The Appomattox watershed, located in central Virginia, covers an area of approximately 1,885 square miles. The watershed is characterized by a combination of lowlands and uplands, with the Appomattox River serving as the main waterway in the area. The region experiences a humid subtropical climate, with hot and humid summers and mild winters. The hydrology of the Appomattox watershed is influenced by a variety of factors, including precipitation patterns, land use, and topography. During the winter months, the area typically experiences some snowfall, although snowpack levels can vary significantly from year to year. Surface water in the Appomattox watershed is primarily used for drinking water, irrigation, and recreation. The area is home to several large reservoirs, including Lake Chesdin and Lake Matoaca, which provide water to thousands of residents in the surrounding communities. In recent years, the Appomattox watershed has experienced a number of interesting climatic trends, including increasing temperatures and more frequent and severe storms. These changes have had implications for water management and land use practices in the area, as stakeholders work to adapt to a changing climate.