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The channel form and processes of erosion and transportation in a river are intimately tied to the fluvial and flood regimes which, in turn, are controlled by the regional hydro-climatic conditions. The Kaveri River serves as a lifeline for the vast population. It is, therefore, necessary to understand the fluvial and flood regime characteristics of the river. Daily, monthly mean discharge data and the annual maximum series (AMS) data were obtained from the Central Water Commission. The analyses of data indicate that the monsoon regime plays a role of considerable importance in determining the river regime conditions. Like the parent stream, the mean annual hydrographs of the tributaries are characterized by one pronounced peak. Although the Kaveri River is perennial, more than 60 to 95% of the flows are recorded in the monsoon months. This is, therefore, the period of geomorphic effectiveness. The time series plots of AMS data reflect substantial maximum interannual variability. The unit discharge of t he Kaveri Basin is 0.18 m³ s-¹ km-², which is lower than other Indian rivers. The values of the coefficient of variation of AMS data range from 0.36 to 1.89, indicating low to high variability. All values of the coefficient of skewness (Cs) are positive and vary between 0.55 and 3.39. The positive values of Cs indicate a few very high-magnitude floods during the gauged period. The envelop curve of the Kaveri Basin falls much below the world envelop curve, revealing that the basin is not capable of producing very large magnitude floods for a given catchment area. The study of hydrographs indicates that large flows occur for 7 to 15 days. Thus, the investigation indicates that the fluvial and flood regime characteristics of the Kaveri River and its tributaries are controlled by monsoonal rainfall pattern and by the release of water from the reservoirs.
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Bibliogr. 45 poz., rys., tab.
Twórcy
autor
- HPT Arts and RYK Science College, Savitribai Phule Pune University, India
- HPT Arts and RYK Science College, Savitribai Phule Pune University, India
autor
- RNC Arts, JDB Commerce and NSC Science College, India
Bibliografia
- Baker V.R., 1977, Stream-channel response to floods, with examples from central Texas, Geological Society of American Bulletin, 88 (8), 1057-1071, DOI: 10.1130/0016-7606(1977)882.0.CO;2.
- Baker V.R., 1994, Geomorphological understanding of floods, Geomorphology, 10 (1-4), 139-156, DOI: 10.1016/0169- 555X(94)90013-2.
- Baker V.R., 1995, Global palaeohydrological change, Quaestiones Geographicae, 4, 27-35.
- Baker V.R., Kochel R.C., Patton P.C., 1988, Flood Geomorphology, Wiley.
- Brauman K.A., Daily G.C., Duarte T.K., Mooney H.A., 2007, The nature and value of ecosystem services: an overview highlighting hydrologic services, Annual Review of Environment and Resources, 32, 67-98, DOI: 10.1146/annurev.energy.32.031306.102758.
- Charlton R., 2008, Fundamentals of Fluvial Geomorphology, Routledge.
- Chow V.T., 1964, Handbook of Applied Hydrology, McGraw-Hill, New York.
- Costa J.E., O'Connor J.E., 1995, Gemorphologically effective foods, [in:] Natural and Anthropogenic Influences in Fluvial Geomorphology, Geophysical Monograph, 89, 45-56.
- CWC, 2020, Water Year Book 2018-19: Cauvery and Southern Rivers Circle, Central Water Commission, Ministry of Jal Shakti, Government of India.
- Ekka A., Keshav S., Pande S., Zaag P., Jiang Y., 2022, Dam-induced hydrological alterations in the upper Cauvery river basin, Journal of Hydrology: Regional Studies, 44, DOI: 10.1016/j.ejrh.2022.101231.
- Enzel Y., Ely L.L., House P.K., Baker V.R., 1993, Palaeoflood evidences for a natural upper bound to flood magnitudes in the Colorado Basin, Water Resources Research, 29 (7), 2287-2297, DOI: 10.1029/93WR00411.
- Erskine W.D., Livingstone E.A., 1999, In-channel benches: the role of floods in their formation and destruction on bedrockconfined rivers, [in:] Varieties of Fluvial Form, A.J. Miller, A. Gupta (eds.), John Wiley and Sons Ltd., Chichester, 445-475.
- Gopal B., 2016, A conceptual framework for environmental flows assessment based on ecosystem services and their economic valuation, Ecosystem Services, 21 (Part A), 53-58, DOI: 10.1016/j.ecoser.2016.07.013.
- Goswami D.C., 1985, Brahmaputra River, Assam, India: Physiography, basin denudation, and channel aggradation, Water Resources Research, 21 (7), 959-978, DOI: 10.1029/WR021i007p00959.
- Gupta A., 1988, Large floods as geomorphic events in the humid tropics, [in:] Flood Geomorphology, V.R. Baker, R.C. Kochel, P.C. Patton (eds.), Wiley, New York, 301-315.
- Gupta A., 1995, Magnitude, frequency, and special factors affecting channel form and processes in the seasonal tropics, [in:] Natural and Anthropogenic influences in the Fluvial Geomorphology, J.E. Costa, A.J. Miller, K.W. Potter, P. Wilcock (eds.), American Geophysical Union, Washington, DC, Monograph 89, 125-136.
- Gupta A., Kale V.S., Rajaguru S.N., 1999, The Narmada River, India, through space and time, [in:] Varieties of Fluvial Form, A.J. Miller, A. Gupta (eds.), John Wiley and Sons Ltd., Chichester, 113-341.
- Hire P.S., 2000, Geomorphic and Hydrologic Studies of Floods in Tapi Basin, PhD thesis. University of Pune, Pune, India.
- Kale V.S., Ely L.L., Enzel Y., Baker V.R., 1994, Geomorphic and hydrologic aspects of monsoon floods on the Narmada and Tapi Rivers in central India, Geomorphology, 10 (1-4), 157-168, DOI: 10.1016/0169-555X(94)90014-0.
- Kale V.S., Sengupta S., Achyuthan H., Jaiswal M.K., 2014, Tectonic controls upon Kaveri River drainage, cratonic Peninsular India: Inferences from longitudinal profiles, morphotectonic indices, hanging valleys and fluvial records, Geomorphology, 227, 153-165, DOI: 10.1016/j.geomorph.2013.07.027.
- Kochel R.C., 1988, Geomorphic impact of large floods: review and new perspectives on magnitude and frequency, [in:] Flood Geomorphology, V.R. Baker, R.C. Kochel, P.C. Patton (eds.), Wiley, New York, 169-187.
- Leopold L.B., Wolman M.G., Miler J.P., 1964. Fluvial Process in Geomorphology. Freeman, San Francisco.
- McMahon T.A., Finlayson B.L., Haines A.T., Srikanthan R. (eds.), 1992, Global runoff - Continental Comparisons of Annual Flows and Peak Discharges, Catena Paperback, 166 pp.
- Mutreja K.N., 1995, Applied Hydrology, Tata McGraw-Hill Publishing Company Ltd., New Delhi.
- Pagare S.R., Hire P.S., Patil A.D., 2025, Magnitude and frequency analyses of floods on the Kaveri River of the Southern India by using Gumbel Extreme Value type I probability distribution, Hydrospatial Analysis, 9 (1), 1-9, DOI: 10.21523/gcj3.2025090101.
- Patil A.D., 2017, Bedrock Channel of the Par River: Its Forms and Processes, PhD thesis. Tilak Maharashtra Vidyapeeth, Pune, India.
- Patil A.D., Hire P.S., Bramhankar G.W., Khandare P.R., Gunjal R.P., Anwat V.K., 2024a, Flood meteorology, hydrology, and geomorphology of the Upper Godavari River, Western India, Meteorology Hydrology and Water Management, 12 (1), 65-82, DOI: 10.26491/mhwm/191702.
- Patil A.D., Pawar U.V., Bramhankar G.W., Hire P.S., 2024b, Flood hydrology, hydraulics, and hydrodynamics of the Tapi River, Western India, [in:] Rivers of India, S. Kanhaiya, S. Singh, A. Dixit, A.K. Singh (eds.), Springer, 213-232, DOI: 10.1007/978- 3-031-49163-4_13.
- Pawar U.V., 2019, An Analytical Study of Geomorphological, Hydrological, and Meteorological Characteristics of Floods in the Mahi River Basin: Western India, PhD Thesis, Tilak Maharashtra Vidyapeeth, Pune, India.
- Ramaswamy S.M., 2006, Remote sensing and active tectonics of South India, International Journal of Remote Sensing, 27 (20), 4397-4431, DOI: 10.1080/01431160500502603.
- Renofalt B.M., Jansson R., Nilsson C., 2010, Effects of hydropower generation and opportunities for environmental flow management in Swedish riverine ecosystems, Freshwater Biology, 55 (1), 49-67, DOI: 10.1111/j.1365-2427.2009.02241.x.
- Sakthivadivel R., Raghupathy A., 1978, Frequency analysis of floods in some Indian rivers, Hydrology Review, 4, 57-67.
- Schumm S.A., 1977, The Fluvial System, John Wiley and Sons, New York.
- Seth S.M., 1998, Flood hydrology and flood management in India, [in:] Floods Studies in India, V.S. Kale (ed.), Geological Society of India, Memoir, 41, 155-172.
- Shaligram V.M., Lele V.S., 1978, Analysis of hydrologic data using Pearson Type III distribution, Nordic Hydrology, 9, 31-42.
- Sharma A., Rajamani V., 2001, Weathering of charnockites and sediment production in the catchment area of the Cauvery River, southern India, Sedimentary Geology, 143 (1-2), 169-184, DOI: 10.1016/S0037-0738(01)00102-6.
- Shaw E.M., 1988, Hydrology in Practice, VanNostrand Reibhold Int. Co. Ltd., London.
- Vaidyanadhan R., 1971, Evolution of the drainage of Cauvery in South India, Journal Geological Society of India 12 (1), 14-23, DOI: 10.17491/jgsi/1971/120102.
- Vaithiyanathan P., Ramanathan Al., Subramanian V., 1992, Sediment transport in the Cauvery River basin: sediment characteristics and controlling factors, Journal of Hydrology 139 (1-4), 197-210, DOI: 10.1016/0022-1694(92)90202-7.
- Valdiya K.S., 2001, Tectonic resurgence of the Mysore plateau and surrounding regions in cratonic Southern India, Current Science, 81 (8), 1068-1089.
- Viessman W., Lewis G.L., Knapp J.W., 1989, Introduction to Hydrology, Happer and Row Publishers, Singapore.
- Ward R., 1978, Floods. A Geographical Perspective, The MacMillan Press Ltd., London.
- Wells N.A., Dorr J.A., 1987, Shifting of the Kosi River, Northern India, Geology, 15 (3), 204-207, DOI: 10.1130/0091-7613(1987)152.0.CO;2.
- Wohl E.E., 1992, Bedrock benches and boulder bars: Floods in the Burdekin Gorge of Australia, Geological Society of America Bulletin, 104 (6), 770-778, DOI: 10.1130/0016-7606(1992)1042.3.CO;2.
- Wolman M.G., Miller J.P., 1960, Magnitude and frequency of forces in geomorphic processes, Journal of Geology, 68 (1), 54-74, DOI: 10.1086/626637.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-18dfc63c-e55f-4c29-a8d2-7986aa8b82b4
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