Abstract
The impact of increased temperature on the Third Pole, as the Himalayas is referred to, and the likely cascading impacts on the general downstream hydrology have been widely noted. However, the impact on fluvial geomorphology has not received specific attention. Change in the glacial domain in terms of melt increase will change discharge and sediment flux into fluvial system, which will induce changes in fluvial processes and forms. The present work attempts to study this process-based glacio-fluvial coupling in the two neighbouring glaciated river basins in the Northwest Himalaya, viz., the Sutlej and the Yamuna river basins till the mountain front. A total of 194 samples of river, tributary and groundwater of pre- and post-monsoon seasons in the two river basins were analysed for stable isotopes. The trend of δ18O and electrical conductivity along the mainstream gives qualitative idea on the influence of headwaters in the downstream of the catchment thereby allowing inference on melt contribution. Further, two component mixing model using stable oxygen isotope of two seasons water samples showed that melt contributes about 41.1–66.8 and 6.6–10.6% at different points to the total river discharge in the Sutlej and the Tons River (the glaciated, major tributary of the Yamuna River) basins, respectively. For different scenarios of increase in melt, stream power increase in the Sutlej River basin is significant as opposed to the Tons River. River channel in the Sutlej River basin will be significantly more impacted in comparison with the Yamuna River system.
Similar content being viewed by others
References
Ahluwalia RS, Rai SP, Jain SK, Kumar B, Dobhal DP (2013) Assessment of snowmelt runoff modelling and isotope analysis: a case study from the western Himalaya, India. Ann Glaciol 54:299–304. https://doi.org/10.3189/2013AoG62A133
Bagnold RA (1966) An approach to the sediment transport problem from general physics. Geol Surv Prof Pap 422-I:I1–I37
Barnett TP, Adam JC, Lettenmaier DP (2005) Potential impacts of a warming climate on water availability in snow-dominated regions. Nature 438:303–309. https://doi.org/10.1038/nature04141
Bawa N, Jain V, Shekhar S, Kumar N, Jyani V (2014) Controls on morphological variability and role of stream power distribution pattern, Yamuna River, western India. Geomorphology 227:60–72. https://doi.org/10.1016/j.geomorph.2014.05.016
Behrens H, Moser H, Oerter H, Rauert W, Stichler W, Ambach W (1978) Models for the runoff from a glaciated catchment area using measurements of environmental isotope contents. In: Isotope hydrology. Proceedings of a symposium, Neuherberg, 19–23 June 1978, IAEA, Vienna, vol ll, W-05. IAEA-SM-228/41 2, pp 829–846
Benetti M, Reverdin G, Pierre C, Merlivat L, Risi C, Steen-Larsen HC, Vimeux F (2014) Deuterium excess in marine water vapor: dependency on relative humidity and surface wind speed during evaporation. J Geophys Res Atmos 119:584–593. https://doi.org/10.1002/2013JD020535
Berthier E, Arnaud Y, Kumar R, Ahmad S, Wagnon P, Chevallier P (2007) Remote sensing estimates of glacier mass balances in the Himachal Pradesh (Western Himalaya, India). Remote Sens Environ 108:327–338. https://doi.org/10.1016/j.rse.2006.11.017
Bizzi S, Lerner DN (2015) The use of stream power as an indicator of channel sensitivity to erosion and deposition processes. River Res Appl 31:16–27. https://doi.org/10.1002/rra.2717
Bolch T et al (2012) The state and fate of Himalayan Glaciers. Science 336:310–314. https://doi.org/10.1126/science.1215828
Bookhagen B, Burbank DW (2010) Toward a complete Himalayan hydrological budget: spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge. J Geophys Res. https://doi.org/10.1029/2009jf001426
Bookhagen B, Strecker MR (2012) Spatiotemporal trends in erosion rates across a pronounced rainfall gradient: examples from the southern Central Andes. Earth Planet Sci Lett 327:97–110
Bookhagen B, Thiede RC, Strecker MR (2005) Late Quaternary intensified monsoon phases control landscape evolution in the northwest Himalaya. Geology 33:149. https://doi.org/10.1130/g20982.1
Brenninkmeijer CAM, Morrison PD (1987) An automated system for isotopic equilibration of CO2 and H2O for 18O analysis of water. New Dev Appl Isot Geosci Chem Geol Sect 66:21–26. https://doi.org/10.1016/0168-9622(87)90024-8
Clark ID, Fritz P (1997) Environmental isotopes in hydrogeology. Taylor & Francis, London
Cooper LW (1998) Isotopic fractionation in snow cover. Elsevier, Amsterdam
Craig H (1961) Isotopic variations in meteoric waters. Science 133:1702–1703. https://doi.org/10.1126/science.133.3465.1702
Dalai TK, Bhattacharya SK, Krishnaswami S (2002) Stable isotopes in the source waters of the Yamuna and its tributaries: seasonal and altitudinal variations and relation to major cations. Hydrol Process 16:3345–3364. https://doi.org/10.1002/hyp.1104
Dansgaard W (1964) Stable isotopes in precipitation. Tellus 16:436–468. https://doi.org/10.1111/j.2153-3490.1964.tb00181.x
Dinçer T, Payne BR, Florkowski T, Martinec J, Tongiorgi E (1970) Snowmelt runoff from measurements of tritium and oxygen-18. Water Resour Res 6:110–124. https://doi.org/10.1029/WR006i001p00110
Dobhal DP, Pratap B (2015) Variable response of glaciers to climate change in Uttarakhand Himalaya, India. In: Joshi R et al (eds) Dynamics of climate change and water resources of Northwestern Himalaya. Springer, Cham, pp 141–150. https://doi.org/10.1007/978-3-319-13743-8_12
Engelhardt M, Schuler TV, Andreassen LM (2014) Contribution of snow and glacier melt to discharge for highly glacierised catchments in Norway. Hydrol Earth Syst Sci 18:511–523. https://doi.org/10.5194/hess-18-511-2014
Epstein S, Mayeda T (1953) Variation of O18 content of waters from natural sources. Geochim Cosmochim Acta 4:213–224. https://doi.org/10.1016/0016-7037(53)90051-9
Fisher GB, Bookhagen B, Amos CB (2013) Channel planform geometry and slopes from freely available high-spatial resolution imagery and DEM fusion: implications for channel width scalings, erosion proxies, and fluvial signatures in tectonically active landscapes. Geomorphology 194:46–56
Frey H, Paul F, Strozzi T (2012) Compilation of a glacier inventory for the western Himalayas from satellite data: methods, challenges, and results. Remote Sens Environ 124:832–843. https://doi.org/10.1016/j.rse.2012.06.020
Froehlich K, Gibson JJ, Aggarwal PK (2001) Deuterium excess in precipitation and its climatological significance. Study of environmental change using isotope techniques. International Atomic Energy Agency, Vienna, pp 54–65
Gat JR (1996) Oxygen and hydrogen isotopes in the hydrologic cycle. Annu Rev Earth Planet Sci 24:225–262
Gat J, Carmi I (1970) Evolution of the isotopic composition of atmospheric waters in the Mediterranean Sea area. J Geophys Res 75:3039–3048
Gat JR, Gonfiantini R (1981) Stable isotope hydrology. Deuterium and oxygen-18 in the water cycle. International Atomic Energy Agency (IAEA), Vienna
Gibson JJ, Birks SJ, Edwards TWD (2008) Global prediction of δA and δ2H–δ18O evaporation slopes for lakes and soil water accounting for seasonality. Glob Biogeochem Cycles 22:GB2031. https://doi.org/10.1029/2007GB002997
Gonfiantini R, Gallo G, Payne BR, Taylor CB (1976) Environmental isotopes and hydrochemistry in groundwater of Gran Canaria. Interpretation of environmental isotope and hydrochemical data in ground water hydrology. International Atomic Energy Agency (IAEA), Vienna, pp 159–170
Goudie AS (2006) Global warming and fluvial geomorphology. Geomorphology 79:384–394. https://doi.org/10.1016/j.geomorph.2006.06.023
Guan H, Simmons CT, Love AJ (2009) Orographic controls on rain water isotope distribution in the Mount Lofty Ranges of South Australia. J Hydrol 374:255–264. https://doi.org/10.1016/j.jhydrol.2009.06.018
Guan H, Zhang X, Skrzypek G, Sun Z, Xu X (2013) Deuterium excess variations of rainfall events in a coastal area of South Australia and its relationship with synoptic weather systems and atmospheric moisture sources. J Geophys Res Atmos 118:1123–1138. https://doi.org/10.1002/jgrd.50137
Hack JT (1957) Studies of longitudinal stream profiles in Virginia and Maryland, U.S. Geological Survey Professional Paper, 294-B
Hancock G, Martinez C, Evans K, Moliere D (2006) A comparison of SRTM and high-resolution digital elevation models and their use in catchment geomorphology and hydrology: Australian examples. Earth Surf Proc Land 31:1394–1412
Hooper RP, Shoemaker CA (1986) A comparison of chemical and isotopic hydrograph separation. Water Resour Res 22:1444–1454. https://doi.org/10.1029/WR022i010p01444
Hren MT, Bookhagen B, Blisniuk PM, Booth AL, Chamberlain CP (2009) δ18O and δD of streamwaters across the Himalaya and Tibetan Plateau: implications for moisture sources and paleoelevation reconstructions. Earth Planet Sci Lett 288:20–32. https://doi.org/10.1016/j.epsl.2009.08.041
Immerzeel WW, Beek LPHv, Bierkens MFP (2010) Climate change will affect the Asian water towers. Science 328:1382–1385
Jain SK, Singh P, Saraf A, Seth S (2003) Estimation of sediment yield for a rain, snow and glacier fed river in the western Himalayan region. Water Resour Manag 17:377–393
Jain V, Preston N, Fryirs K, Brierley G (2006) Comparative assessment of three approaches for deriving stream power plots along long profiles in the upper Hunter River catchment, New South Wales, Australia. Geomorphology 74:297–317. https://doi.org/10.1016/j.geomorph.2005.08.012
Jha P, Subramanian V, Sitasawad R (1988) Chemical and sediment mass transfer in the Yamuna River—a tributary of the Ganges system. J Hydrol 104:237–246
Jouzel J, Merlivat L (1984) Deuterium and oxygen 18 in precipitation: modeling of the isotopic effects during snow formation. J Geophys Res Atmos 89:11749–11757. https://doi.org/10.1029/JD089iD07p11749
Jouzel J, Merlivat L, Lorius C (1982) Deuterium excess in an East Antarctic ice core suggests higher relative humidity at the oceanic surface during the last glacial maximum. Nature 299:688–691
Knighton AD (1999) Downstream variation in stream power. Geomorphology 29:293–306. https://doi.org/10.1016/S0169-555X(99)00015-X
Kulkarni AV, Karyakarte Y (2014) Observed changes in Himalayan glaciers. Curr Sci 106:237–244
Kumar B et al (2010) Isotopic characteristics of Indian precipitation. Water Resour Res 46:W12548. https://doi.org/10.1029/2009wr008532
LeFavour G, Alsdorf D (2005) Water slope and discharge in the Amazon River estimated using the shuttle radar topography mission digital elevation model. Geophys Res Lett 32:L17404
Lutz AF, Immerzeel WW, Shrestha AB, Bierkens MFP (2014) Consistent increase in High Asia’s runoff due to increasing glacier melt and precipitation. Nat Clim Change 4:587–592. https://doi.org/10.1038/nclimate2237
Martinec J, Siegenthaler U, Oeschger H, Tongiorgi E (1974) New insights into the run-off mechanism by environmental isotopes. IAEA, International Atomic Energy Agency (IAEA), Vienna
Maulé CP, Stein J (1990) Hydrologic flow path definition and partitioning of spring meltwater. Water Resour Res 26:2959–2970. https://doi.org/10.1029/WR026i012p02959
Maurya AS, Shah M, Deshpande RD, Bhardwaj RM, Prasad A, Gupta SK (2011) Hydrograph separation and precipitation source identification using stable water isotopes and conductivity: river Ganga at Himalayan foothills. Hydrol Process 25:1521–1530. https://doi.org/10.1002/hyp.7912
Mehta M, Dobhal DP, Pratap B, Verma A, Kumar A, Srivastava D (2013) Glacier changes in Upper Tons River basin, Garhwal Himalaya, Uttarakhand, India. Zeitschrift für Geomorphologie 57:225–244. https://doi.org/10.1127/0372-8854/2012/0095
Merlivat L, Jouzel J (1979) Global climatic interpretation of the deuterium-oxygen 18 relationship for precipitation. J Geophys Res Oceans 84:5029–5033. https://doi.org/10.1029/JC084iC08p05029
Nijampurkar V, Rao D (1993) Ice dynamics and climatic studies on Himalayan glaciers based on stable and radioactive isotopes. IAHS Publ Publ Int Assoc Hydrol Sci 218:355–370
Nijampurkar V, Rao K, Sarin M, Gergan J (2002) Isotopic study on Dokriani Bamak glacier, central Himalaya: implications for climatic changes and ice dynamics. J Glaciol 48:81–86
Nolin AW, Phillippe J, Jefferson A, Lewis SL (2010) Present-day and future contributions of glacier runoff to summertime flows in a Pacific Northwest watershed: implications for water resources. Water Resour Res. https://doi.org/10.1029/2009WR008968
Obradovic MM, Sklash MG (1986) An isotopic and geochemical study of snowmelt runoff in a small arctic watershed. Hydrol Process 1:15–30. https://doi.org/10.1002/hyp.3360010104
Pande K, Padia J, Ramesh R, Sharma K (2000) Stable isotope systematics of surface water bodies in the Himalayan and Trans-Himalayan (Kashmir) region. J Earth Syst Sci 109:109–115
Pang Z, Kong Y, Froehlich K, Huang T, Yuan L, Li Z, Wang F (2011) Processes affecting isotopes in precipitation of an arid region. Tellus 63B:352–359
Poage MA, Chamberlain CP (2001) Empirical relationships between elevation and the stable isotope composition of precipitation and surface waters; considerations for studies of paleoelevation change. Am J Sci 301:1–15
R Core Team (2015) R: a language and environment for statistical computing. R Foundation for Statistical Computing, Vienna
Rai SP, Kumar B, Singh P (2009) Bhagirathi River near Gaumukh, western Himalayas, India, using oxygen-18 isotope. Curr Sci 97:240
Rai SP, Kumar B, Arora M, Singh RD (2013a) Isotopic Characterization of Snow, Ice and Glacial Melt in the Western Himalayas, India. In: Isotopes in hydrology, marine ecosystems and climate change studies. Proceedings of an international symposium, Monaco, 27 March–1April 2011, Vol 1. International Atomic Energy Agency (IAEA)
Rai SP, Purushothaman P, Kumar B, Jacob N, Rawat YS (2013b) Stable isotopic composition of precipitation in the River Bhagirathi Basin and identification of source vapour. Environ Earth Sci 71:4835–4847. https://doi.org/10.1007/s12665-013-2875-0
Rai SP, Thayyen RJ, Purushothaman P, Kumar B (2016) Isotopic characteristics of cryospheric waters in parts of Western Himalayas, India. Environ Earth Sci. https://doi.org/10.1007/s12665-016-5417-8
Ramesh R, Sarin M (1992) Stable isotope study of the Ganga (Ganges) river system. J Hydrol 139:49–62
Rozanski K, Araguás Araguás L, Gonfiantini R (1993) In: Swart PK et al (eds) Isotopic patterns in modern global precipitation Climate change in continental isotopic records, vol 78. Geophysics monograph series. AGU, Washington, pp 1–36
Scherler D, Bookhagen B, Strecker MR (2011) Spatially variable response of Himalayan glaciers to climate change affected by debris cover. Nat Geosci 4:156–159. https://doi.org/10.1038/NGEO1068
Scherler D, Bookhagen B, Strecker MR (2014) Tectonic control on 10Be derived erosion rates in the Garhwal Himalaya, India. J Geophys Res Earth Surf 119:83–105
Schumann G, Matgen P, Cutler M, Black A, Hoffmann L, Pfister L (2008) Comparison of remotely sensed water stages from LiDAR, topographic contours and SRTM. ISPRS J Photogr Remote Sens 63:283–296
Siegenthaler U (1979) Stable hydrogen and oxygen isotopes in the water cycle. Lectures in isotope geology. Springer, Berlin, pp 264–273
Siegenthaler U, Oeschger H (1980) Correlation of 18O in precipitation with temperature and altitude. Nature 285:314–317
Singh P, Jain S (2003) Modelling of streamflow and its components for a large Himalayan basin with predominant snowmelt yields. Hydrol Sci J 48:257–276
Singh P, Kumar N (1997) Effect of orography on precipitation in the western Himalayan region. J Hydrol 199:183–206
Sinha R, Gaurav K, Chandra S, Tandon S (2013) Exploring the channel connectivity structure of the August 2008 avulsion belt of the Kosi River, India: application to flood risk assessment. Geology 41:1099–1102
Sinha R, Mohanta H, Jain V, Tandon SK (2017) Geomorphic diversity as a river management tool and its application to the Ganga River, India. River Res Appl 33(7):1156–1176. https://doi.org/10.1002/rra.3154
Sun G, Ranson KJ, Kharuk VI, Kovacs K (2003) Validation of surface height from shuttle radar topography mission using shuttle laser altimeter. Remote Sens Environ 88:401–411
Tockner K, Paetzold A, Karaus U, Claret C, Zettel J (2006) Ecology of braided rivers. In: Smith GHS, Best JL, Bristow CS, Petts GE (eds) Braided rivers: process, deposits, ecology and management, special publication-international association of sedimentologists, vol 36. Blackwell Publishing Ltd., Oxford, UK, p 339. https://doi.org/10.1002/9781444304374.ch17
Unnikrishna PV, McDonnell JJ, Kendall C (2002) Isotope variations in a Sierra Nevada snowpack and their relation to meltwater. J Hydrol 260:38–57
Van den Berg JH (1995) Prediction of alluvial channel pattern of perennial rivers. Geomorphology 12:259–279
Vannay J-C, Grasemann B, Rahn M, Frank W, Carter A, Baudraz V, Cosca M (2004) Miocene to Holocene exhumation of metamorphic crustal wedges in the NW Himalaya: evidence for tectonic extrusion coupled to fluvial erosion. Tectonics. https://doi.org/10.1029/2002tc001429
Wang Y, Liao M, Sun G, Gong J (2005) Analysis of the water volume, length, total area and inundated area of the Three Gorges Reservoir. China using the SRTM DEM data. Int J Remote Sens 26:4001–4012
Warrier CU, Babu MP (2011) A comparative study on isotopic composition of precipitation in wet tropic and semi-arid stations across southern India. J Earth Syst Sci 120:1085–1094. https://doi.org/10.1007/s12040-011-0121-2
Webb AAG, Yin A, Harrison TM, Célérier J, Gehrels GE, Manning CE, Grove M (2011) Cenozoic tectonic history of the Himachal Himalaya (northwestern India) and its constraints on the formation mechanism of the Himalayan orogen. Geosphere 7:1013–1061. https://doi.org/10.1130/GES00627.1
Wulf H, Bookhagen B, Scherler D (2012) Climatic and geologic controls on suspended sediment flux in the Sutlej River Valley, western Himalaya. Hydrol Earth Syst Sci 16:2193–2217. https://doi.org/10.5194/hess-16-2193-2012
Wulf H, Bookhagen B, Scherler D (2016) Differentiating between rain, snow, and glacier contributions to river discharge in the western Himalaya using remote-sensing data and distributed hydrological modeling. Adv Water Resour 88:152–169. https://doi.org/10.1016/j.advwatres.2015.12.004
Yin A (2006) Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth Sci Rev 76:1–131. https://doi.org/10.1016/j.earscirev.2005.05.004
Yurtsever Y, Gat J (1981) Atmospheric waters. In: Gat JR, Gonfiantini R (eds) Stable isotope hydrology, deuterium and oxygen-18 in the water cycle, vol 210. Technical reports series. International Atomic Energy Agency, Vienna, pp 103–142
Zhou S, Nakawo M, Sakai A, Matsuda Y, Duan K, Pu J (2007) Water isotope variations in the snow pack and summer precipitation at July 1 Glacier, Qilian Mountains in northwest China. Chin Sci Bull 52:2963–2972. https://doi.org/10.1007/s11434-007-0401-z
Acknowledgements
The authors are thankful to Dr. R. D. Singh, Director, National Institute of Hydrology, Roorkee for permitting to carry out this study. The authors are also thankful to Mr. Vishal Gupta and Mr. Jamil Ahmad for providing assistance in analysing the sample on IRMS. The stream power work was carried out in the project Ganga River Basin Environment Management Plan (GRBEMP) funded by Ministry of Environment and Forest (MoEF). Authors are thankful to Central Water Commission (CWC) for providing hydrological data of the Yamuna River. LSV would like to gratefully acknowledge the financial assistance extended by Council of Scientific and Industrial Research (CSIR), New Delhi, India, in the form of Junior/Senior Research Fellowships (JRF/SRF) (Grant No. 09/045/(1121)/2011-EMR-I).
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Varay, L.S., Rai, S.P., Singh, S.K. et al. Estimation of snow and glacial melt contribution through stable isotopes and assessment of its impact on river morphology through stream power approach in two Himalayan river basins. Environ Earth Sci 76, 809 (2017). https://doi.org/10.1007/s12665-017-7142-3
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12665-017-7142-3