Research Article
Spatiotemporal Variability in the Hydrometeorological Time-Series over Upper Indus River Basin of Pakistan
Figure 3
Spatial distribution of trends detected by Mann–Kendall test and estimated by Sen’s method in seasonal maximum temperature showing change in °C·decade−1 (upward and downward arrows show positive and negative trends, respectively; blue arrow shows significant trend at α = 0.05 and green arrow shows insignificant trend).
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