|Title||Robotic observations of high wintertime carbon export in California coastal waters|
|Publication Type||Journal Article|
|Year of Publication||2016|
|Authors||Bishop J.KB, Fong M.B, Wood T.J|
|Type of Article||Article|
|Keywords||basin; deep-ocean; Marine snow; neutrally buoyant; northeast pacific; particle fluxes; particulate matter; sediment traps; southern-ocean; twilight zone|
Biologically mediated particulate organic and inorganic carbon (POC and PIC) export from surface waters is the principal determinant of the vertical oceanic distribution of pH and dissolved inorganic carbon and thus sets the conditions for air-sea exchange of CO2; exported organic matter also provides the energy fueling communities in the mesopelagic zone. However, observations are temporally and spatially sparse. Here we report the first hourly-resolved optically quantified POC and PIC sedimentation rate time series from an autonomous Lagrangian Carbon Flux Explorer (CFE), which monitored particle flux using an imaging optical sedimentation recorder (OSR) at depths below 140aEuro-m in the Santa Cruz Basin, CA, in May 2012, and in January and March 2013. Highest POC vertical flux (similar to aEuro parts per thousand aEuro-100-240aEuro-mmolaEuro-CaEuro-m(-2)aEuro-d(-1)) occurred in January, when most settling material was millimeter- to centimeter-sized aggregates but when surface biomass was low; fluxes were similar to aEuro parts per thousand aEuro-18 and similar to aEuro parts per thousand aEuro-6aEuro-mmolaEuro-CaEuro-m(-2)aEuro-d(-1), respectively, in March and May, under high surface biomass conditions. An unexpected discovery was that January 2013 fluxes measured by CFE were 20 times higher than that measured by simultaneously deployed surface-tethered OSR; multiple lines of evidence indicate strong undersampling of aggregates larger than 1aEuro-mm in the latter case. Furthermore, the January 2013 CFE fluxes were about 10 times higher than observed during multiyear sediment trap observations in the nearby Santa Barbara and San Pedro basins. The strength of carbon export in biologically dynamic California coastal waters is likely underestimated by at least a factor of 3 and at times by a factor of 20.