In the northern part of Iceland an unknown force is creating mysterious changes in the mud of its deepest lakes. Every 80-100 years, the chemical fingerprint of the lake mud changes dramatically for a brief time and then returns to what it was before. This bizarre cyclical behavior has been going on for at least 900 years and nothing like it has been reported anywhere else in the world. If Lisa Doner is right, the answer to this mystery lies in a climate feature called the North Atlantic Oscillation.
Doner, a research professor at the Center for the Environment at Plymouth State University, was recently awarded a $600,000 National Science Foundation grant to study the deposits in the bottom of lakes in Iceland and how the North Atlantic Oscillation affects the process of deposition. Doner explains, “The North Atlantic Oscillation, or NAO for short, and a related, larger circulation pattern called the Arctic Oscillation (AO), together control most of the Northern Hemisphere’s year-to-year atmospheric variation. The NAO and AO have been credited with causing many of the recent patterns of drought, flooding and severe weather in North America, Europe and the Middle-East, including last winter’s repeated snowstorms in the southeast and the colder and wetter winters in NH.”
So why is Iceland the only region that seems to show this phenomenon? And how does this relate to our regional climate?













