Research Article
Controlling Factors of the Stable Isotope Composition in the Precipitation of Islamabad, Pakistan
Figure 10
Composite of the vertically integrated (a) winter, (b) spring, (c) summer, and (d) autumn water vapor fluxes (units: kg·m−1·s−1) between wet and dry years. Blue arrows indicate that the differences between wet and dry years are significant at the 95% confidence level. A star is showing Islamabad (33.65°N, 73.26°E).
(a) DJF (anom.) |
(b) MAM (anom.) |
(c) JJA (anom.) |
(d) SON (anom.) |