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The percentage of human-induced runoff reduction to total runoff reduction is approximate 61.5%%.
Human-induced runoff reduction accounts for 61.5%% of the total runoff reduction over 1980 2013.
However, the total runoff reduction increases from 40.6 mm in 1980 1999 to 69.2 mm in 2000 2013 due to the environmental changes.
The integrated GI configuration has effective reduction percentage, such as the total runoff reduction was ranged from 100%too 85.0% and the peak flow reduced 100 92.8%.
Runoff depth over the catchment in 1980 2013 reduced by 52.4 mm compared to the previous period, in which human activities and climate change contribute 61.5 and 38.5 % of the total runoff reduction, respectively.
Moreover, studying the drivers of changes in runoff of the Luan River over the period of 1958 2008, Zeng et al. (2015) found climate-induced runoff reduction accounted for 28.3 46.8%% of the total runoff reduction while human activities played a principal role in decreases of runoff.
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The decline of river discharge was due to the reduction of total runoff from the lake watershed.
All in all, this reduction in total runoff could prevent not only stream bank from getting eroded only but also contributes to restoring pre-development hydrology which has an important role in maintaining the aquatic life and restoring the ecological system.
In addition, we found that absolute runoff reductions have increased in response to human activities and climate change, with average reductions of 70.1% and 29.9% in total runoff being caused by human activities and climate change, respectively.
In the United States alone, total water utilization is equivalent to one-third of total runoff, with about 2 percent of the water used coming from underground wells.
For the world as a whole, groundwater contributes perhaps 30 percent of total runoff, although the proportion varies widely from basin to basin, within basins, and through time.
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