Dataset: Surface and mixed-layer averaged diel cycles of O2 and optically-based POC from repeated CTD casts in the North Pacific from 2017-09-05 to 2017-09-25

This dataset has not been validatedData not availableVersion 0 (2020-04-09)Dataset Type:Cruise Results

Principal Investigator: Angelicque E. White (Oregon State University)

Co-Principal Investigator: Paul Quay (University of Washington)

BCO-DMO Data Manager: Mathew Biddle (Woods Hole Oceanographic Institution)


Project: Collaborative Research: Measuring Ocean Productivity from the Diurnal Change in Oxygen and Carbon (ProdChangeO2Carb)


Abstract

Time series of Winkler-calibrated mixed-layer averaged dissolved oxygen (Aandera optode) obtained via repeated CTD casts. Mixed-layer averaged particulate beam-attenuation coefficients (cp) calibrated to particulate organic carbon (POC) concentrations derived from repeated CTD casts. The cruise (KM1713) transited from Seward, AK to Honolulu, HI from 3-26 September 2017 onboard the R/V Kilo Moana. Six extended stations (Stn), three in subpolar waters (Stn 1 at 55°N, Stn 2 at 50°N, and Stn 3 at 46...

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The cruise (KM1713) transited from Seward, AK to Honolulu, HI from 3-26 September 2017 onboard the R/V Kilo Moana. Six extended stations (Stn), three in subpolar waters (Stn 1 at 55°N, Stn 2 at 50°N, and Stn 3 at 46°N), one in the transition zone between subpolar and subtropical waters (Stn 4 at 42°N), and two in the subtropical gyre (Stn 5 at 34°N, and Stn 6 at 24°N) were occupied for 2-3 day periods during which continuous measurements of conductivity, temperature, O2, O2/Ar and beam attenuation were measured continuously on surface seawater supplied via the ships’ intake line and using CTD profiles of conductivity, temperature, pressure, oxygen, and the particulate beam attenuation coefficient conducted at ~2-hr intervals. An autonomous profiling float was deployed for ~ 2 days at four stations, retrieving CTD and oxygen profiles at approximately 3-hour intervals. Another float with same mission design was deployed near station ALOHA (22.45° N, 158° W) during July 2017 to provide mixed-layer averaged O2 near station 6. When available, the ship followed the trajectory of the profiling float, yielding a near-Lagrangian sampling strategy with the aim to minimize horizontal mixing effects.


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Methods

Kara, A. B., Rochford, P. A., & Hurlburt, H. E. (2000). An optimal definition for ocean mixed layer depth. Journal of Geophysical Research: Oceans, 105(C7), 16803–16821. doi:10.1029/2000jc900072