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MIT-WHOI Joint Program announces new leadership

After 13 years as director of the MIT-Woods Hole Oceanographic Institution (WHOI) Joint Program in Oceanography/Applied Ocean Science and Engineering, Ed Boyle, professor of ocean geochemistry in the MIT Department of Earth, Atmospheric and Planetary

MIT-WHOI Joint Program announces new leadership

Study reveals uncertainty in how much carbon the ocean absorbs over time

Credits: Credit: © Woods Hole Oceanographic Institution Caption: When they die, phytoplankton collectively sink through the water column as “marine snow,” carrying with them the carbon that they initially absorbed. Shown here are white flakes and pellets that typically make up sinking marine material. Credits: Credit: © Woods Hole Oceanographic Institution Previous image Next image The ocean’s “biological pump” describes the many marine processes that work to take up carbon dioxide from the atmosphere and transport it deep into the ocean, where it can remain sequestered for centuries. This ocean pump is a powerful regulator of atmospheric carbon dioxide and an essential ingredient in any global climate forecast.

Study reveals uncertainty in how much carbon ocean absorbs over time

Massachusetts Institute of Technology The ocean’s “biological pump” describes the many marine processes that work to take up carbon dioxide from the atmosphere and transport it deep into the ocean, where it can remain sequestered for centuries. This ocean pump is a powerful regulator of atmospheric carbon dioxide and an essential ingredient in any global climate forecast. But a new MIT study points to a significant uncertainty in the way the biological pump is represented in climate models today. Researchers found that the “gold standard” equation used to calculate the pump’s strength has a larger margin of error than previously thought, and that predictions of how much atmospheric carbon the ocean will pump down to various depths could be off by 10 to 15 parts per million.

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