Abstract
River Ganges one of important rivers in the northern part of India receives water from two of its tributaries, Alaknanda and Bhagirathi. In this present study, we have tried to characterise the precipitation in the Bhagirathi River Basin. The study shows that isotopic composition of precipitation shows depleted nature during monsoon period due to moisture source from the oceanic region and from African region of Indian Ocean and enriched isotopic composition during non-monsoon period due to moisture source from westerlies and local evaporation. The study also shows that temperature and amount show expected positive and negative relationship with individual locations. A positive relationship is exhibited by amount for the entire region due to depleted isotopic composition with increase in altitude. The altitude effect shows that there is a depletion of up to −0.24 to −0.29 ‰ of isotopic composition with an increase in 100 m of elevation.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig1_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig2_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig3_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig4_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig5_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig6_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig7_HTML.gif)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs12665-013-2875-0/MediaObjects/12665_2013_2875_Fig8_HTML.gif)
Similar content being viewed by others
References
Andreo B, Linan C, Carrasco F, de Cisneros CJ, Caballero F, Mudry F (2004) Influence of rainfall quantity on the isotopic composition (18O and 2H) of water in mountainous areas: application for groundwater research in the Yunquera–Nieves karst aquifers (S Spain). Appl Geochem 19:561–574
Araguas–Araguas L, Froehlich K, Rozanski K (2000) Deuterium and oxygen-18 isotope composition of precipitation and atmospheric moisture. Hydrol Process 14:1341–1355
Aravena R, Suzuki O, Pefia H, Pollastri A, Fuenzalida H, Grilli A (1999) Isotopic composition and origin of the precipitation in Northern Chile. Appl Geochem 14:411M22
Bhattacharya SK, Froehlich K, Aggrawal PK, Kulkarni KM (2003) Isotope variation in Indian monsoon precipitation: records from Bombay and New Delhi. Geophys Res Lett 30:2285. doi:10.1029/2003GL018453
Bowen GJ (2008) Spatial analysis of the intra-annual variation of precipitation isotope ratios and its climatological corollaries. J Geophys Res 113:D05113. doi:10.1029/2007JD009295
Bowen GJ et al (2005) Global application of stable hydrogen and oxygen isotopes to wildlife forensics. Oecologia 143:337–348
Bowen GJ, Wilkinson B (2002) Spatial distribution of δ 18O in meteoric precipitation. Geol 30:315–318
Breitenbach SFM, Adkins JF, Meyer H, Marwan N, Kumar KK, Haug GH (2010) Strong influence of water vapor source dynamics on stable isotopes in precipitation observed in Southern Meghalaya, NE India. Earth Planet Sci Lett 292:212–220
Brenninkmeijer CAM, Morrison PD (1987) An automated system for isotopic equilibration of CO2 and H2O for 18O analysis of water. Chem Geol 66:21–26
Chakrapani GJ, Saini RK (2009) Influence of monsoon on the variations in water discharge and sediment load in the Alaknanda and Bhagirathi rivers in Himalayas, India. J Asian Earth Sci 35:545–553
Chakrapani GJ, Saini RK, Yadav SK (2009) Chemical weathering rates in the Alaknanda–Bhagirathi river basins in Himalayas, India. J Asian Earth Sci 34:347–362
Chidambaram S, Prasanna MV, Ramanathan AL, Vasu K, Hameed S, Warrier UK, Srinivasamoorthy K, Manivannan R, Tirumalesh K, Anandhan P, Johnsonbabu G (2009) A study on the factors affecting the stable isotopic composition in precipitation of Tamil Nadu, India. Hydrol Process 23:1792–1800
Clark ID, Fritz P (1997) Environmental isotopes in hydrogeology. Lewis, Boca Raton, p 328
Craig H (1961) Standard for reporting concentrations of deuterium and Oxygen-18 in natural water. Science 133:1833–1834
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
Dansgaard W (1964) Stable isotopes in precipitation. Tellus 16:436–468
Das PK (2005) The Monsoons. National Book Trust of India, New Delhi
Datta PS, Tyagi SK, Chandrasekharan H (1991) Factors controlling stable isotopic composition of rainfall in New Delhi, India. J Hydrol 128:223–236
Epstein S, Mayeda T (1953) Variations of the 18O/16O ratio in natural waters. Geochim Cosmochim Acta 4:213–224
Ersek V, Mix AC, Clark PU (2010) Variations of δ 18O in rainwater from southwestern Oregon. J Geophys Res 115:D09109. doi:10.1029/2009JD013345
Froehlich K, Gibson JJ, Aggarwal PK (2002) Deuterium excess in precipitation and its climatological significance. In: Study of environmental change using isotope techniques. Vienna, International Atomic Energy Agency, 54–65
Gimeno L, Drumond A, Nieto R, trigo RM, Stohl A (2010) On the origin of continental precipitation. Geophys Res Lett 37:L13804
Gourcy LL, Groening M, Aggarwal PK (2005) Stable oxygen and hydrogen isotopes in precipitation. In: Aggarwal PK, Gat JR, Froehlich KFO (eds) Isotopes in the water cycle: past, present and future of a develo** science, pp 39-51
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
Gupta SK, Deshpande RD (2003) Synoptic hydrology of India from the data of isotopes in precipitation. Curr Sci 85:1591–1595
Kang S, Kreutz KJ, Mayewski PA, Qin D, Yao T (2002) Stable- isotope composition of precipitation over the northern slope of the central Himalaya. J Glaciol 48:519–526
Kumar B, Athavale RN, Sahay KSN (1982) Stable isotope geohydrology of the Lower Maner Basin, Andhra Pradesh, India. J Hydrol 59:315–330
Kumar B, Rai SP, Saravana Kumar U, Verma SK, Garg P, Vijaya Kumar SV, Jaiswal R, Purendra BK, Kumar SR, Pande NG (2010) Isotopic characteristics of Indian precipitation. Water Resour Res 46:W12548
Lawrence JR, Gedzelman SD, Dexheimer D, Cho H-K, Carrie GD, Gasparini R, Anderson CR, Bowman KP, Biggerstaff MI (2004) Stable isotopic composition of water vapor in the tropics. J Geophys Res 109:D06115. doi:10.1029/2003JD004046
Liang X, Liu Y, Wu G (2005) The role of land-sea distribution in the formation of the Asian summer monsoon. Geophys Res Lett 32:L03708
Liu Z, Tian L, Yao T, Gong T, Yin C (2008) Influence of moisture transport on stable isotope in precipitation in Yarlungzangbo River basin. Front Earth Sci China 2:49–57
Longinelli A, Anglesio E, Flora O, Iacumin P, Selmo E (2006) Isotopic composition of precipitation in Northern Italy: reverse effect of anomalous climatic events. J Hydrol 329:471–476
Lutz A, Thomas JM, Panorska A (2011) Environmental controls on stable isotope precipitation values over Mali and Niger, West Africa. Environ Earth Sci 62:1749–1759
Mukherjee TK, Chandrasekharan H (1993) Environmental stable isotopes of rainfall over Delhi and Bombay: some observations. J Nucl Agric Bio 22:34–41
Pande K, Padia JT, Ramesh R, Sharma KK (2000) Stable isotope systematics of surface water bodies in the Himalayan and Trans-Himalayan (Kashmir) region. Earth Planet Sci 109:109–115
Pang H, He Y, Lu A, Zhao J, Ning B, Yuan L, Song B (2006) Synoptic-scale variation of δ 18O in summer monsoon rainfall at Lijiang, China. China Sci Bull 51:2897–2904
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
Price RM, Swart PK, Willoughby HE (2008) Seasonal and spatial variation in the stable isotopic composition (δ 18O and δD) of precipitation in south Florida. J Hydrol 358:193–205
Rajan CK (1988) Studies on some characteristics of Indian rainfall. Ph.D. thesis, Cochin University of Science and Technology, Cochin, India
Ramesh R, Sarin MM (1992) Stable isotope study of Ganga (Ganges) river system. J Hydrol 139:49–62
Rao YP (1976) Southwest monsoon. Meteorological Monograph, Synoptic Meteorology 1/1976, 367 pp., Indian Meteorological Department Monograph, New Delhi
Risi C, Bony S, Vimeux F (2008) Influence of convective processes on the isotopic composition (δ 18O and δD) of precipitation and water vapor in the tropics: 2. Physical interpretation of the amount effect. J Geophys Res 113:D19306. doi:10.1029/2008JD009943
Rozanski K, Araguas-Araguas L, Gonfiantini R (1993) Isotopic patterns in modern global precipitation. In: Swart et al (eds) Climate change in continental isotopic records, vol 78. American Geophysical Union, Geophysical Monograph, pp 1–36
Rozanski K, Sonntag C, Munnich KO (1982) Factors controlling stable isotope composition of European precipitation. Tellus 34:142–150
Saravana Kumar U, Kumar B, Rai SP, Sharma S (2010) Stable isotope ratios in precipitation and their relationship with meteorological conditions in the Kumaon Himalayas. Indian J Hydrol 391:1–8
Sengupta S, Sarkar A (2006) Stable isotope evidence of dual (Arabian Sea and Bay of Bengal) vapour sources in monsoonal precipitation over north India. Earth Planet Sci Lett 250:511–521
Siegenthaler U, Oeschger H (1980) Correlation of O-18 in precipitation with temperature and altitude. Nature 285:314–317
Tian L, Yao T, White JWC, Yu W, Wang N (2005) Westerly moisture transport to the middle of Himalayas revealed from the high deuterium excess. China Sci Bull 50:1026–1030
Tian L, Ma L, Yu W, Liu Z, Yin C, Zhao Z, Tang W, Wang Y (2008) Seasonal variations of stable isotope in precipitation and moisture transport at Yushu, eastern Tibetan Plateau. Sci China Ser D-Earth Sci 51:1121–1128
van der Ent RJ, Savenije HHG, Schaefli B, Steele-Dunne SC (2010) Origin and fate of atmospheric moisture over continents. Water Resour Res 46:W09525
Vuille M, Bradley RS, Werner M, Healy R, Keimig F (2003) Modeling δ 18O in precipitation over the tropical Americas: 1 interannual variability and climatic controls. J Geophys Res 108:4174. doi:10.1029/2001JD002038
Warrier CU, Babu MP, Manjula P, Velayudhan KT, Shahul Hameed A, Vasu K (2010) Isotopic characterization of dual monsoon precipitation: evidence from Kerala, India. Curr Sci 98:1487–1495
Welker JM (2000) Isotopic (δ 18O) characteristics of weekly precipitation collected across the USA: an initial analysis with application to water source studies. Hydrol Process 14:1449–1464
Wu J, Ding Y, Ye B, Yang Q, Zhang X, Wang J (2010) Spatio-temporal variation of stable isotopes in precipitation in the Heihe River Basin, Northwestern China. Environ Earth Sci 61:1123–1134
Wulf H, Bookhagen B, Scherler D (2010) Seasonal precipitation gradients and their impact on fluvial sediment flux in the Northwest Himalaya. Geomorphology 118:13–21
Yadava MG, Ramesh R, Pandarinath K (2007) A positive ‘amount effect’ in the Sahayadri (Western Ghats) rainfall. Curr Sci 93:560–564
Yu W, Yao T, Tian L, Wang Y, Yin C (2005) Isotopic composition of atmospheric water vapour before and after the monsoon’s end in the Nagqu River basin. China Sci Bull 50:2755–2760
Yurtsever Y, Gat JR (1981) Atmospheric waters. In: stable isotope hydrology: Deuterium and Oxygen-18 in the water cycle, IAEA, (ed), technical report series no. 210, IAEA, Vienna, 103–142
Zhang X, Liu J, Sun W, Huang Y, Zhang J (2007) Relations between oxygen stavle isotopic ratios in precipitation and relevant meteorological factors in southwest china. Sci China Ser D 50:571–581
Acknowledgments
The authors are thankful to Dr. Pradeep Aggarwal, Head, Isotope Hydrology Section, IAEA, Vienna, Austria for getting some of our precipitation samples analysed at the IAEA, Isotope Hydrology Laboratory at Vienna. The authors express their sincere gratitude to Mr. S. K. Verma and Mr. Pankaj Garg of National Institute of Hydrology, Roorkee for help during sampling in the Bhagirathi Basin and to the Director, National Institute of Hydrology, Roorkee, for administrative and financial support. Authors are thankful to Mr. Vishal Gupta (RA) and Mr. Jamil Ahmad (SRA) for laboratory to analyse the sample. The authors thank Gunter Doerhoefer, Editor in Chief, EES and the anonymous reviewers for critically reviewing the manuscript. The authors are grateful to Department of Atomic Energy for funding the project entitled: “Streamflow Modelling of Bhagirathi River: Hydrograph Separation Using Isotopic and Geochemical Techniques” through BRNS, Mumbai.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Rai, S.P., Purushothaman, P., Kumar, B. et al. Stable isotopic composition of precipitation in the River Bhagirathi Basin and identification of source vapour. Environ Earth Sci 71, 4835–4847 (2014). https://doi.org/10.1007/s12665-013-2875-0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s12665-013-2875-0