–689. https://doi.org/10.1061/(ASCE)0733-9429(1986)112:8(671)CrossRef

Hughes DA, Sami K (1992) Transmission losses to alluvium and associated moisture dynamics in a semiarid ephemeral channel system in Southern Africa. Hydrol Process 6:45–53. https://doi.org/10.1002/hyp.3360060105ADSCrossRef

Jerolmack DJ (2009) Conceptual framework for assessing the response of delta channel networks to Holocene sea level rise. Quatern Sci Rev 28(17–18):1786–1800ADSCrossRef

Jones LS, Schumm SA (1999) Causes of avulsion: an overview. Fluv Sedimentol VI:169–178CrossRef

Kadam P, Sen D (2012) Flood inundation simulation in Ajoy River using MIKE-FLOOD. ISH J Hydraul Eng 18:129–141. https://doi.org/10.1080/09715010.2012.695449CrossRef

Kale VS (2003a) The spatio-temporal aspects of monsoon floods in India: Implications for flood hazard management. Disaster Manag Univ Press Hyderabad: 22–47

Kale VS (2003b) Geomorphic effects of monsoon floods on Indian rivers. Nat Haz 28:65–84. https://doi.org/10.1023/A:1021121815395CrossRef

Kale VS, Gupta A (2001) Introduction to geomorphology. Orient-Blackswan India Pvt. Limited

Kemp J (2010) Downstream channel changes on a contracting, anabranching river: the Lachlan, southeastern Australia. Geomorphology 121:231–244. https://doi.org/10.1016/J.GEOMORPH.2010.04.018ADSCrossRef

Keppel RV, Renard KG (1962) Transmission losses in ephemeral stream beds. J Hydralulics Div Proc Am Soc Civ Eng 3116:59–68

Knighton AD (1974) Variation in width-discharge relations and some implications for hydraulic geometry. Geol Soc Am Bull 85:1069–1076CrossRef

Knighton D (1999) Downstream variation in stream power. Geomorphology 29:293–306. https://doi.org/10.1016/S0169-555X(99)00015-XADSCrossRef

Knighton D (2014) Fluvial forms and processes : a new perspective. Taylor and Francis, LondonCrossRef

Knighton AD, Nanson GC (1994a) Flow transmission along an arid zone anastomosing river, cooper creek, australia. Hydrol Process 8:137–154. https://doi.org/10.1002/hyp.3360080205ADSCrossRef

Knighton AD, Nanson GC (1994b) Waterholes and their significance in the anastomosing channel system of Cooper Creek, Australia. Geomorphology 9:311–324. https://doi.org/10.1016/0169-555X(94)90052-3ADSCrossRef

Knox JC (1984) Responses of river systems to Holocene climates. Late Quat Environ US 2:26–41. https://doi.org/10.5749/j.ctttt09b.8CrossRef

Kondolf GM (1997) PROFILE: hungry water: effects of dams and gravel mining on river channels. Environ Manage 21(4):533–551CrossRefPubMed

Labbe JM, Hadley KS, Schipper AM et al (2011) Geomorphology in fl uence of bank materials, bed sediment, and riparian vegetation on channel form along a gravel-to-sand transition reach of the Upper Tualatin River, Oregon, USA. Geomorphology 125:374–382. https://doi.org/10.1016/j.geomorph.2010.10.013ADSCrossRef

Lekach J, Schick AP, Schlesinger A (1992) Bedload yield and in-channel provenance in a flash-flood fluvial system. In: Dynamics of Gravel-bed Rivers, pp 537–554

Leopold LBLLB, Maddock JT (1953) The hydraulic geometry of stream channels and some physiographic implications. Prof Pap 252:56. https://doi.org/10.3133/PP252CrossRef

Let S, Pal S (2011) Human impact and channel hydrological modification: a study on Dwarka river of Eastern India. Int Proc Integr Sci Engenieering Manag Soc:261–267

Lewin J, Brewer PA, Wohl E (2018) Fluvial geomorphology. In: Reference module in earth systems and environmental sciences. Elsevier

Malik S, Pal SC (2020a) Application of 2D numerical simulation for rating curve development and inundation area mapping: a case study of monsoon dominated Dwarkeswar River. Int J River Basin Manag. https://doi.org/10.1080/15715124.2020.1738447CrossRef

Malik S, Pal SC (2020b) Downstream decreasing channel capacity of a monsoon-dominated Bengal Basin River: a case study of Dwarkeswar River, Eastern India. Chinese Geogr Sci. https://doi.org/10.1007/s11769-020-1143-yCrossRef

Malik S, Pal SC (2020c) Anthropogenic Impact on Channel and Extra-Channel Geomorphology of the Dwarkeswar River Basin. In: Das BC, Ghosh S, Islam A, Roy S (eds) Anthropogeomorphology of Bhagirathi-Hooghly River System in India. CRC Press

Manners RB, Schmidt JC, Scott ML (2014) Mechanisms of vegetation-induced channel narrowing of an unregulated canyon river: Results from a natural field-scale experiment. Geomorphology 211:100–115. https://doi.org/10.1016/j.geomorph.2013.12.033ADSCrossRef

Martin CW, Johnson WC (1987) Historical channel narrowing and riparian vegetation expansion in the medicine lodge River Basin, Kansas, 1871–1983. Ann Assoc Am Geogr 77

Mason PJ, Sykes RI (1979) Flow over an isolated hill of moderate slope. Q J R Meteorol Soc 105:383–395. https://doi.org/10.1002/qj.49710544405ADSCrossRef

McKenney R, Jacobson RB, Wertheimer RC (1995) Woody vegetation and channel morphogenesis in low gradient, gravel-bed streams in the Ozark Plateaus, Missouri and Arkansas. Geomorphology 13:175–198. https://doi.org/10.1016/0169-555X(95)00034-3ADSCrossRef

Millar RG (2000) Influence of bank vegetation on alluvial channel patterns. Water Resour Res 36:1109–1118. https://doi.org/10.1029/1999WR900346ADSCrossRef

Mishra PK, Sharma S (1994) Theoretical considerations in design of farm ponds for minimising evaporation and seepage losses. Indian J Dryl Agric Res Dev 9:114–120

Moges G, Bhole V (2016) Change in channel morphology, grain size and hydraulic parameters downstream of Goro, an Ephemeral River in Dire-Dawa, Ethiopia. Geosciences 6(2):45–73. https://doi.org/10.5923/j.geo.20160602.03CrossRef

Morgan AM, Craddock RA (2019) How accurate are paleodischarge estimates for martian rivers? LPSC. https://doi.org/10.3133/pp252CrossRef

Morisawa M, Clayton KM (1985) Rivers : form and process. Longman, London, New York

Mukhopadhyay S (2010) A geo-environmental assessment of flood dynamics in lower ajoy river inducing sand splay problem in eastern India. Ethiop J Environ Stud Manag 3:96–110. https://doi.org/10.4314/ejesm.v3i2.59841CrossRef

Mukhopadhyay S, Let S (2014) Changing flood intensity zone of Dwarka river basin in eastern India. Trans Inst Indian Geogr 36:123–132

Mukhopadhyay S, Mukhopadhyay M, Pal S (2010) Advance river geography. ABC Publication, Kolkata

Murgatroyd AL, Ternan JL (1983) The impact of afforestation on stream bank erosion and channel form. Earth Surf Process Landforms 8:357–369. https://doi.org/10.1002/esp.3290080408ADSCrossRef

Nanson GC, Young RW (1981) Downstream reduction of rural channel size with contrasting urban effects in small coastal streams of southeastern Australia. J Hydrol 52:239–255. https://doi.org/10.1016/0022-1694(81)90173-6CrossRef

Nath SK, Roy D, Kumar K, Thingbaijam S (2008) Disaster mitigation and management for West Bengal , India—an appraisal. Curr Sci 94

Pal S, Let S (2012) Flood intensity and potential flood loss estimation in Dwarka River Basin of Eastern India. Online An Online Int J Available 2:116–122

Park CC (1976) The relationship of slope and stream channel form in the River Dart, Devon. J Hydrol 29:139–147. https://doi.org/10.1016/0022-1694(76)90010-XCrossRef

Park CC (1977) World-wide variations in hydraulic geometry exponents of stream channels: an analysis and some observations. J Hydrol 33:133–146. https://doi.org/10.1016/0022-1694(77)90103-2CrossRef

Patton PC, Schumm SA (1975) Gully erosion, Northwestern Colorado: a threshold phenomenon. Geology 3:88–90. https://doi.org/10.1130/0091-7613(1975)3%3c88:GENCAT%3e2.0.CO;2ADSCrossRef

Phillips JD, Slattery MC (2007) Downstream trends in discharge, slope, and stream power in a lower coastal plain river. J Hydrol 334:290–303. https://doi.org/10.1016/j.jhydrol.2006.10.018CrossRef

Pietsch TJ, Nanson GC (2011) Geomorphology Bankfull hydraulic geometry; the role of in-channel vegetation and downstream declining discharges in the anabranching and distributary channels of the Gwydir distributive fl uvial system, southeastern Australia. Geomorphology 129:152–165. https://doi.org/10.1016/j.geomorph.2011.01.021ADSCrossRef

Pitlick J, Cress R (2002) Downstream changes in the channel geometry of a large gravel bed river. Water Resour Res 38:34-1–34-11. https://doi.org/10.1029/2001wr000898CrossRef

Prosser IP, Rutherfurd ID, Olley JM, Young WJ, Wallbrink PJ, Moran CJ (2001) Large-scale patterns of erosion and sediment transport in river networks, with examples from Australia. Mar Freshw Res 52(1):81–99CrossRef

RMSI (2015) India FloodRisk India’s first countrywide flood risk model

Rosgen DL (1994) A classification of natural rivers. In: Catena. pp 169–199

Rowntree KM, Dollar ESJ (1999) Vegetation controls on channel stability in the Bell River, Eastern Cape, South Africa. Earth Surf Process Landforms 24:127–134ADSCrossRef

Roy S, Dutta S (2014) Role of embankment in flood: a study in the confluence zone of Kunur And Ajay Rivers, Lower Ajay River Basin, West Bengal. Indian Streams Res J 3:1–6. https://doi.org/10.9780/22307850CrossRef

Roy S, Mistri B (2013) Estimation of peak flood discharge for an ungauged river: a case study of the Kunur River, West Bengal. Geogr J 2013:1–11. https://doi.org/10.1155/2013/214140CrossRef

Roy S, Sahu AS (2016) Effect of land cover on channel form adjustment of headwater streams in a lateritic belt of West Bengal (India). Int Soil Water Conserv Res 4:267–277. https://doi.org/10.1016/j.iswcr.2016.09.002CrossRef

Roy NG, Sinha R (2018) Integrating channel form and processes in the Gangetic plains rivers: implications for geomorphic diversity. Geomorphology 302:46–61. https://doi.org/10.1016/j.geomorph.2017.09.031ADSCrossRef

Rudra K (2009) Water resource and its quality in west bengal: a state of environment report

Rutherfurd (1994) Inherited controls on the form of a large, low energy river: the Murray River, Australia. In: American Society of Civil Engineers (ed) The variability of large alluvial rivers, pp 177–197

Schumm SA (1960) The shape of Alluvial channels in relation to sediment type. US Geol Surv Prof Pap B 352:17–30

Schumm SA (1971) Fluvial geomorphology: channel adjustment and river metamorphosis. River Mech 1:1–22

Schumm SA (1985) Patterns of alluvial rivers. Annu Rev Earth Planet Sci 13:5–27. https://doi.org/10.1146/annurev.ea.13.050185.000253ADSCrossRef

Schumm SA (1993) River response to baselevel change: implications for sequence stratigraphy. J Geol 101:279–294. https://doi.org/10.1086/648221ADSCrossRef

Schumm SA, Dumount J, Holbrook J (2000) Active tectonics and alluvial rivers, 1st edn. Cambridge University Press, Cambridge

Simon A, Collison AJC (2001) Pore-water pressure effects on the detachment of cohesive streambeds: seepage forces and matric suction. Earth Surf Process Landforms 26:1421–1442. https://doi.org/10.1002/esp.287ADSCrossRef

Simon A, Collison AJC (2002) Quantifying the mechanical and hydrologic effects of riparian vegetation on streambank stability. Earth Surf Process Landforms 27:527–546ADSCrossRef

Singh S (2018) Geomorphology, 2018th edn. Pravalika Publications Prayag Pustak Bhawan, Allahabad

Sklar L, Dietrich WE (1998) River longitudinal profiles and bedrock incision models: Stream power and the influence of sediment supply. In: Geophysical Monograph Series. pp 237–260

Szewczyk L, Grimaud J-L, Cojan I (2020) Experimental evidence for bifurcation angles control on abandoned channel fill geometry. Earth Surf Dyn 8:275–288. https://doi.org/10.5194/esurf-8-275-2020ADSCrossRef

Tal M, Gran K, Murray AB, et al (2013) Riparian vegetation as a primary control on channel characteristics in multi-thread rivers. In: Riparian Vegetation and Fluvial Geomorphology

Tal M, Paola C (2010) Effects of vegetation on channel morphodynamics: Results and insights from laboratory experiments. Earth Surf Process Landforms. https://doi.org/10.1002/esp.1908CrossRef

Tan C, Feng S, Zhao X, Shan X, Feng X (2021) Longitudinal variations in channel morphology of an ephemeral stream from upland to lowland, Daihai Lake basin, North China. Geomorphology 372:107450CrossRef

Thakur P, Chauhan N (2018) Delhi most vulnerable UT in India’s first disaster risk index Maharashtra Leads States. Times of India Online Publication: https://timesofindia.indiatime

Tooth S (1999) Downstream changes in floodplain character on the Northern Plains of arid central Australia: 93–112

Tooth S (2000a) Process, form and change in dryland rivers: a review of recent research. Earth Sci Rev 51:67–107ADSCrossRef

Tooth S (2000b) Downstream changes in dryland river channels: the Northern Plains of arid central Australia. Geomorphology 34:33–54. https://doi.org/10.1016/S0169-555X(99)00130-0ADSCrossRef

Trimble SW (1997) Stream channel erosion and change resulting from riparian forests. Geology 25:467–469. https://doi.org/10.1130/0091-7613(1997)025%3c0467:SCEACR%3e2.3.CO;2ADSCrossRef

VanLooy JA, Martin CW (2005) Channel and vegetation change on the Cimarron River, Southwestern Kansas, 1953–2001. Ann Assoc Am Geogr 95:727–739. https://doi.org/10.1111/j.1467-8306.2005.00483.xCrossRef

Vargas-Luna A, Crosato A, Byishimo P, Uijttewaal WSJ (2019a) Impact of flow variability and sediment characteristics on channel width evolution in laboratory streams. J Hydraul Res 57:51–61. https://doi.org/10.1080/00221686.2018.1434836CrossRef

Vargas-Luna A, Duró G, Crosato A, Uijttewaal W (2019b) Morphological adaptation of river channels to vegetation establishment: a laboratory study. J Geophys Res Earth Surf 124:1981–1995. https://doi.org/10.1029/2018JF004878ADSCrossRef

Wohl E (2004) Limits of downstream hydraulic geometry. Geology 32:897–900. https://doi.org/10.1130/G20738.1ADSCrossRef

Wolman MG, Gerson R (1978) Relative scales of time and effectiveness of climate in watershed geomorphology. Earth Surf Process 3:189–208. https://doi.org/10.1002/esp.3290030207CrossRef

Yousefi N, Khodashenas SR, Eslamian S, Askari Z (2016) Estimating width of the stable channels using multivariable mathematical models. Arab J Geosci. https://doi.org/10.1007/s12517-016-2322-0CrossRef

Zimmerman RC, Goodlett JC, Comer GH (1967) The influence of vegetation on channel form of small streams. In: Symposium on River Morphology, Publication No. 75. International Association of Hydrological Sciences, pp 255–275

Titel: Decreasing trends of downstream channel width: a comprehensive review of the scientific literature
verfasst von: Sadhan Malik
Subodh Chandra Pal
Abu Reza Md. Towfiqul Islam
Publikationsdatum: 01.02.2024
Verlag: Springer International Publishing
Erschienen in: Sustainable Water Resources Management / Ausgabe 1/2024
Print ISSN: 2363-5037
Elektronische ISSN: 2363-5045
DOI: https://doi.org/10.1007/s40899-023-00991-3

Springer Professional

Abstract

Bitte loggen Sie sich ein, um Zugang zu Ihrer Lizenz zu erhalten.

Sie haben noch keine Lizenz? Dann Informieren Sie sich jetzt über unsere Produkte:

Springer Professional "Wirtschaft+Technik"

Springer Professional "Technik"

Weitere Artikel der Ausgabe 1/2024

Groundwater quality evaluation using Water Quality Index (WQI) under GIS framework for Mandya City, Karnataka

Evaluating adaptive capacity and identifying climate change barriers to adaptation (case study: Qarranqu Basin, Iran)

Water supply and demand balancing and forecasting in a semi-arid region of Algeria using the WEAP model: a case study of El Bayadh province

Dams and their safety under the extreme climate conditions: study of dams on Godavari River

Financial assessment of groundwater and rainwater treatments for school clean water supply

Necessity and ways to improve the calculation of a closed collector-drainage network of drainage systems