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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 26, issue 7
Ann. Geophys., 26, 2019–2035, 2008
https://doi.org/10.5194/angeo-26-2019-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 26, 2019–2035, 2008
https://doi.org/10.5194/angeo-26-2019-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  28 Jul 2008

28 Jul 2008

Satellite remote sensing of a low-salinity water plume in the East China Sea

Y. H. Ahn, P. Shanmugam, J. E. Moon, and J. H. Ryu Y. H. Ahn et al.
  • Ocean Satellite Research Group, Korea Ocean Research and Development Institute, Ansan, P.O. Box 29, Seoul 425-600, Korea

Abstract. With the aim to map and monitor a low-salinity water (LSW) plume in the East China Sea (ECS), we developed more robust and proper regional algorithms from large in-situ measurements of apparent and inherent optical properties (i.e. remote sensing reflectance, Rrs, and absorption coefficient of coloured dissolved organic matter, aCDOM) determined in ECS and neighboring waters. Using the above data sets, we derived the following relationships between visible Rrs and absorption by CDOM, i.e. Rrs (412)/Rrs (555) vs. aCDOM (400) (m−1) and aCDOM (412) (m−1) with a correlation coefficient R2 0.67 greater than those noted for Rrs (443)/Rrs (555) and Rrs (490)/Rrs (555) vs. aCDOM (400) (m−1) and aCDOM (412) (m−1). Determination of aCDOM (m−1) at 400 nm and 412 nm is particularly necessary to describe its absorption as a function of wavelength λ using a single exponential model in which the spectral slope S as a proxy for CDOM composition is estimated by the ratio of aCDOM at 412 nm and 400 nm and the reference is explained simply by aCDOM at 412 nm. In order to derive salinity from the absorption coefficient of CDOM, in-situ measurements of salinity made in a wide range of water types from dense oceanic to light estuarine/coastal systems were used along with in-situ measurements of aCDOM at 400 nm, 412 nm, 443 nm and 490 nm. The CDOM absorption at 400 nm was better inversely correlated (R2=0.86) with salinity than at 412 nm, 443 nm and 490 nm (R2=0.85–0.66), and this correlation corresponded best with an exponential (R2=0.98) rather than a linear function of salinity measured in a variety of water types from this and other regions. Validation against a discrete in-situ data set showed that empirical algorithms derived from the above relationships could be successfully applied to satellite data over the range of water types for which they have been developed. Thus, we applied these algorithms to a series of SeaWiFS images for the derivation of CDOM and salinity in the context of operational mapping and monitoring of the springtime evolution of LSW plume in the ECS. The results were very encouraging and showed interesting features in surface CDOM and salinity fields in the vicinity of the Yangtze River estuary and its offshore domains, when a regional atmospheric correction (SSMM) was employed instead of the standard (global) SeaWiFS algorithm (SAC) which revealed large errors around the edges of clouds/aerosols while masking out the nearshore areas. Nevertheless, there was good consistency between these two atmospheric correction algorithms over the relatively clear regions with a mean difference of 0.009 in aCDOM (400) (m−1) and 0.096 in salinity (psu). This study suggests the possible utilization of satellite remote sensing to assess CDOM and salinity and thus provides great potential in advancing our knowledge of the shelf-slope evolution and migration of the LSW plume properties in the ECS.

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