Associate Professor Morgan State University, Maryland, United States
Abstract Submission: This research explores the influence of temperature variations, driven by climate change, on the volumetric discharge of the Herring Run, a river system located in Baltimore, Maryland. Using data collected from the United States Geological Survey (USGS) from 2013 to 2022, the study examines how temperature increases affect river discharge, with a particular focus on the seasonal changes and sediment buildup during periods of low flow. The findings indicate a clear inverse relationship between rising temperatures and decreasing river discharge, particularly during the summer months when temperatures are highest. This reduction in discharge is associated with increased sediment accumulation, potentially impacting the overall health and flow of the watershed. The research underscores the growing risks of drought in the area due to insufficient rainfall during high-temperature periods, emphasizing the need for long-term monitoring and improved hydrological data to mitigate potential environmental impacts. Recommendations include the installation of permanent flow recording stations to provide more accurate data for future river modeling and management efforts.
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