Fig. 8From: Seasonal variation in isotopic composition and the origin of precipitation over BangladeshThe spatial distributions of the vertically integrated moisture flux and differences between the amount of moisture originating from the ocean (the Arabian Sea, the Bay of Bengal, the Indian Ocean) and land surface divided by the TPW in late March (pentad 16–18), early June (pentad 33–35), and late September (pentad 53–55). Red (blue) shaded indicated that moisture originating from the ocean (the land surface) was dominantBack to article page