Diurnal variation in robotic observations of carbon export in California coastal waters
One of the most interesting components of the global carbon cycle is the movement of carbon from the atmosphere to the deep ocean, where it is deposited as particulates, a process called the Biological Carbon Pump (BCP). The BCP combines physical oceanography and biology, as the majority of the carbon dioxide that is pulled from the atmosphere into our oceans for biological processes in the photic zone, and then moves from the surface to the deep ocean as zooplankton excrement. Using robotic devices to monitor this chemical and biological cycle, I hope to better understand the diurnal fluctuations in the BCP from the atmosphere to the deep ocean, and therefore better understand how surface zooplankton contribute to carbon cycling on our planet.
Message to Sponsor
- Major: Marine Science, Integrative Biology
- Mentor: Jim Bishop