EVALUATING THE IMPACTS OF ENVIRONMENTAL CHANGE ON PLAYA FORM AND FUNCTION
Playas occupy the lowest elevational position within internally-drained watersheds, so water and wind- and water-transported material accumulates within playas. Playa function or health is directly related to sedimentation rates; if sedimentation rates are accelerated above geologic norms, sediment deposited within playas can reduce pore space and infiltration rates and decrease playa storage capacity and hydroperiod. This can result in reduced vegetative cover and habitat value, and, in extreme cases, completely fill-in playas. Linking sedimentation rates and processes to landscape-scale variables, such as land use, vegetation cover, and climate is essential to provide a robust model to examine and assess playa functions. While there is a growing body of research concerning the role of land use on sedimentation within playas, the impacts of climate change on playa sedimentation rates and processes have often been overlooked.
This research project establishes essential benchmark information about natural playa sedimentation processes and rates and determines how these processes and rates have responded to changes in land use, vegetative cover, and climate. Research directly assesses several questions related to sedimentation within playas, with emphasis placed on evaluating impacts to playa hydrological and ecological functions. By evaluating multiple playas that have undergone a range of land use changes, including efforts to protect and improve playa functions, the effectiveness of grassed buffers as a sediment management technique is directly assessed. By taking a landscape-scale approach, research also addresses questions related to habitat and landscape functions and conditions for both playas and the surrounding uplands.