Southern New England is typically described as a “well-watered” temperate forest landscape. This is generally accurate until prolonged periods of low rainfall and/or mild winters substantially alter the water balance. Reservoir water levels begin to decrease when rates of withdrawal and use exceed rates of inflow from streams and aquifers. In extreme cases, such as the 1960s, the effect can persist for years. On Sunday, February 12 from 2 – 3 pm, please join Dr. Paul Barten, Professor of Forestry and Hydrology, University of Massachusetts Amherst, to learn more about the vital and dynamic connection between the forest …and the faucet. The free lecture is presented at the Quabbin Visitor Center, Ware Road in Belchertown, and for more information call 413-323-7221.