Modelling surface run-off and trends analysis over India
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  • 作者:P K Gupta ; S Chauhan ; M P Oza
  • 关键词:Run ; off ; curve number ; Mann–Kendall test ; medium river basin.
  • 刊名:Journal of Earth System Science
  • 出版年:2016
  • 出版时间:August 2016
  • 年:2016
  • 卷:125
  • 期:6
  • 页码:1089-1102
  • 全文大小:3,360 KB
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciencesr>Geosciencesr>Extraterrestrial Physics and Space Sciencesr>
  • 出版者:Springer India
  • ISSN:0973-774X
  • 卷排序:125
文摘
The present study is mainly concerned with detecting the trend of run-off over the mainland of India, during a time period of 35 years, from 1971–2005 (May–October). Rainfall, soil texture, land cover types, slope, etc., were processed and run-off modelling was done using the Natural Resources Conservation Service (NRCS) model with modifications and cell size of 5×5 km. The slope and antecedent moisture corrections were incorporated in the existing model. Trend analysis of estimated run-off was done by taking into account different analysis windows such as cell, medium and major river basins, meteorological sub-divisions and elevation zones across India. It was estimated that out of the average 1012.5 mm of rainfall over India (considering the study period of 35 years), 33.8% got converted to surface run-off. An exponential model was developed between the rainfall and the run-off that predicted the run-off with an R2 of 0.97 and RMSE of 8.31 mm. The run-off trend analysed using the Mann–Kendall test revealed that a significant pattern exists in 22 medium, two major river basins and three meteorological sub-divisions, while there was no evidence of a statistically significant trend in the elevation zones. Among the medium river basins, the highest positive rate of change in the run-off was observed in the Kameng basin (13.6 mm/yr), while the highest negative trend was observed in the Tista upstream basin (−21.4 mm/yr). Changes in run-off provide valuable information for understanding the region’s sensitivity to climatic variability.

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