Carbon export and fate beneath a dynamic upwelled filament off the California coast
نویسندگان
چکیده
Abstract. To understand the vertical variations in carbon fluxes biologically productive waters, four autonomous flux explorers (CFEs), ship-lowered CTD-interfaced particle-sensitive transmissometer and scattering sensors, surface-drogued sediment traps were deployed a filament of offshore flowing, recently upwelled water, during June 2017 California Current Ecosystem – Long Term Ecological Research process study. The Lagrangian CFEs operating at depths from 100–500 m yielded its partitioning with size 30 µm–1 cm three intensive study locations within waters outside filament. Size analysis codes intended to enable long-term CFE operations independent ships are described. Different particle classes (anchovy pellets, copepod > 1000 µm aggregates) dominated 100–150 successive stages evolution as it progressed offshore. Fluxes very high all filament; below 150 m, was invariant or increased depth two closer coast. Martin curve b factors (± denotes 95 % confidence intervals) for total particulate +0.37 ± 0.59, +0.85 0.31, ?0.24 0.68, ?0.45 0.70 successively occupied plume, transitional waters. Interestingly, profiles particles < 400 much fit canonical profile (b?0.86); however, most (typically 90 %) carried by sized aggregates which depth. Mechanisms explain factor 3 increase between 500 mid-plume location investigated.
منابع مشابه
Range-only Benthic Rover Localization off the Central California Coast
. Nowadays, the use of autonomous vehicles for ocean research has increased, since these vehicles have a better cost/performance ratio than crewed vessels or oceanographic ships. For example, autonomous surface vehicles can be used to localize underwater targets. This paper describes a mission to find a crawling robot Benthic Rover on the abyssal plain in the north eastern Pacific, using single...
متن کاملDevelopment, implementation and evaluation of a data-assimilative ocean forecasting system off the central California coast
The development and implementation of a real-time ocean forecast system based on the Regional Ocean Modeling System (ROMS) off the coast of central California are described. The ROMS configuration consists of three nested modeling domains with increasing spatial resolutions: the US West coastal ocean at 15-km resolution, the central California coastal ocean at 5 km, and the Monterey Bay region ...
متن کاملA forcing mechanism for the poleward flow off the southern California coast
It is shown that when the wind distribution along a coast is anisotropic, such that its cross-shore scale is smaller than its alongshore scale, the coastal sea level (or the upper layer anamoly) “A” of an ocean forced by both wind and wind curl is governed by a modified (nondimensionalized) Kelvin wave equation: A/t* 1 A/ y* 5 k0(0, y*, t*) 1 * k1/ y* dtL where k0 and k1 are wind stress a...
متن کاملAircraft Observations of a Coastally Trapped Wind Reversal off the California Coast
During summertime months the low-level airflow over the eastern Pacific is dominated by the circulation associated with the Pacific High typically situated about 1000 km off the west coast of the United States. Subsidence above the Pacific High establishes a sharp temperature inversion at the top of the well-mixed marine boundary layer (MBL) with its depth increasing offshore to the west. A low...
متن کاملObservations of continental biogenic impacts on marine aerosol and clouds off the coast of California
During the 2011 Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) and 2013 Nucleation in California Experiment (NiCE) field campaigns, a predominantly organic aerosol (> 85% by mass) was observed in the free troposphere over marine stratocumulus off the coast of California. These particles originated from a densely forested region in the Northwestern United States. The organic mass spe...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Biogeosciences
سال: 2021
ISSN: ['1726-4189', '1726-4170']
DOI: https://doi.org/10.5194/bg-18-3053-2021