4.7 Article

Diurnal Variability of Turbidity Fronts Observed by Geostationary Satellite Ocean Color Remote Sensing

Journal

REMOTE SENSING
Volume 8, Issue 2, Pages -

Publisher

MDPI
DOI: 10.3390/rs8020147

Keywords

GOCI; turbidity front; entropy-based algorithm; sea surface currents

Funding

  1. National High Technology and Development Program of China [2014AA123301]
  2. National Basic Research Program (973 Program) of China [2015CB954002]
  3. Public Science and Technology Research Fund Projects for Ocean Research [201505003]
  4. National Natural Science Foundation of China [41322039, 41321004, 41271378, 41406202]
  5. National Program on Global Change and Air-Sea Interaction of China [GASI-03-03-01-01, GASI-02-SCS-YGST01, GASI-02-PAC-YGST01, GASI-02-IND-YGST01]

Ask authors/readers for more resources

Monitoring front dynamics is essential for studying the ocean's physical and biogeochemical processes. However, the diurnal displacement of fronts remains unclear because of limited in situ observations. Using the hourly satellite imageries from the Geostationary Ocean Color Imager (GOCI) with a spatial resolution of 500 m, we investigated the diurnal displacement of turbidity fronts in both the northern Jiangsu shoal water (NJSW) and the southwestern Korean coastal water (SKCW) in the Yellow Sea (YS). The hourly turbidity fronts were retrieved from the GOCI-derived total suspended matter using the entropy-based algorithm. The results showed that the entropy-based algorithm could provide fine structure and clearly temporal evolution of turbidity fronts. Moreover, the diurnal displacement of turbidity fronts in NJSW can be up to 10.3 km in response to the onshore-offshore movements of tidal currents, much larger than it is in SKCW (around 4.7 km). The discrepancy between NJSW and SKCW are mainly caused by tidal current direction relative to the coastlines. Our results revealed the significant diurnal displacement of turbidity fronts, and highlighted the feasibility of using geostationary ocean color remote sensing technique to monitor the short-term frontal variability, which may contribute to understanding of the sediment dynamics and the coupling physical-biogeochemical processes.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available