Satellite Detection of Pre-Earthquake Thermal Anomaly and Sea Water Turbidity Associated with the Great Sumatra Earthquake

2006 ◽  
pp. 249-260
Finisterra ◽  
2012 ◽  
Vol 30 (59/60) ◽  
Author(s):  
Eugénia Albergaria Moreira

SEA-SIDE LIMIT OF SADO ESTUARY IN LANDSAT IMAGERIES - The outside limit of Sado estuary corresponds to the submarine delta front, with an arcuate and digitate contour. It was individualised on the MSS Landsat data imageries. Multispectral data classification allowed to verify that the turbidity-plum of Sado estuary mouth rather corresponds to the low-sea-water surface associated to the brightness of the bottom sediments, that to the water turbidity content.


1984 ◽  
Vol 17 (8) ◽  
pp. 1749-1758 ◽  
Author(s):  
D M Philips ◽  
R H Abbot ◽  
M F Penny

1984 ◽  
Vol 37 (1) ◽  
pp. 75 ◽  
Author(s):  
DM Phillips ◽  
BW Koerber

An airborne laser technique for remote measurement of sea water turbidity is studied theoretically. The limits of validity of an analytic model are established using Monte Carlo simulation computations. It is shown that, if the field of view of the airborne receiver is large enough, the backscatter signal from the water is attenuated at a rate determined by the absorption coefficient of the water. Apart from geometrical factors, the amplitude of the backscatter signal at the water surface depends on the scattering coefficient of the water. The method therefore allows both the absorption and scattering coefficients of water to be determined independently.


2017 ◽  
Vol 77 (1) ◽  
pp. 269-277 ◽  
Author(s):  
José Otavio Goulart Pecly

Abstract The alternative use of effluent turbidity to determine the dilution field of a domestic marine outfall located off the city of Rio de Janeiro was evaluated through field work comprising fluorescent dye tracer injection and tracking with simultaneous monitoring of sea water turbidity. A preliminary laboratory assessment was carried out with a sample of the outfall effluent whose turbidity was measured by the nephelometric method before and during a serial dilution process. During the field campaign, the dye tracer was monitored with field fluorometers and the turbidity was observed with an optical backscattering sensor interfaced to an OEM data acquisition system. About 4,000 samples were gathered, covering an area of 3 km × 3 km near the outfall diffusers. At the far field – where a drift towards the coastline was observed – the effluent plume was adequately labeled by the dye tracer. The turbidity plume was biased due to the high and variable background turbidity of sea water. After processing the turbidity dataset with a baseline detrending method, the plume presented high correlation with the dye tracer plume drawn on the near dilution field. However, dye tracer remains more robust than effluent turbidity.


1919 ◽  
Vol 87 (2257supp) ◽  
pp. 211-211
Author(s):  
Paul T. Bruhl
Keyword(s):  

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