Abstract
The main objective of the study was to assess the integrated multiple hydrological hazards and their environmental and socio-economic risks in Himalaya through geographical information system (GIS) and database management system (DBMS). The Dabka Watershed constitutes a part of the Kosi Basin in the Kumaun Lesser Himalaya has been selected for the case illustration. The Dabka DBMS is constituted of three GIS modules, that is, geo-informatics, hydro-informatics and hazard-informatics. Through the integration and superimposing of these modules prepared Hydrological Hazard Index to identify the level of vulnerability for existing hydrological hazards and their socio-economic and environmental risks. The results suggested that geo-environmentally most stressed barren land areas have high rate of runoff, flood magnitude, erosion sediment load and denudation during rainy season particularly in the month of August (i.e., respectively, 84.56 l/s/km2, 871.80 l/s/km2, 78.60 t/km2 and 1.21 mm/year), which accelerates high hazards and their socio-economic and environmental risks, whereas geo-environmentally least stressed dense forest areas experience low rate of stream runoff, flood magnitude, erosion sediment load and denudation in the same season and month (i.e., respectively, 20.67 l/s/km2, 58.12 l/s/km2, 19.50 t/km2 and 0.20 mm/year) comparatively have low hazards and their socio-economic and environmental risks. The other frazzled geo-environment that also found highly vulnerable for natural hazards and their risks is agricultural land due to high stream runoff, flood magnitude, erosion sediment load and denudation rates (i.e., respectively, 53.15 l/s/km2, 217.95 l/s/km2, 90.00 t/km2 and .92 mm/year). This makes it necessary to take up an integrated and comprehensive sustainable land use policy for the entire Himalaya region based on the scientific interpretation of the crucial linkages between land use and hydrological hazards, that is, floods, erosion, landslides during rainy season and drought due to dry-up of natural springs and streams during summer season. The study would help the village, district and state development authority to formulate decision support system for alternate planning and management for the Himalaya region.
Similar content being viewed by others
References
Ali A, Qadir DA (1989) Study of river flood hydrology in Bangladesh with AVHRR data. Int J Remote Sens 47:1873–1891
Anbalagan R, Singh B (1996) Landslide hazard and risk assessment mapping of mountainous terrain: a case study from Kumaun Himalaya, India. Eng Geol 43:237–246
Apel H, Thieken AH, Merz B, Blöschl G (2006) A probabilistic modelling system for assessing flood risk. Nat Hazards 38:79–100
Auden JB (1934) The geology of the Krol belt. Rec Geol Surv India 67:357–454
Bajracharya B, Shrestha AB, Rajbhandari L (2007) Glacial lake outburst floods in the Sagarmatha region: hazard assessment using GIS and hydrodynamic modelling. Mt Res Dev 27:336–344
Bates PD, Horritt MS, Smith CN, Mason D (1997) Integrating remote sensing observations of flood hydrology and hydraulic modeling. Hydrol Process 11(14):1777–1795
Bates PD, Marks KJ, Horritt MS (2003) Optimal use of high-resolution topographic data in flood inundation models. Hydrol Process 17(3):537–557
Birkland TA, Burby RJ, Conrad D, Cortner H, Michener WK (2003) River ecology and flood hazard mitigation. Nat Hazards Rev 4(1):46–54
Brivio PA, Colombo R, Maggi M, Tomasoni R (2002) Integration of remote sensing data and GIS for accurate mapping of flooded areas. Int J Remote Sens 23(3):429–441
Brody SD, Zahran S, Highfield WE, Grover H, Vedlitz A (2007) Identifying the impact of the built environment on flood damage in Texas. Disasters 32(1):1–18
Buchele B, Kreibich H, Kron A, Thieken A, Ihringer J, Oberel P, Merz B, Nestmann F (2006) Flood-risk mapping: contributions towards an enhanced assessment of extreme events and associated risks. Nat Hazards Earth Syst 6:485–503
Clandillon S, De Fraipont P (2000) Environmental risks within natural areas; the Ill River’s flood plain, Alsace, France—water quality and flooding, surveys. Geophysics 21(2–3):223–228
Cruz RAD (1992) The determination of suitable upland agricultural areas using GIS technology. Asian pac Remote Sens J 5:123–132
Delmeire S (1997) Use of ERS-1 data for the extraction of flooded areas. Hydrol Process 11(10):1393–1396
Fuchs G, Sinha AK (1978) The tectonics of the Garhwal-Kumaun Lesser Himalaya. Jahrb Geol BA 121(2):219–241
Gregory KG, Walling DE (1973) Drainage basin form and processes: a geomorphological approach. Edward Arnold, London
Gupta P, Anbalagan R, Jain N, Sikdar PK (2001) Landslide hazard evaluation and geostatistical studies in Garhwal Himalaya, India. Rock Mech Tunn Technol 1(1):41–59
Haigh MJ, Rawat JS, Bartarya SK (1988) Environmental indicators of landslide activity along the Kilbury road, Nainital, Kumaun Lesser Himalaya. Mt Res Dev 9(1):25–33
Hamilton LS (1987) What are the impacts of Himalayan deforestation on the Ganges–Brahmaputra lowland and delta? Assumptions and facts. Mt Res Dev 7(3):256–263
Imhoff ML, Vermillion C, Story MH, Choudhury AM, Gafoor A, Polcyn F (1987) Monsoon flood boundary delineation and damage assessment using space borne imaging radar and Landsat data. Photogramm Eng Remote Sens 47:405–413
Islam M, Sado K (2000) Flood hazard assessment in Bangladesh using NOAA AVHRR data with geographical information system. Hydrol Process 14(3):605–620
Ives JD (1989) Deforestation in the Himalaya: the cause of increased flooding in Bangladesh and Northern India. Land Use Policy 6:187–193
Jain SK, Kumar S, Varghese J (1994) Estimation of soil erosion for a Himalayan watershed using GIS technique. Geol Soc Lond 151(1):217–220
Jain SK, Singh RD, Jain MK, Lohani AK (2005) Delineation of flood-prone areas using remote sensing techniques. Water Resour Manage 19(4):333–347
Jonkman SN (2005) Global perspectives on loss of human life caused by floods. Nat Hazards 34:151–175
Larson L, Pasencia D (2001) No adverse impact: new direction in floodplain management policy. Nat Hazards Rev 2(4):167–181
Muller L (1968) The rock slide in the Vaiont Valley. Rock Mech Eng 2:148–212
Nearing MA, Jetten V, Baffaut C, Cerdan O, Couturier A, Hernandez M, Le Bissonnais Y, Nichols MH, Nunes JP, Renschler CS, Souchère V, Oost K (2005) Modeling response of soil erosion and runoff to changes in precipitation and cover. Catena 61(2–3):131–154
Nibanupudi HK, Mool P, Rawat PK (2012) Climate change resilience and disaster risk reduction in the Hindu Kush—Himalayan Region. Int J Mt Res Dev, Accepted and in Press
Overton IC (2005) Modelling floodplain inundation on a regulated river: integrating GIS, remote sensing and hydrological models. River Res Appl 21(9):991–1001
Pant CC, Goswami PK (2003) Tide-storm dominated shelf sequence of the Neoproterozoic Blaini Formation and its implications on the sedimentation history of Krol belt, Kumaun Lesser Himalaya, India. Nepal Geol Soc 28:19–39
Rawat JS, Rawat MS (1994) Accelerated erosion and denudation in the Nana Kosi Watershed, Central Himalaya. Mt Res Dev 14(1):25–38
Rawat PK, Tiwari PC, Pant CC (2011a) Modeling of stream runoff and sediment output for erosion hazard assessment in Lesser Himalaya; need for sustainable land use plane using remote sensing and GIS: a case study. Int J Nat Hazards 59:1277–1297
Rawat PK, Tiwari PC, Pant CC, Sharama AK, Pant PD (2011b) Climate change and its geo-hydrological impacts on mountainous terrain: a case study through remote sensing and GIS modelling. Int Sci Res J 3(1):51–69
Rawat PK, Tiwari PC, Pant CC (2011c) Morphometric analysis of third order river basins using high resolution satellite imagery and GIS technology: special reference to natural hazard vulnerability assessment. E-Int Sci Res J 3(2):70–87
Rawat PK, Tiwari PC, Pant CC (2012) Climate change accelerating land use dynamic and its environmental and socio-economic risks in Himalaya: mitigation through sustainable land use. Int J Clim Change Strategy Manag, Accepted and in press for upcoming issue
Scheling D (1988) Flooding and road destruction in Eastern Nepal [Sun-Koshi]. Mt Res Dev 8(1):78–79
Sharma PK, Chopra R, Verma VK, Thomas A (1996) Flood management using remote sensing technology: the Punjab (India) experience. Int J Remote Sens 17(17):3511–3521
Shrestha AB (2009) Climate change in the Hindu Kush-Himalayas and its impacts on water and hazards. Asia Pac Mt Netw Bull 9:1–5
Sing SK (2006) Spatial variability in erosion in the Brahmaputra basin: causes and impacts. Curr Sci 90(9):1272–1276
Strahler AN (1956) Quantitative slope analysis. Bull Geol Soc Am 67:571–596
Tiwari PC (2000) Land use changes in Himalaya and their impact on the plains ecosystem: need for sustainable land use. Land Use Policy 17:101–111
Townsend PA (2001) Mapping seasonal flooding in forested wetlands using multi-temporal radarsat SAR. Photogramm Eng Remote Sens 67:857
Valdiya KS, Bartarya SK (1989) Problem of mass-movement in part of Kmaun Himalaya. Curr Sci 58:486–491
Wentworth CK (1950) A Simplified method of determining the average slope of land surfaces. Am J Sci Ser 5:20
Zhou C, Luo J, Yang C, Li B, Wang S (2000) Flood monitoring using multi-temporal AVHRR and RADARSAT imagery. Photogramm Eng Remote Sens 66:633–638
Acknowledgments
This study constitutes part of multidisciplinary project, Department of Science and Technology (D.S.T.) Gov. of India, No.ES/11/599/01 Dated 27/05/2005, “Geo-environmental Appraisal of the Dabka Watershed, Kumaun Lesser Himalaya, District Nainital: A Model Study for Sustainable Development” funded to Prof. Charu C. Pant, Head Department of Geology Kumaun University Nainital. Dr. Pradeep K. Goswami, Department of Geology, Kumaun University Nainital and Dr. P. K. Joshi IIRS-Dehradun helped in GIS analysis for which authors indebted to them. Thanks to Shri M.S. Bargali, project assistant helped during the intensive field work.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Rawat, P.K., Tiwari, P.C. & Pant, C.C. Geo-hydrological database modeling for integrated multiple hazards and risk assessment in Lesser Himalaya: a GIS-based case study. Nat Hazards 62, 1233–1260 (2012). https://doi.org/10.1007/s11069-012-0144-2
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11069-012-0144-2