Abstract: Globally, changes in stable isotope ratios of oxygen and hydrogen (δ18Oand δD) in the meteoric water cycle result from distillation and evaporation processes. Isotope fractionation occurs when air masses rise in elevation, cool, and reduce their water-vapor holding capacity with decreasing temperature. Assuch, δ18Oand δDvalues from a variety of sedimentary archives are often used to reconstruct changes in continental paleohydrology as well as paleoaltimetry of mountain ranges. Based on 234 stream-water samples, wedemonstrate that areas experiencing deep convective storms in the eastern south?central Andes (22?28◦S) do not show the commonly observed relationship between δ18Oand δDwith elevation. These convective storms arise from i...