This algorithm returns the concentration of particulate organic carbon (POC) in mg m-3, calculated using an empirical relationship derived from in situ measurements of POC and blue-to-green band ratios of remote sensing reflectances (Rrs).
Support for this algorithm is contingent on the availability of bands centered at 443 in the blue region and between 547 and 565 nm in the green region. This implies support for CZCS, OCTS, MODIS-Aqua and Terra, MERIS, SeaWiFS, VIIRS. For PACE OCI, an updated POC algorithm is used, and it is described here.
Algorithm Point of Contact: Dariusz Stramski, Scripps Institute of Oceanography, and Bryan Franz, NASA Goddard Space Flight Center.
The algorithm is a power law applied to a blue-to-green band ratio.
The algorithm is a power-law relationship between a ratio of $R_{rs}$ and POC:
$poc = a\times \left(\frac{Rrs(443)}{Rrs(555)}\right)^b$
where
In cases where Rrs(555) is not available an equivalence is estimated from the closest native green wavelength using the empirical relationships described in convert_band.c . The input wavelengths used for the various sensors are shown in the table below.
SeaWiFS | 443, 555 |
MODIS | 443, 547 |
MERIS | 443, 560 |
VIIRS | 443, 551 |
Product Short Name | poc |
Level-2 Product Suite | OC |
Level-3 Product Suite | POC |
Level-3 Masking | ATMFAIL,LAND,HISATZEN,STRAYLIGHT,CLDICE,LOWLW, NAVWARN,ATMWARN, HISOLZEN,NAVFAIL,FILTER,HIGLINT |
For further details on the implementation in the NASA ocean color processing code, see the algorithm source code and the dependency graph.
Satellite-to-in-situ validation results are available from the SeaWiFS Bio-Optical Archive and Storage System (SeaBASS) for the following missions:
Stramski, D., Reynolds, R. A., Babin, M., Kaczmarek, S., Lewis, M. R., Röttgers, R., … Claustre, H. (2008). Relationships between the surface concentration of particulate organic carbon and optical properties in the eastern South Pacific and eastern Atlantic Oceans. Biogeosciences, 5(1), 171-201. doi:10.5194/bg-5-171-2008