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Flow and sediment circulation patterns in different seasons were inferred using current velocity, salinity and suspended sediment concentration (SSC) time series collected in the hydrographic surveys in conjunction with fathometer profiles in bathymetry surveys.
It is hypothesized that sediment circulation in the estuary can be separated into two different systems: the "tidal zone" is under the influence of marine sediment from the Pearl River estuary, whereas the "fluvial zone" is mainly affected by terrestrial sediment from the river.
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Analysis of patterns of coastal circulation and sediment dispersal is an essential step for the study of controlling factors influencing the long-term dynamics of coastal systems.
In order to explain the significant differences in evacuated sediment ratio, the induced circulation is analyzed by measuring the flow field on two vertical planes using the ultrasonic Doppler method.
At the same time, the inclusion of physical parameters from the environment, such as temperature, salinity, circulation, waves, sediment properties, can be added in order to define the boundary conditions for surveyed organisms and processes.
If conditions clear tomorrow, we hope to core the ocean bed to obtain sediments for reconstructing ocean circulation changes in the past".
Of particular interest has been the effort to learn more about such processes in the Mediterranean as air-sea interactions, sediment deposition, deepwater formation, and circulation (notably as it is affected by increased salinity); there has been general agreement that greater knowledge of these processes increases the understanding of global climatic change.
This convective cell structure indicates ancient and recent fluid circulation across the sediment-basement interface.
By connecting lands, lakes and the sea, they enable the circulation of nutrients, sediments and living beings.
Following their deaths at the hands of phages, those carbon-containing microorganisms sink down into the marine sediment, effectively removing greenhouse gases from circulation.
In general, gravitational circulation, tidal trapping, and sediment resuspension and deposition processes are the primary TM formation mechanisms in the PRE.
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