Beneath the Amargosa desert of the southwest United States lies a hidden gem for climate research. The Devils Hole cave system, named after its bottomless depths, provides a window into the vast desert aquifer below. The cave system is home to a peculiar type of calcite deposit. As groundwater slowly passes through the cave, calcite precipitates layer by layer on the rock walls. "These thin layers have been accumulating on the walls for nearly one million years," explains Kathleen Wendt from the Quaternary Research Group in the Department of Geology at the University of Innsbruck. "The height of ancient deposits in Devils Hole cave tell us how high the water table was in the past."
Together with her colleagues, the geologist has conducted research in the cave for several years (see report: https:/
Follow the water
Rises and falls in the local water table provide important clues to how rainfall patterns in the southwest United States have changed. Most of the rainfall that recharges the desert aquifer comes from winter storms that move east along the Pacific storm track. The position and intensity of these winter storms depend on many factors, including surface ocean temperatures and the strength of pressure systems in the eastern Pacific. Whenever these factors changed dramatically in the past, such as during an ice age, the position of the Pacific storm track shifted in latitude. "Shifts in the Pacific storm track influenced the amount of rainfall reaching the southwest United States, resulting in pronounced changes in the Devils Hole water table height," says Kathleen Wendt. "The past has shown us that this 'water supplier' is incredibly sensitive to global climate changes."
Lessons from the Amargosa desert's distant past point to an even drier future. The already hot and dry southwest United States region is particularly sensitive to increasing global temperatures. "Climate models predict that this region will experience even higher temperatures and less precipitation in the next century," says Kathleen Wendt. The predicted drying trend is largely due to a gradual northward shift of the Pacific storm track, which will further reduce the amount of rainfall reaching the southwest in the future. "Understanding the natural variability of the Pacific storm track over long periods of time is an important part of understanding how it will behave in the future," explains the geologist. "This data helps improve our long-term prognoses of future climate developments, which are expected to be even more rapid and extreme due to human influences."