Abstract

Autonomous Observations of the Ocean Biological Carbon Pump Carbon Flux Explorer at Dawn w R/V Sproul in the San Clemente Basin. James K. B. Bishop 1,2 1. Professor Marine Science, Department of Earth and Planetary Science, U.C. Berkeley, Berkeley, CA, 94720-4767; jkbishop@berkeley.edu; 2. Faculty Senior Scientist, Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, 94720-0001 Abstract Prediction of the substantial biologically mediated carbon flows in a rapidly changing and acidifying ocean requires model simulations informed by observations of key carbon cycle processes on the appropriate space and time scales. From 2000 to 2004, the National Oceanographic Partnership Program (NOPP) supported the development of the first low-cost fully-autonomous ocean profiling Carbon Explorers that demonstrated that year-round real-time observations of particulate organic carbon (POC) concentration and sedimentation could be achieved in the world's ocean. NOPP also initiated the development of a sensor for particulate inorganic carbon (PIC) suitable for operational deployment across all oceanographic platforms. As a result, PIC profile characterization that once required shipboard sample collection and shipboard or shore based laboratory analysis, is now possible to full ocean depth in real time using a 0.2W sensor operating at 24 Hz. NOPP developments further spawned US DOE support to develop the Carbon Flux Explorer, a free-vehicle capable of following hourly variations of particulate inorganic and organic carbon sedimentation from near surface to kilometer depths for seasons to years and capable of relaying contemporaneous observations via satellite.

Highlights

  • Prediction of the substantial biologically mediated carbon flows in a rapidly changing and acidifying ocean requires model simulations informed by observations of key carbon cycle processes on the appropriate spatial and temporal scales

  • We summarize below the development of the Optical Sedimentation Recorder (OSR) and the integration of OSR with a highly modified SOLO float to produce a first prototype Carbon Flux Explorer (CFE; Figure 4 and title page photo)

  • We focused on sensors for measuring particulate organic carbon (POC) and particulate inorganic carbon (PIC) pools and fluxes, and their integration with low-power, long-lived Lagrangian floats

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Summary

Carbon Pump

B. B i s h op Carbon Flux Explorer awaiting recovery at dawn at the end of its first 1.5-day mission in the San Clemente Basin near San Diego, CA, June 2007. Photo credit: Roy Kaltschmidt, Lawrence Berkeley National Laboratory

Intermediate Water
Little is known about how carbonate
Work is required to transition
Image Cycle
Reference s
Atlantic Pacific
Findings
The authors would like to acknowledge the National Oceanographic Partnership
Full Text
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