Skip to main content

Advertisement

Log in

Hydrological Characteristics of 7th February 2021 Rishi Ganga Flood: Implication towards Understanding Flood Hazards in Higher Himalaya

  • Research Articles
  • Published:
Journal of the Geological Society of India

Abstract

A flash flood that originated from Raunthi Gad-a tributary of the Rishi Ganga river, in Garhwal Himalaya, caused unprecedented loss to lives and damaged two hydropower projects on 7th Februray 2021. In order to asses the flood magnitude, the flow parameters of the flood were calculated using the super-elevation of the flood marks preserved in the flood affected valleys.

The textural characteristics of the flood deposits in the upper reaches of the valleys indicate dominance of debris flows. The peak discharge upstream of the confluence of Rishi Ganga and Dhauli Ganga was around 1.1×105 m3/s, which was four order of magnitiude higher than the normal peak discharge (∼ 3 m3/s). The flow achieved a velocity of 30±3 m/s. An exponential reduction in the flow velocity (from ∼37 to 2 m/s) with distance is observed. For which the river gradient and increase in sediment load is implied flow that along its entrained way downstream between Raini and Tapovan. Considering the sensitivity of paraglacial zones to climate change, the paper calls for detailed studies pertaining to the response of paraglacial zones to extreme weather events. Importantly, it is necessary to have more hydrological data covering multiple valleys for predictive model simulation of the nature and magnitude of such disasters in future.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Bovis, M.J. and Jakob, M. (1999) The role of debris supply conditions in predicting debris flow activity. Earth Surf. Process. Landforms, v.24, pp.1039–1054.

    Article  Google Scholar 

  • Carrivick, J.L., Boston, C.M., King, O., James, W.H.M., Quincey, D.J., Smith, M.W., Grimes, M. and Evans, J. (2019) Accelerated Volume Loss in Glacier Ablation Zones of NE Greenland, Little Ice Age to Present. Geophys. Res. Lett, pp.1–9, doi: https://doi.org/10.1029/2018GL081383.

  • Chow, V.T. (1959) Open-channel hydraulics. McGraw-Hill, New York.

    Google Scholar 

  • Costa, J.E. (1988) Evaluation of the flood hydrology in the Colorado Front using precipitation, streamflow and paleo flood data for the big Thompson River Basin. U.S. Geological Survey 87, 4117. Johnson, A.M., 1984. Debris flow. In: Brunsden, D., Prior, D.B. (Eds.), Slope Instability. John Wiley & Sons, Chichester, UK, pp.257–361.

    Google Scholar 

  • Costa, J.E. (1988) Rheologic, geomorphic, and sedimentological differentiation of water floods, hyperconcentrated flows, and debris flows. In: Flood Geomorphology (Eds Baker, V.R., Kochel, R.C. & Patton, R.C.), pp.113–122. John Wiley & Sons, New York.

    Google Scholar 

  • Dobhal., D.P., Gupta, A.K., Mehta, M. and Khandelwal, D.D. (2013) Kedarnath disaster: facts and plausible causes. Curr. Sci., v.105, pp.171–174.

    Google Scholar 

  • Gartner, J.D., William, B.D., Renshaw, C.E., Magilligan, F.J. and Buraas, E.M. (2015) Gradient in stream power influence lateral and downstream sediment flux in floods. Geology, v.43(11), pp.983–986.

    Article  Google Scholar 

  • Hack, J.K. (1957) Studies of longitudinal river profiles in Verginia and Maryland.U.S. Geologic Survey Prof. Paper 249B, 99p.

  • Iverson, R.M. (1997) The physics of debris flows. Rev. Geophys., v.35, pp.245–296.

    Article  Google Scholar 

  • Iverson, R. M., LaHusen, R.G., Major, J.J. and Zimmerman, C.L. (1994) Debris flow against obstacles and bends: dynamics and deposits. Eos, Trans., Amer. Geophys. Union, v.75, pp.274.

    Google Scholar 

  • Jakob, M. and Hungr, O. (2005) Debris flow hazards and related phenomena. Springer Book Series.

  • Jarrett, R.D. (1984) Hydraulics of high-gradient streams. Jour. Hydraul. Eng., v.110, pp.1519–1539.

    Article  Google Scholar 

  • Juyal, N. (2010) Cloud burst-triggered debris flows around Leh. Curr. Sci., v.99, pp.1166–1167.

    Google Scholar 

  • Korup, O., Strom, A.L. and Weidinger, J.T. (2006) Fluvial response to large rock-slope failures: examples from the Himalayas, the Tien Shan, and the Southern Alps in New Zealand. Geomorphology, v.78, pp.3–21.

    Article  Google Scholar 

  • Kumar, V., Shukla, T., Mehta, M., Dothan, D.P., Bisht, M.P.S. and Nautiyal, S. (2020) Glacier changes and associated climate drivers for the last three decades, Nana Devi region, Central Himalaya, India. Quaternary Internat., v.575–576, pp.1040–6182.

    Google Scholar 

  • Liu, M., Zhang, Y., Tian, S.F., Chen, N., Mahfuzr, R. and Javed, I. (2020) Effects of loose deposits on debris flow processes in the Aizi Valley, southwest China. Jour. Mountain Sci., v.17(1), DOI:https://doi.org/10.1007/s11629-019-5388-9.

  • Magilligan, F.J. (1992) Threshold and the spatial variability of flood power during extreme Floods. Geomorphology, v.5(3–5), pp.373–390.

    Article  Google Scholar 

  • Mukherjee, P.K., Jain, A.K., Singhal, S., Singha, N.B., Singh, S., Kislay, K., Seth, P. and Patel, R.C. (2019) U-Pb zircon ages and Sm-Nd isotopic characteristics of the Lesser and Great Himalayan sequences, Uttarakhand Himalaya, and their regional tectonic implications; Gondwana Res., v.75, pp.282–297. doi: https://doi.org/10.1016/j.gr.2019.06.001.

    Article  Google Scholar 

  • O’Connor, J.E. and Costa, J.E. (1993) Geological and hydrological hazards in glacierized in North America resulting from 19th and 20th century global warming. Natural Hazards, v.8, pp.121–140.

    Article  Google Scholar 

  • Panda, S., Kumar, A., Das, S., Devrani, R., Rai, S., Prakash, K. and Srivastava, P. (2020) Chronology and sediment provenance of extreme floods of Siang River (Tsangpo Brahmaputra River valley), northeast Himalaya. Earth Surface Processes and Landform, v.45, pp.2495–2511. DOI:https://doi.org/10.1002/esp.4893

    Article  Google Scholar 

  • Pierson, T.C. (1985) Initiation and flow behavior of the 1980 Pine Creek and Muddy River lahars, Mount St. Helens, Washington. GSA Bull., v.96, pp.1056–1069.

    Article  Google Scholar 

  • Pierson, T.C. (2005) Hyperconcentrated flow-transitional process between water flow and debris flow. In: Debris-flow Hazards and Related Phenomena. Springer Praxis Books. Springer, Berlin, Heidelberg. doi:https://doi.org/10.1007/3-540-27129-5_8

    Google Scholar 

  • Pierson, T.C. and Scott, K.M. (1985) Downstream dilution of lahar: transition from debris flow to hyper concentrated streamflow. Water Resour. Res., v.21(10), pp.1511–1524.

    Article  Google Scholar 

  • Prochaska, A.B., Santi, P.M., Higgins, J.D. and Cannon, S.H. (2008) Debrisflow runout predictions based on the average channel slope (ACS). Engg. Geol., v.98, pp.29–40.

    Article  Google Scholar 

  • Rana, N., Sundriyal, Y.P. and Juyal, N. (2012) Recent cloudburst-induced landslides around Okhimath, Uttarakhand. Curr. Sci., v.103, pp.1389–1390.

    Google Scholar 

  • Rana, N., Sharma, S., Sundriyal, Y., Kaushik, S., Pradhan, S., Tiwari, G., Khan, F., Sati, S.P. and Juyal, N. (2021) A preliminary assessment of the 7th February 2021 flash flood in lower Dhauli Ganga valley, Central Himalaya, India. Jour. Earth Syst. Sci., v.130, 78. doi:https://doi.org/10.1007/s12040-021-01608-z

    Article  Google Scholar 

  • Rana, N., Singh, S., Sundriyal, Y.P. and Juyal, N. (2013) Recent and past floods in the Alaknanda valley: causes and consequences. Curr. Sci., v.105, pp.1209–1212.

    Google Scholar 

  • RGI Consortium (2017) Randolph Glacier Inventory (RGI) — A Dataset of Global Glacier Outlines: Version 6.0. Technical Report, Global Land Ice Measurements from Space, Boulder, Colorado, USA. Digital Media, doi: https://doi.org/10.7265/N5-RGI-60.

    Google Scholar 

  • Rico, M., Benito, G. and Barnolas, A. (2001) Combined palaeoflood and rainfall-runoff assessment of mountain flood (Spanish Pyrenees). Jour. Hydrol., v.245, pp.59–72.

    Article  Google Scholar 

  • Sah, M.P, Asthana, A.K.L. and Rawat, B.S. (2003) Cloud burst of August 10, 2002 and related landslides and debris flows around BudhaKedar (ThatiKathur) in Balganga valley, district Tehri. Him. Geol., v.24, pp.87–101.

    Google Scholar 

  • Sati, S.P. and Gahalaut V.K. (2013) The fury of the floods in the NW Himalayan region: the Kedarnath tragedy: Geomatics, Natural Hazards and Risk, v.4, pp.193–201.

    Article  Google Scholar 

  • Shekhar, M. (2014) Application of Multi-Proxy Tree-Ring Parameters in the Reconstruction of Climate Vis-A-Vis Glacial Fluctuation from the Eastern Himalaya Ph.D. Thesis. Department of Botany, University of Lucknow.

  • Shekhar, M., Pal, A.K., Bhattacharyya, A., Ranhotra, P.S. and Roy, I. (2018) Tree-ring based reconstruction of winter drought since 1767 CE from Uttarkashi, Western Himalaya. Quaternary Internat., v.479, 5 pp.8–69.

    Google Scholar 

  • Shukla, A. and Garg, P.K. (2019) Evolution of a debris-covered glacier in the western Himalaya during the last four decades (1971–2016): a multi parametric assessment using remote sensing and field observations. Geomorphology, v.341, pp.1–14.

    Article  Google Scholar 

  • Srivastava, P., Kumar, A., Chaudhary, S., Meena, N., Sundriyal, Y.P., Rawat, S., Rana, N., Perumal, R.J., Bisht, P., Sharma, D. and Agnihotri, R. (2017) Paleofloods records in Himalaya. Geomorphology, v.284, pp.17–30.

    Article  Google Scholar 

  • Sundriyal, Y.P., Shukla, A.D., Rana, N., Jayangondaperumal, R., Srivastava, P., Chamyal, L.S., Sati, S.P. and Juyal, N. (2015) Terrain response to the extreme rainfall event of June 2013: Evidence from the Alaknanda and Mandakini River Valleys, Garhwal Himalaya, India. Episodes, v.38(3), pp.179–188.

    Article  Google Scholar 

  • Tang, C., Rengers, N., Asch, Th. W. J. van, Yang, Y. H. and Wang, G. F. (2011) Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China. Natural Hazards Earth System Science, v.11, pp.2903–2912.

    Article  Google Scholar 

  • Wasson, R.J., Sundriyal, Y.P., Chaudhary, S., Jaiswal, M.K., Morthekai, P., Sati, S.P. and Juyal, N. (2013) A 1000-year history of large floods in the Upper Ganga catchment, central Himalaya, India. Quaternary Sci. Rev., v.77, pp.156–166.

    Article  Google Scholar 

  • Yadav, R.R., Misra, K.G., Yadava, A.K., Kotlia, B.S. and Misra, S. (2015) Tree-ring footprints of drought variability in last∼ 300 years over Kumaun Himalaya, India and its relationship with crop productivity. Quaternary Sci. Rev., v.117, pp.113–123.

    Article  Google Scholar 

  • Ziegler, A.D., Wasson, R.J., Bhardwaj, A., Sundriyal, Y.P., Sati, S.P., Juyal, N., Nautiyal, V., Srivastava, P., Gillen, J. and Saklani, U. (2014) Pilgrims, progress, and the political economy of disaster preparedness-the example of the 2013 Uttarakhand flood and Kedarnath disaster. Hydrol. Process, v.28, pp.5985–5990.

    Article  Google Scholar 

Download references

Acknowledgements

We acknowledge the DST grant number DST/CCP/MRDP/187/2019(G) dated 29/06/2020 for carrying out this study. We thank Vice-Chancellor of HNB Garhwal University for extending her support for this study. N.R. thanks Dr. R.S. Gusain for long profile construction, and people of Raini, Paing and Lata for various cooperation during field work. We thank the anonymouss reviewers for their constructive feedback.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yaspal Sundriyal.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Rana, N., Sundriyal, Y., Sharma, S. et al. Hydrological Characteristics of 7th February 2021 Rishi Ganga Flood: Implication towards Understanding Flood Hazards in Higher Himalaya. J Geol Soc India 97, 827–835 (2021). https://doi.org/10.1007/s12594-021-1781-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s12594-021-1781-4

Navigation