Fig. 3From: Seasonal variation in isotopic composition and the origin of precipitation over BangladeshThe relation between the amount of and δ18O values of precipitation for observations (a, b, c) and IsoGSM simulations (d, e, f) at Sylhet (a, d), Dhaka (b, e), and Chittagong (c, f). Values with a simulated precipitation amount of < 1.0 mm/day were excludedBack to article page