Carbon export and fate beneath a dynamic upwelled filament off the California coast

• Published in: Biogeosciences 2021-05, Vol.18 (10), p.3053-3086
• Main Authors: Bourne, Hannah L, Bishop, James K. B, Connors, Elizabeth J, Wood, Todd J
• Format: Article
• Language: English
• Subjects: Aggregates; Analysis; Aquatic crustaceans; California Current; Carbon; Carbon cycle; Coasts; Confidence intervals; Depth; Ecological research; Exports; Fluctuations; Fluxes; Locations (working); Offshore; Particle settling; Pellets; Plankton; Productivity; Satellites; Sediment traps; Ships; Transmissometers
• ISSN: 1726-4189; 1726-4170; 1726-4189
• DOI: 10.5194/bg-18-3053-2021

To understand the vertical variations in carbon fluxes in biologically productive waters, four autonomous carbon flux explorers (CFEs), ship-lowered CTD-interfaced particle-sensitive transmissometer and scattering sensors, and surface-drogued sediment traps were deployed in a filament of offshore flowing, recently upwelled water, during the June 2017 California Current Ecosystem – Long Term Ecological Research process study. The Lagrangian CFEs operating at depths from 100–500 m yielded carbon flux and its partitioning with size from 30 µm–1 cm at three intensive study locations within the filament and in waters outside the filament. Size analysis codes intended to enable long-term CFE operations independent of ships are described. Different particle classes (anchovy pellets, copepod pellets, and > 1000 µm aggregates) dominated the 100–150 m fluxes during successive stages of the filament evolution as it progressed offshore. Fluxes were very high at all locations in the filament; below 150 m, flux was invariant or increased with depth at the two locations closer to the coast. Martin curve b factors (± denotes 95 % confidence intervals) for total particulate carbon flux were +0.37 ± 0.59, +0.85 ± 0.31, −0.24 ± 0.68, and −0.45 ± 0.70 at the three successively occupied locations within the plume, and in transitional waters. Interestingly, the flux profiles for all particles  90 %) of the particle flux was carried by > 1000 µm sized aggregates which increased with depth. Mechanisms to explain the factor of 3 flux increase between 150 and 500 m at the mid-plume location are investigated.