Event Description
Guest lecturer Dr. Richard Feely will discuss the present and future implications of increased temperature and CO2 levels as they relate to the health of our West Coast ocean ecosystems. He will also conduct a live demonstration of ocean acidification.
Carbon dioxide (CO2) is one of the most important “greenhouse” gases in the atmosphere affecting the radiative heat balance of the Earth. As a direct result of the industrial and agricultural activities of humans over the past two centuries, atmospheric CO2 concentrations have increased by about 100 parts per million.
The atmospheric concentration of CO2 is now higher than experienced on Earth for at least the last 800,000 years and is expected to continue to rise. This will lead to significant temperature increases in the atmosphere and ocean by the end of this century. The global ocean is the largest natural long-term reservoir for this excess heat and CO2. It absorbs approximately 85 percent of the heat and 30 percent of the anthropogenic (human-sourced) carbon released into the atmosphere since the beginning of the industrial era.









