Research Article
Controlling Factors of the Stable Isotope Composition in the Precipitation of Islamabad, Pakistan
Figure 1
Seasonal vertically integrated water vapor flux (300–1000 hpa) from 1992 to 2006 during (a) winter, (b) spring, (c) summer, and (d) autumn (units: kg·m−1·s−1). A star is showing Islamabad (33.65°N, 73.26°E).
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