Fig. 2From: Seasonal variation in isotopic composition and the origin of precipitation over BangladeshDaily variations in the amount (bar) and δ18O values (cross) of precipitation in 2010 at Sylhet (a), Dhaka (b), and Chittagong (c). Red and blue crosses indicate observations and IsoGSM simulations, respectively. The correlation coefficient (R), number of samples (N), probability (p), and root mean square error (RMSE) between the observed and simulated δ18O values of precipitation are shownBack to article page