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            <gco:CharacterString>Cite this dataset as: Huang, H., Bochdansky, A. B., Couret, M., Hernández-León, S. (2026) Vertical profiles of low and high-optical-density particles (LODP and HODP) and CTD hydrographic data from Focused Shadowgraph Imaging (FoSI) in the NE Atlantic, Jan-Mar 2023 (DESAFÍO). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-08-04 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.1003447.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Dataset Description: &amp;lt;p&amp;gt;See the &amp;quot;Related Datasets&amp;quot; section for other datasets from the same profiles.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Acronyms:&amp;amp;nbsp;&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
DESAFÍO = DisEntangling Seasonality of Active Flux in the Ocean (expedition name)&amp;lt;br /&amp;gt;
FoSI = Focused Shadowgraph Imaging&amp;lt;br /&amp;gt;
LODP = Low Optical-Density Particles&amp;lt;br /&amp;gt;
HODP = High Optical-Density Particles&amp;lt;br /&amp;gt;
OD = Optical Density&amp;lt;br /&amp;gt;
ESD =&amp;amp;nbsp;equivalent spherical diameter&amp;lt;br /&amp;gt;
AZ = Azores&amp;lt;br /&amp;gt;
CI = Canary Islands&amp;lt;br /&amp;gt;
OO = Open Ocean&amp;lt;br /&amp;gt;
RGF = Relative Gel Fraction&amp;lt;br /&amp;gt;
ART ANOVA = Aligned Rank Transform (ART)&amp;amp;nbsp;Analysis of Variance (ANOVA)&amp;lt;br /&amp;gt;
ANCOVA = Analysis of Covariance&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Particle and hydrographic profile data were collected during the DESAFÍO expedition (DisEntangling Seasonality of Active Flux in the Ocean; PID2020-118118RB-100) in the Northeastern subtropical Atlantic Ocean, from 31 January to 2 March 2023, along a transect between the Azores (AZ; 41°5'32.39&amp;quot;N, 24°58'41.00&amp;quot;W) and the Canary Islands (CI; 28°41'00.00&amp;quot;N, 13°12'2.40&amp;quot;W). Twenty-two CTD casts were grouped into three geographic regions — CI (casts 1–6), the open-ocean station OO (casts 7–14, west of CI and south of the Azores), and AZ (casts 15–22) — and profiles were further partitioned into three depth strata: epipelagic (≤200 m), mesopelagic (200–1,000 m), and bathypelagic (&amp;amp;gt;1,000 m). Because the particle imaging system was mounted directly on the CTD rosette, particle and hydrographic data were collected simultaneously on the same vertical casts, allowing direct depth-matching between the two profile types. Four casts (5, 6, 18, and 20) have incomplete particle profiles due to unexpected camera shutdowns, likely from low battery voltage.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/882081.rdf" xlink:title="OCE-2128438" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2128438 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2128438</gmx:Anchor>
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&lt;p&gt;Globally, the ocean removes more carbon dioxide than it releases into the atmosphere storing a portion of the excess carbon in the deep sea. Sinking particles, both living plankton and non-living detritus, are major contributors to this flux of carbon. Modern camera systems and image analysis techniques have made it possible to count, measure and classify these particles, thus providing oceanographers with a tool to estimate carbon transfers to the deep ocean at high resolution in space and time. Unfortunately, it is not enough to know the sizes of particles to estimate how fast these particles sink because shape and particle density also influence the sinking velocity. This project examines the velocities of individual particles as they sink into the deep ocean using a camera attached to a particle trap. For each of these particles, classification criteria, such as size, shape factors, optical density, and in the case of plankton, taxonomic identification, is determined and compared to their individual sinking velocities. This information serves to calculate overall sinking velocities from surveys of particles in the water column and thereby produce more reliable estimates of carbon fluxes from camera images. This project supports technology development in underwater imaging systems, graduate and undergraduate student education, and science literacy initiatives for middle-school students and their mentors through public outreach programs.&lt;/p&gt;
&lt;p&gt;Shipboard and autonomous vehicle surveys of oceanic particle inventories hold great promise for estimating carbon fluxes at high temporal and spatial resolutions. However, while the sinking velocities of larger particles such as foraminifera shells and fecal pellets of salps, krill, and larger copepods are relatively well constrained, the dynamics of the smaller particle size pool (50–500 micrometers) remain more elusive. Despite their size and presumed slow sinking velocities, small particles occur in large numbers in the mesopelagic layer and sediment-trap material. Their abundance in the mesopelagic could be the result of deep mixing, or small particles could be remnants of digested larger particles, particles with a high excess density such as lithogenic dust particles, minipellets egested by protists, protist spores, or the result of fragmentation at depth due to the activity of flux feeders, among other possibilities. This project addresses some unanswered questions about the small particle pool by linking individually-resolved optical features with sinking velocities. Using Stokes’ law, excess density is being estimated from size and sinking velocity and then assigned to particles from optical surveys. A horizontally installed camera system records sinking velocities, sizes, and features of particles in a sediment trap attached to the Oceanic Flux Program mooring array. The recorded particles are being characterized using 1) classic image analysis, taking various shape factors into account; 2) opacity of individual particles; and 3) image classification with supervised and unsupervised deep learning using convolutional neural networks. A second identical camera surveys the particle inventory at the same station and time in the water column to integrate flux estimates over the existing and undisturbed particle pool. Niskin bottle samples and microscopic examination of particles augment the interpretation of image data. The results of this project contribute to the overarching goal of achieving higher predictive power for carbon flux models based on optical particle surveys.&lt;/p&gt;
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	Name: Depth
	Units: meters (m)
	Description: &lt;p&gt;Depth at which particles were imaged&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004165.rdf
	Name: Part_No
	Units: particles per liter (#/L)
	Description: &lt;p&gt;Particle abundance. Particle number per liter of water sample derived from FoSI image data.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004166.rdf
	Name: TotalParticleArea
	Units: pix/frame
	Description: &lt;p&gt;Particle area per image frame derived from FoSI image data&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004167.rdf
	Name: TotalParticleVolume
	Units: parts per million (ppm)
	Description: &lt;p&gt;Total particle volume concentration in part per million (ppm) derived from FoSI image data&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004168.rdf
	Name: Date
	Units: unitless
	Description: &lt;p&gt;Date when particles were imaged (ISO format).&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004169.rdf
	Name: Conductivity
	Units: Siemens per meter (S/m)
	Description: &lt;p&gt;Shows how well the water carries electricity measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004170.rdf
	Name: Density
	Units: kilograms per cubic meter (kg/m^3)
	Description: &lt;p&gt;Shows how dense the water was,  measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004171.rdf
	Name: Fluorescence
	Units: milligrams per cubic meter (mg/m^3)
	Description: &lt;p&gt;An indicator of Chlorophyll concentration measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004172.rdf
	Name: Oxygen
	Units: milliliters per liter (mL/L)
	Description: &lt;p&gt;Oxygen concentration in water measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004173.rdf
	Name: PotentialTemperature
	Units: degrees Celsius
	Description: &lt;p&gt;The temperature a water parcel would have if moved adiabatically to the surface, eliminating pressure effects measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004174.rdf
	Name: SalinityPractical
	Units: practical salinity units (PSU)
	Description: &lt;p&gt;Determined by measuring electrical conductivity, in-situ temperature, and pressure (depth) measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004175.rdf
	Name: Turbidity
	Units: nephelometric turbidity units (NTU)
	Description: &lt;p&gt;An indicator of water clarity measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004176.rdf
	Name: PAR
	Units: micromoles of photons per square meter per second (umol photons/m^2/sec)
	Description: &lt;p&gt;Photosynthetically Active Radiation measured by CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004177.rdf
	Name: Latitude
	Units: decimal degrees
	Description: &lt;p&gt;The latitude of the sampling cast. North-south position from the equator&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004179.rdf
	Name: Longitude
	Units: decimal degrees
	Description: &lt;p&gt;The longitude of the sampling cast. East-west position from the prime meridian&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/1004181.rdf
	Name: ParticlePool
	Units: unitless
	Description: &lt;p&gt;Indicate which particle pool the data belong to. LODP represent low-optical density particles, HODP represent high-optical density particles.&lt;/p&gt; 
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&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;Huang H and Bochdansky AB (2025) Optimizing an image analysis protocol for ocean particles in focused shadowgraph imaging systems. Front. Mar. Sci. 12:1539828. doi: 10.3389/fmars.2025.1539828&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;</gco:CharacterString>
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