Float profile data collected during surface ascents in the Sargasso Sea from 2013-2014 (NCEI Accession 0278798)
This dataset contains biological, chemical, optical, and physical data collected at R/V Atlantic Explorer and shoreside SargassoSea during cruises AE1315, AE1318, AE1320, AE1323, and AE1402 and deployments F033 and F034 in the North Atlantic Ocean from 2013-07-06 to 2014-11-24. These data include Oxygen in volts, beam attenuation, chlorophyll a, colored dissolved organic matter, dissolved Oxygen, particulate organic Carbon (POC), salinity calculated from CTD primary sensors, and water pressure. The instruments used to collect these data include CTD Sea-Bird, Dissolved Oxygen Sensor, Fluorometer, Optical Backscatter Sensor, and Transmissometer. These data were collected by Dr Margaret L. Estapa of Skidmore College and Dr Kenneth O. Buesseler of Woods Hole Oceanographic Institution as part of the "Rapid, Autonomous Particle Flux Observations in the Oligotrophic Ocean (RapAutParticleFlux)" project and "Ocean Carbon and Biogeochemistry (OCB)" program. The Biological and Chemical Oceanography Data Management Office (BCO-DMO) submitted these data to NCEI on 2018-04-25.
The following is the text of the dataset description provided by BCO-DMO:
Float profile data collected during surface ascent.
Dataset Description:
Float profile data collected during surface ascent.
The following is the text of the dataset description provided by BCO-DMO:
Float profile data collected during surface ascent.
Dataset Description:
Float profile data collected during surface ascent.
Dataset Citation
- Cite as: Estapa, Margaret L.; Buesseler, Kenneth O. (2023). Float profile data collected during surface ascents in the Sargasso Sea from 2013-2014 (NCEI Accession 0278798). [indicate subset used]. NOAA National Centers for Environmental Information. Dataset. https://www.ncei.noaa.gov/archive/accession/0278798. Accessed [date].
Dataset Identifiers
ISO 19115-2 Metadata
gov.noaa.nodc:0278798
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Ordering Instructions | Contact NCEI for other distribution options and instructions. |
Distributor |
NOAA National Centers for Environmental Information +1-301-713-3277 NCEI.Info@noaa.gov |
Dataset Point of Contact |
NOAA National Centers for Environmental Information ncei.info@noaa.gov |
Time Period | 2013-07-06 to 2014-11-24 |
Spatial Bounding Box Coordinates |
West: -69.025
East: -61.376
South: 28.409
North: 34.573
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Spatial Coverage Map |
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Data Presentation Form | Digital table - digital representation of facts or figures systematically displayed, especially in columns |
Dataset Progress Status | Complete - production of the data has been completed Historical archive - data has been stored in an offline storage facility |
Data Update Frequency | As needed |
Supplemental Information | Acquisition Description: Multiple deployments of two Sea-Bird Scientific Navis BGCi floats (numbers F033 and F034) equipped with CTDs, transmissometers, O 2 optodes, backscattering (700 nm), fluorescence (chlorophyll, colored dissolved organic matter), and tilt sensors were conducted between July 2013 and November 2014 in conjunction with Bermuda Atlantic Time-series Study cruises. Short-term deployments (1.5 – 3 days) followed by recovery of the floats were conducted during four monthly BATS cruises in July – October 2013 and one cruise in March 2014. Both floats were deployed during the July and August 2013 cruises and float F034 was deployed for the remaining cruises. Each float collected one profile per cruise with the exception of the August 2013 cruise, during which the two floats together collected 13 profiles. During short-term deployments, floats first completed an initial descent and ascent without parking, then completed 1 or 2 more profile cycles with different, consecutive target depths. Following the initial descent/ascent described above, the short-term profile cycles were structured as described below for long-term deployments. In addition to the short-term cruise deployments, F033 profiled continuously from October 2013 until early April 2014, yielding 77 profiles, and F034 profiled continuously from March 2014 until late November 2014, yielding 139 profiles. During these long-term deployments, a typical cycle consisted of 1) the descent to the target park depth, 2) a park phase at the target depth lasting 1.5 – 2.5 days during which measurements are made every 15 minutes, 3) a descent to 1000 dbar, 4) an ascent to the surface during which measurements are made, and 5) a surface telemetry phase, during which a GPS fix is obtained, data are uploaded via Iridium, and instructions for the next cycle are downloaded. During long-term deployments, floats cycled through park phases at 150/200, 300, 500, and 1000 dbar every 7 days, spending 2.5 days at 1000 dbar and 1.5 days at the shallower depths. The sequence of park phase depth at the three shallowest depths was varied between each 7-day cycle over a 21-day period to avoid aliasing in particle flux profiles. A float firmware error early in the project prevented collection of upper water column data in some of the short-term deployments. This was remedied before long-term deployment of the floats commenced. The floats occasionally performed a reboot during ascent profiles. The affected profiles are missing data for some pressure bins. Colored dissolved organic matter data are not available for float F034 profiles from cruises B295 and B296 due to sensor malfunction. Profile data were acquired during the ascent to the surface following each park phase acquisition at a sampling rate of 4 dbar below 500 dbar and 2 dbar above 500 dbar. Related References: References Benson, B.B., Krause, D., Jr., 1984. The concentration and isotopic fractionation of oxygen dissolved in freshwater and seawater in equilibrium with the atmosphere. Limnol. Oceanogr. 29, 620-632. http://dx.doi.org/10.4319/lo.1984.29.3.0620. Bittig, H.C., Fielder, B., Fietzk, P., Kortzinger, A., 2015. Pressure response of Aanderaa and Sea-Bird oxygen optodes. J. Atmos. Oceanic Tech. 32, 2305-2317. http://dx.doi.org/10.1175/JTECH-D-15-0108.1. Boss, E., Pegau, W.S., 2001. Relationship of light scattering at an angle in the backward direction to the backscattering coefficient. Appl. Opt. 40, 5503-5507. http://doi.org/10.1364/AO.40.005503. Briggs, N., Perry, M.J., Cetinić, I., Lee, C., D'Asaro, E., Gray, A.M., Rehm, E., 2011. High-resolution observations of aggregate flux during a sub-polar North Atlantic spring bloom. Deep-Sea Res. I 58, 1031-1039. http://dx.doi.org/10.1016/j.dsr.2011.07.007. Estapa, M.L., Buesseler, K., Boss, E., Gerbi, G., 2013. Autonomous, high-resolution observations of particle flux in the oligotrophic ocean. Biogeosciences 10, 5517–5531. http://dx.doi.org/10.5194/bg-10-5517-2013. Garcia, H.E., Gordon, L.I., 1992. Oxygen solubility in seawater: Better fitting equations. Limnol. Oceanogr. 37, 1307-1312. http://dx.doi.org/10.4319/lo.1992.37.6.1307. Morgan, P.P., Pender, L., 1993. SEAWATER. MATLAB Central File Exchange. Retrieved August 8, 2017. https://www.mathworks.com/matlabcentral/fileexchange/47595-mixing--mx--oceanographic-toolbox-for-em-apex-float-data. Thierry, V., Bittig, H., Gilbert, D., Kobayashi, T., Sato, K., Schmid, C., 2016. Processing Argo OXYGEN data at the DAC level. v2.2. http://dx.doi.org/10.13155/39795. Weiss, R.F., Price, B.A., 1980. Nitrous oxide solubility in water and seawater. Mar. Chem. 8, 347-359. http://dx.doi.org/10.1016/0304-4203(80)90024-9. Xing, X., Claustre, H., Boss, E., Roesler, C., Organelli, E., Poteau, A., Barbieux, M., D’Ortenzio, F., 2017. Correction of profiles of in-situ chlorophyll fluorometry for the contribution of fluorescence originating from non-algal matter: FDOM-based correction of Chla fluorescence. Limnol. Oceanogr.: Methods 15, 80–93. http://dx.doi.org/10.1002/lom3.10144. |
Purpose | This dataset is available to the public for a wide variety of uses including scientific research and analysis. |
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Last Modified: 2024-05-31T15:15:28Z
For questions about the information on this page, please email: ncei.info@noaa.gov
For questions about the information on this page, please email: ncei.info@noaa.gov