Skip to main content

Advertisement

Log in

Rainfall variability and indices of extreme rainfall-analysis and perception study for two stations over Central Himalaya, India

  • Original Paper
  • Published:
Natural Hazards Aims and scope Submit manuscript

Abstract

The analysis of rainfall pattern and indices of extreme rainfall events is performed for two meteorological stations located in the Central Himalayan Region which is highly vulnerable to rain-induced hazards. The records of these rain-induced disasters suggest that such events are generally observed in later part of monsoon season, when soil is saturated after monsoon rains. An attempt is made here to test trends of 19 different extreme rainfall indices that have been widely used in the literature, using daily rainfall data for two urban centres (Nainital and Almora) over the period 1992–2005. We have used statistical tools such as Sen’s method and Mann–Kendall test for detection of trend in annual rainfall, monsoon rainfall, number of rainy days and 1-day extreme rainfall. Principal component analysis gives the correlation between different extreme rainfall indices. Time series of principal components are representing the trends of extreme indices, their variation and interrelation between different indices. The perception study conducted in the same sites indicates that extreme rainfall events and change in rainfall amount and timing are well perceived by the local people.

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

Access this article

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

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

References

  • Borgaonkar HP, Pant GB, Kumar KR (1998) A study of seasonal patterns and magnitudes of climatological inputs to the hydrology of Western Himalaya. In: Tappeiner U, Ruffini FV, Fumai M (eds) HeadWater’98 hydrology, water resources and ecology of mountain areas. Poster volume of the international conference HEADWATER’98, European Academy, Bolzano, pp 235–239

  • Gansser H (1964) Geology of the Himalaya. Inter Science Publication, Wiley, London, p 289

    Google Scholar 

  • Goswami P, Ramesh KV (2007) Extreme rainfall events: vulnerability analysis for disaster management and observation system design. Research Report, RRCM 0703

  • Goswami BN, Venugopal V, Sengupta D, Madhusoodanan MS, Xavier PK (2006) Increasing trend of extreme rain events over India in a warming environment. Science 314:1442–1445. doi:10.1126/science.1132027

    Article  Google Scholar 

  • Graham S (1988) Precipitation: process and analysis. Wiley, New York, p 455

    Google Scholar 

  • Guhathakurta P, Menon P, Mazumdar AB, Sreejith OP (2010) Change in extreme rainfall events and flood risk in India during the last Century. NCC Research Report, RR No. 3

  • http://support.sas.com/publishing/pubcat/chaps/55129.pdf. Accessed 6th Oct 2011

  • IPCC (2007) Climate change 2007: the physical science basis. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge and New York

  • Kaiser HF (1959) Computer program for varimax rotation in factor analysis. Psychol Meas 19:413–420

    Article  Google Scholar 

  • Kendall MG (1975) Rank correlation methods, 4th edn. Charles Griffin, London

    Google Scholar 

  • Kothyari UC, Singh VP (1992) Temporal variation of rainfall and temperature in the Ganga Basin. Proceedings of the international symposium on hydrology of mountainous areas, pp 13–28

  • Kripalani RH, Kulkarni A (1997) Climatic impact of El Nino/La Nina on the Indian monsoon: a new perspective. Weather 52:39–46

    Article  Google Scholar 

  • Kripalani RH, Kulkarni A (2003) Indian monsoon variability in a global warming scenario. Nat Hazards 29:189–206

    Article  Google Scholar 

  • Krishna Kumar K, Rajagopalan B, Cane MA (1999) On the weakening relationship between the Indian monsoon and ENSO. Science 284:2156–2159

    Article  Google Scholar 

  • Kumar K, Satyal GS (1999) Cost analysis of losses caused by the Malpa landslide in Kumaun Himalaya: a basic framework for risk assessment. Curr Sci 77(8):1023–1028

    Google Scholar 

  • Kumar K, Joshi V, Joshi S, Supyal KS, Roy J, Ghosh A (2004) Global change impact assessment for Himalayan mountain regions—India report. Final Technical Report, 158 p

  • Kumar K, Joshi S, Joshi V (2008) Climate variability, vulnerability, and coping mechanism in Alaknanda catchment, Central Himalaya, India. Ambio 37(4):286–291

    Article  Google Scholar 

  • Mann HB (1945) Non-parametric tests against trend. Econometrica 13:245–259

    Article  Google Scholar 

  • Mooley DA (1997) Variation of summer monsoon rainfall over India in El Nino. Mausam 48:413–420

    Google Scholar 

  • Parthasarathy B, Pant GB (1985) Seasonal relationships between Indian summer rainfall and the southern oscillation. J Clim 5:369–378

    Article  Google Scholar 

  • Peralta-Hernandez AR, Balling RC, Barba-Martinez LR (2009) Comparative analysis of indices of extreme rainfall events: variations and trends from southern Mexico. Atmosfera 22(2):219–228

    Google Scholar 

  • Powar KB, Gairola VH, Dixit PC (1969) Relation between volcanism, plutonism, regional metamorphism and tectonism in Himalayan orogeny as related to the rocks of a part of Kumaun Himalaya. Public Centre of Advanced Study in Geology Panjab University Chandigarh, pp 1–7

  • Preisendorfer RW (1988) Principal component analysis in meteorology and oceanography. Elsevier, New York, p 425

    Google Scholar 

  • Rajeevan M, Bhate MJ, Kale JD, Lal B (2006) High-resolution daily gridded rainfall data for the Indian region: analysis of break and active monsoon spells. Curr Sci 91:296–306

    Google Scholar 

  • Rasmusson EM, Carpenter TH (1983) The relationship between eastern equatorial Pacific Sea surface temperatures and rainfall over India and Sri Lanka. Mon Weather Rev 111:517–528

    Article  Google Scholar 

  • Revadekar JV, Kulkarni A (2008) The El Nino-Southern Oscillation and winter precipitation extremes over India. Int J Climatol 28:1445–1452

    Article  Google Scholar 

  • Richman MB (1986) Rotation of principal components. J Climatol 6:293–335

    Article  Google Scholar 

  • Roy SS, Goodrich GB, Balling RC (2003) Influence of El Niño/southern oscillation, Pacific decadal oscillation, and local sea-surface temperature anomalies on peak season monsoon precipitation in India. Clim Res 25:171–178

    Article  Google Scholar 

  • Sen PK (1968) Estimates of the regression coefficient based on Kendall’s tau. J Am Stat As 63:1379–1389

    Article  Google Scholar 

  • Sikka DR (1980) Some aspects of large scale fluctuations of summer monsoon rainfall over India in relation to fluctuations in the planetary and regional scale circulation parameters. Proc Indian Acad Sci (Earth Planet Sci) 89:179–195

    Google Scholar 

  • Srivastava P, Mitra G (1994) Thrust geometries and deep structures of the Outer and Lesser Himalaya, Kumaun and Garhwal (India): implications for evolution of the Himalayan fold and thrust belt. Tectonics 13:89–109

    Article  Google Scholar 

  • Thiele HA (1950) Rank-invariant method of linear and polynomial regression analysis, part 3. Proc K Ned Akad Wet A 53:1397–1412

    Google Scholar 

  • Valdia KS, Joshi DD, Sanwal S et al (1984) Geomorphic development across the active main boundary thrust: an example from the Nainital Hills in Kumaun Himalaya. J Geol Soc 25:761–774

    Google Scholar 

  • Valdiya KS (1976) Himalayan transverse faults and folds and their parallelism with source structures of North Indian Plains. Tectonophysics 32:353–386

    Article  Google Scholar 

  • Valdiya KS (1980) Discovery of late Paleozoic brachiopod in the upper krol of the neonatal Hills, Kumaun Himalaya. J Geol Soc India 21:97–101

    Google Scholar 

  • Valdiya KS (1988) The tectonics and evolution of the central sector of Himalaya. Philos Trans R Soc Lond A326:151–175

    Article  Google Scholar 

Download references

Acknowledgments

We are thankful to the Director G. B. Pant, Institute of Himalayan Environment and Development, Kosi-Katarmal, Almora, for his motivating attitude and timely help during the work.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Sneh Joshi.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Joshi, S., Kumar, K., Joshi, V. et al. Rainfall variability and indices of extreme rainfall-analysis and perception study for two stations over Central Himalaya, India. Nat Hazards 72, 361–374 (2014). https://doi.org/10.1007/s11069-013-1012-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11069-013-1012-4

Keywords

Navigation