Underwater light field patterns in subtropical coastal waters: A case study from the Gulf of Eilat (Aqaba)

2012 ◽  
Vol 60 (1) ◽  
pp. 265-275 ◽  
Author(s):  
Gal Dishon ◽  
Zvy Dubinsky ◽  
Maoz Fine ◽  
David Iluz
2020 ◽  
Author(s):  
Kristi Uudeberg ◽  
Mirjam Randla ◽  
Age Arikas ◽  
Tuuli Soomets ◽  
Kaire Toming ◽  
...  

<p>Climate change is expected to continue in the 21st century, but the magnitude of change depends on future actions. In the Baltic Sea, specifically in the Pärnu Bay region, this is predicted to mean warmer temperatures, less ice cover, more precipitations and a slight increase in average wind speed, furthermore extreme climatic events such as heavy rains, strong winds and storms will be more intense and frequent. The coastal waters play a central role in humans and nature's everyday lives as providing food, living and recreational opportunities. Since Pärnu Bay is one of the most eutrophied area in the Baltic Sea and provides living hood more the 800 fishermen, then regular monitoring is strongly recommended, but with traditional methods often unfeasible. The availability of free Sentinel satellites data with good spectral, spatial and temporal resolution has generated wide interest in how to use remote sensing capabilities to monitor coastal waters water quality, which affects the underwater light field and can lead even to changes in fish composition. However, these waters are optically complex and influenced independently by coloured dissolved organic matter, phytoplankton and an amount of suspended sediments. Therefore, the remote sensing of optically complex waters is more challenging, and standard remote sensing products often fail. In this study, we use satellite Sentinel-3 data to investigate weather phenomena as strong wind and precipitations effect to Pärnu Bay water quality parameters. We study the spatial and temporal scope of change of water quality parameters after the event. For that, we use optical water type classification based chlorophyll-a, suspended sediments and coloured dissolved organic matter algorithms on Sentinel-3 images and estimate underwater light field changes. Furthermore, we also use in situ data to analyses the frequency and the strength of weather events. Finally, we look at the composition of fish based on literature and we investigate the possible effects of the change of the underwater light field on fish composition.</p>


2020 ◽  
Vol 103 (sp1) ◽  
pp. 453
Author(s):  
Ping Yang ◽  
Zizhao Wu ◽  
Yao Chen ◽  
Yilu Guo ◽  
Peng Zhang ◽  
...  

1985 ◽  
Vol 11 (2) ◽  
pp. 78-81 ◽  
Author(s):  
R. D. Robarts ◽  
T. Zohary ◽  
F. Ojeda ◽  
C. C.E. Lovengreen ◽  
R. D. Walmsley

1981 ◽  
Vol 32 (4) ◽  
pp. 517 ◽  
Author(s):  
JTO Kirk

A Monte Carlo calculation procedure has been developed for computer modelling of the penetration of light into turbid, coloured waters of the type commonly found on the Australian continent. For monochromatic light the structure of the underwater light field is described in terms of the variation of the average cosine (total, downward, upward) and irradiance reflectance, as a function of optical depth at a given ratio of scattering to absorption (bla), and as a function of bia at a given optical depth. The vertical attenuation coefficient for downward irradiance at the mid-point of the euphotic zone [Kd(za)] has been studied as a function of the absorption (a) and scattering (b) coefficients and, with the particular normalized volume scattering function used in these simulations. has been found to conform closely to the equation Kd(zm) = (a2 + 0.256ab)½ The data generated by the model have been used in conjunction with radiative transfer theory to determine the contribution of the different components of the attenuation mechanism to the vertical diminution of irradiance at different ratios of b to a. Simulation of the penetration of photosynthetically available radiation into four water bodies in the southern tablelands of New South Wales has been carried out using measured absorption coefficients and indirectly estimated values for scattering coefficients. The calculated values for vertical attenuation coefficients are in good agreement with those obtained by measurement within the water bodies. The possible use of this modelling procedure as a predictive tool is discussed.


Sign in / Sign up

Export Citation Format

Share Document