Over the next 100 years, the eastern United States will see more winter precipitation because atmospheric carbon dioxide levels are increasing. But more precipitation does not necessarily mean more snow, according to Arthur T. DeGaetano, a Cornell climatologist.
Retrieving every last bit of performance from the system while stopping short of the surge line is no small feat. Dig into sizing, tower selection, chilled water loads and stability, and condenser water management to leave no efficiency stone unturned. Read more in April issue