2014 U.S. AMOC Science Team Meeting;
Seattle, Washington, 9–11 September 2014
Posted inScience Updates
2014 U.S. AMOC Science Team Meeting;
Seattle, Washington, 9–11 September 2014
Variations in large-scale convection in the Atlantic Ocean are likely driven by wind.
Models and observations indicate that the Atlantic Meridional Overturning Circulation exhibits surprising short-term variability, driven largely by wind.
Scientists use satellite and robotic field data to study the environmental conditions driving phytoplankton blooms in the northwestern Mediterranean Sea.
How much does the Weddell Gyre contribute to the Global Overturning Circulation?