VIIRS Diffuse Attenuation Coefficient at 490 nm
Diffuse attenuation coefficient at 490 nm (Kd490) is a measure of water
turbidity or clarity, i.e. the amount of light reduction (attenuation) in
the water due to scattering by particles or due to light absorption by the
water itself. Higher Kd490 values mean more attenuation due to more turbid
water, and lower Kd490 values mean less attenuation due to more clear water.
NOAA CoastWatch produces ocean color products, including Kd490,
from the Visible Infrared Imaging Radiometer
Suite (VIIRS) on-board the polar-orbiting Suomi-NPP and NOAA-20 satellites
(Wang et al., 2017).
Atmospheric correction uses the near-infrared (NIR) approach of
Jiang and Wang (2014), which is an iterative NIR approach combining the
NIR approachs of Bailey et al. (2010), MUMM (or Ruddick et al.
(2000)), and Wang et al. (2012), referred to as the BMW atmospheric
correction (see Jiang and Wang, 2014, for detailed references).
While short-wave infrared (SWIR) approaches, like that used for NOAA's
MODIS ocean color products, generate more accurate results for coastal
waters than NIR approaches, the improved BMW approach of Jiang and Wang
(2014) was found to offer the most accurate results compared to other
Diffuse attenuation coefficient is generated using the Wang et al. (2009)
algorithm, in which separate algorithms for clear open ocean and turbid coastal
waters are weighted into a combined product. This approach improves accuracy
across ocean conditions.
This algorithm was developed for the MODIS-Aqua instrument using in-situ
data from the NASA SeaBASS database.
Validation for Kd490 has only occurred for MODIS-Aqua to date. MODIS-Aqua
Kd490 data were compared with in-situ Kd490 from
the NASA SeaBASS database, representing open ocean and some turbid coastal
measurements. MODIS Kd490 data reasonably agreed with
the in-situ measurements, with a mean ratio of 1.037 (Wang et al., 2009).
To evaluate VIIRS Kd490 performance, images of seasonal averages from 2012-2013
were visually compared between MODIS and VIIRS and found to be similar
(Wang et al., 2017).
There is no quantitative validation of the VIIRS Kd490 data product.
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files by time-interval and region (via http).
Wang, M., Liu, X., Jiang, L., and Son, S.H. 2017.
VIIRS Ocean Color Algorithm Theoretical Basis Document (ATBD),
Version 1, NOAA NESDIS Center for Satellite Applications and Research.
Jiang, L. and Wang, M. 2014. Improved near-infrared ocean reflectance
correction algorithm for satellite ocean color data processing,
Optics Express, 22, 21657–21678.
Wang, M., Son, S.H., and Harding, L.W. 2009. Retrieval of diffuse attenuation
coefficient in the Chesapeake Bay and turbid ocean regions for satellite
ocean color applications, Journal of Geophysical Research, vol. 114, C10011.