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Dataset: Global reconstructions of particle biovolume, size distribution, and carbon export flux from the seasonal euphotic zone and maximum winter time mixed layer from particle profiles conducted during cruises from 2008 to 2020
Final no updates expectedDOI: 10.26008/1912/bco-dmo.856942.2Version 2 (2023-02-02)Dataset Type:Other Field ResultsDataset Type:model results
Global reconstructions of particle biovolume, size distribution, and carbon export flux from the seasonal euphotic zone and maximum winter time mixed layer.
This file shows the reconstructed particles size distribution and particle flux from the base of the maximum mixed layer. All data are generated using a random forest machine learning model. Here we show the monthly climatological reconstructions of the PSD and resulting calculated flux.
File Parameters:
Name,Description,Units,Missing data identifier
latitude,cell-center Latitude,degrees north,NaN
longitude,cell-center Longitude,degrees east,NaN
time,climatological month,month,NaN
area,cell surface area,m^2,NaN
depth,Monthly export horizon,M,NaN
obs_bv,average observed particle biovolume,ppm,NaN
obs_slope,average observed particle size distribution slope,unitless,NaN
pred_bv,reconstructed particle biovolume,ppm,NaN
stdev_bbv,reconstructed particle biovolume standard deviation,ppm,NaN
pred_slope,reconstructed particle size distribution slope,unitless,NaN
stdev_slope,reconstructed particle size distribution slope,unitless,NaN
flux,reconstructed particle carbon flux from the mixed layer,mgC/m^2/dCocoaLigature1,NaN
stdev_flux,reconstructed flux standard deviation,mgC/m^2/dCocoaLigature1,NaN
This file shows the reconstructed particles size distribution and particle flux from the base of the euphotic zone. All data are generated using a random forest machine learning model. Here we show the monthly climatological reconstructions of the PSD and resulting calculated flux.
File Parameters (Name,Description,Units,Missing data identifier):
latitude,cell-center latitude,degrees north,NaN
longitude,cell-center longitude,degrees east,NaN
time,month of reconstruction,month,NaN
area,cell area,m^2,NaN
Depth,Monthly export horizon,m,NaN
obs_bv,average observed particle biovolume,ppm,NaN
obs_slope,average observed particle size distribution slope,unitless,NaN
pred_bv,reconstructed particle biovolume,ppm,NaN
stdev_bbv,reconstructed particle biovolume standard deviation,ppm,NaN
pred_slope,reconstructed particle size distribution slope,unitless,NaN
stdev_slope,reconstructed particle size distribution slope standard deviation,unitless,NaN
flux,reconstructed particle carbon flux from the euphotic zone,mgC/m^2/dCocoaLigature1,NaN
stdev_flux,reconstructed particle carbon flux,mgC/m^2/d,NaN
A list of cruises during which the particle profiles were conducted. More information about these cruises can be found at EcoTaxa (http://ecotaxa.obs-vlfr.fr).
Parameters (data column name, and description):
"Cruise", Cruise identifier in EcoPart (EcoTaxa)
"Year_of_cruise_start",Year of cruise start in format yyyy
"Number_of_profiles", Number of profiles from the cruise
This work is based on the compilation of over 6800 profiles of particulate matter observations from Underwater Vision Profilers (UVP5) (Rainer, 2021). The biovolume of the particle size distribution is calculated as the equivalent spherical volume of the particle size distribution (PSD), by summing the product of particle counts time particle volume in each size class. The slope of the PSD is calculated assuming a power law distribution for the particle abundance, by linear least square fit of the log of particle counts vs. the log of particle size. These quantities are estimated from two different depth horizons, the mixed layer depth (MLD_Export.nc) and the euphotic zone depth (Euphotic_Export.nc). To convert sparse observations to a global climatology, we trained 100 ensembles of regressions trees (Random Forests, RF) to predict biovolume and slope based on their relationship to well-sampled physical and biogeochemical predictors.
We calculate the particle sinking speed and carbon content by combining PSD reconstruction (biovolume and slope) with an empirical relationship between particle size, carbon content and sinking speed, the parameters of which are optimized to match in situ particle flux observations (Bisson et al. 2018). The flux values are calculated as the sum of the PSD time the sinking carbon parameters, for each grid cell. The error for reconstructed quantities is given by the standard deviation of 100 independent realizations of the RF reconstructions.
Sampling and analytical procedures:
This dataset contains a compilation of data from multiple sources. A list of all datasets and the associated information, including cruise name, is included.
Observations of Particle size and biovolume are made via the UVP5 camera, which is lowered in the water column on a CTD rosette. Images are captured at up to 30 images per second while the instrument is lowered at 1m/s. Images are analyzed and the pixel size of each particle is translated into a particle size, and the abundance calculated, following the method described by Picheral et al. (2010).
The data is compiled from multiple sources published and unpublished, and was accessed from EcoPart, the particle module of EcoTaxa https://ecotaxa.obs-vlfr.fr/part/ (Picheral et al., 2017).
Instruments:
Observations of particle abundance and biovolume were made with the Underwater Vision Profiler, version 5 (UVP5).
Clements, D., Bianchi, D. (2024) Global reconstructions of particle biovolume, size distribution, and carbon export flux validated for the upper 2000m of the water column from particle profiles conducted during cruises from 2008 to 2020. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-10-03 http://lod.bco-dmo.org/id/dataset/939274
Related Publications
Results
Clements, D. J., Yang, S., Weber, T., Mcdonnell, A., Kiko, R., Stemmann, L., & Bianchi, D. (2021). Constraining the ocean’s biological pump with in situ 1 optical observations and supervised learning. Part 2: 2 Carbon Flux. https://doi.org/10.1002/essoar.10509084.1
IsDerivedFrom
Kiko, Rainer (2021): The global marine particle size distribution dataset obtained with the Underwater Vision Profiler 5 - version 1. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.924375
IsDerivedFrom
Picheral M, Colin S, Irisson J-O (2017). EcoTaxa, a tool for the taxonomic classification of images. http://ecotaxa.obs-vlfr.fr
Methods
Bisson, K. M., Siegel, D. A., DeVries, T., Cael, B. B., & Buesseler, K. O. (2018). How Data Set Characteristics Influence Ocean Carbon Export Models. Global Biogeochemical Cycles, 32(9), 1312–1328. doi:10.1029/2018gb005934
Methods
Picheral, M., Guidi, L., Stemmann, L., Karl, D. M., Iddaoud, G., & Gorsky, G. (2010). The Underwater Vision Profiler 5: An advanced instrument for high spatial resolution studies of particle size spectra and zooplankton. Limnology and Oceanography: Methods, 8(9), 462–473. doi:10.4319/lom.2010.8.462
Bianchi, D., Clements, D. (2023) Global reconstructions of particle biovolume, size distribution, and carbon export flux from the seasonal euphotic zone and maximum winter time mixed layer from particle profiles conducted during cruises from 2008 to 2020. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 2) Version Date 2023-02-02 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.856942.2 [access date]
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.