The values of pH in the rainy season were found to be in the range of 7.38 ± 0.58 and 7.11 ± 0.59 for Site 1 and Site 2, respectively.
The values of pH in the rainy season for Site 1 were found to be in the range of 7.38 ± 0.583 as compared to the pH of the effluent coming from Site 2, i.e. 7.11 ± 0.598 which shows the non-significant difference.
Despite the heightened anthropogenic influence of the rainy season, values of both metals in the sediments were much lower than their average values in the Earth's crust throughout the sampling period.
After the last significant rain, the ecosystem respiration tended to decrease back to low values (~2.4 g C m−2 dat−1) athehendnd of rainy season and during the subsequent dry season.
The remnant forests had a significant effect (P-value <0.05, R 2 = 0.40) on the spatial variability of the number of rainy days observed over two years (2012 2013), but had little effect on the variability of rainfall distribution.
Seasonal variation exists in the tritium values as rainy season samples systemically are higher than those of the dry season samples.
The maximum mean monthly value of approx. 6.3 m3/s was observed in January which is timed in the mid of rainy season.
Higher values of NDVIs are often most correlated with rainfall occurrence in preceding weeks, particularly during the beginning of rainy seasons.
There were significant differences in the pH values of stream and well samples between the rainy and dry season (Z = −3.748; Z = −3.531 with P < 0.05 for stream and well respectively).
Not in a month of rainy Mancunian Sundays.
