This study investigates the impact of climate change on water availability within the Klamath River Basin, a significant watershed in the western United States. Critical factors including precipitation, snowpack, and potential evapotranspiration (PET) was explored to understand how climate change dynamics may exacerbate water scarcity, and stakeholder conflicts in the region. The study uses 40 years of historical climate data of these sites (Big Red Mountain and Silver Lake), findings indicate a slight but statistically inconclusive decrease in both precipitation and snowpack, despite a significant positive correlation between temperature and PET. Observations from the study highlight the vulnerabilities of the Klamath River Basin's water resources, especially with warmer temperatures that may shift precipitation patterns from snow to increased rainfall, creating concerns for seasonal water storage and availability within the region. The impact of these shifts poses significant risks to agricultural, environmental, and cultural water needs, with implications for regional water management and climate adaptation strategies. The study emphasizes the urgent need for collaborative, data-informed approaches to equitable water allocation amidst growing climate pressures.