highly significantp = 0.0001
Considered separately for Udupi ( Figures 5A,B ) and Shimoga ( Figure 5C,D ), the differences between loads detected in the monsoon season in Udupi (3.47 × 10 3 ; IQR: 1.13 × 10 3 – 1.55 × 10 4 ) and Shimoga (5.02 × 10 3 ; IQR: 3.29 × 10 3 – 1.78 × 10 4 ) compared to the summer season in Udupi (1.55 × 10 3 ; IQR: 1.35 × 10 2 – 4.99 × 10 3 ) and Shimoga (9.18 × 10 2 ; IQR: 5.37 × 10 1 – 1.80 × 10 3 ) were again highly significant ( p = 0.0001 and p < 0.0001, respectively).