 This study examined the potential effects of climate change on sediment yield in the Namo Basin, northern Laos. For general circulation models, GCMs were evaluated for their accuracy in predicting future climate conditions in the region. These models were then used to downscale data from the Mekong River Delta Change Model, Pre-C, and the Soil and Water Assessment Tool, SWAT, to determine how climate change could affect sediment yield in the Namo Basin. The results showed that temperatures in the area could rise by up to 3 degrees Celsius over the next century, with the greatest increases occurring in the dry season. Precipitation levels may also fluctuate significantly, with some areas experiencing decreases and others seeing increases. Overall, these changes could result in significant shifts in sediment yield, with the greatest increases seen in the wet season. This article was authored by Bishresta, MS Babel, Esmaski, and others.