Lake Mead: Understanding Temperature Dynamics And Ecosystem Impact
Lake Mead’s water temperature undergoes seasonal and long-term fluctuations influenced by evaporation, inflow, and precipitation. Thermal stratification, dissolved oxygen levels, and water volume are affected by seasonal variations. Gradual temperature changes over time are shaped by climate change and ENSO. Evaporation rates, water depth, and thermal stratification are influenced by temperature, humidity, and wind speed. Inflow from rivers and streams is a crucial water source, impacting depth, stratification, and oxygen levels. Thermal stratification creates distinct water layers, influencing dissolved oxygen distribution. Overall ecosystem health depends on the interplay of these factors, influenced by seasonal variations and climate change.