Resource Details

The rain–runoff response of tropical humid forest ecosystems to use and reforestation in the Western Ghats of India

Literature: Journal Articles

Krishnaswamy J., Bonell M., Venkatesh B., Purandara B.K., Lele S., Kiran M.C., Reddy V., Badiger S., & Rakesh K.N. 2012. “The rain–runoff response of tropical humid forest ecosystems to use and reforestation in the Western Ghats of India” Journal of Hydrology, vol. 472–473, pp. 216–237.

Contact Info


  • Ashoka Trust for Research in Ecology and The Environment, Jakkur Post, Royal Enclave, Sriramapura, Bangalore 560 064, India
  • The Centre for Water Law, Water Policy and Science Under The Auspices of UNESCO, University of Dundee, Dundee DD1 4HN, Scotland, UK
  • Hard Rock Regional Centre, National Institute of Hydrology, Belgaum, Karnataka 590 001, India
  • TERI, WRC, H. No. 233/GH-2, Vasudha Housing Colony, Alto Santa Cruz, Bambolim, Goa 403 202, India


Journal of Hydrology

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Species Info

Acacia auriculiformis (exotic)


  • The authors expand on a previous study in the Western Ghats of India (Uttar Kannada, Karnataka State), that suggested a greater occurrence of infiltration-excess and potentially higher streamflow in degraded and reforested areas.  
  • Analyzing rainfall–streamflow data, they attempt to determine the impacts of different land cover types on stream discharge hydrograph components (viz, total flow, quickflow and delayed flow), the dominant stormflow pathways, and the impact of reforestation efforts on these processes.
  • Eleven experimental basins ranging from 7 to 23 ha were established in remnant tropical evergreen forest, degraded forest, and Acacia plantations in both coastal and upland locations and rainfall–streamflow observations were collected (daily and at 36 min intervals) between 2003–2005.
  • Using a variety of field (rainfall-runoff, permeability) and analytical methods (Double mass curves, HYDSTRA, linear model/ANOVA, and time-series lag analyses), the authors concluded that degraded forests have enhanced total stream discharge and quickflow both seasonally and by storm event while base flow is reduced.
  • Acacia plantations also have increased overland flow which suggests that they may not be very effective in restoring hydrologic functions in the short-term.
  • However subsurface water flow still continues in both degraded forest and Acacia plantations partly because their sub-soils are comparatively permeable.  Since evapotranspiration is less during the monsoon, differences in streamflow and run-off responses between land-cover is largely attributed to differences in soil infiltration and hydrologic pathways. 

Geographical Region

  • South Asia
  • Country

  • India
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