Longitudinal transport of suspended sediment in the Modaomen Estuary of the Pearl River: effects of river, tide, and mouth bar: Datasets

<p><strong>This&nbsp;dataset supplements the article: Longitudinal transport&nbsp;of suspended sediment in the Modaomen </strong><strong>E</strong><strong>stuary of the Pearl River: effects of river, tide, and mouth bar, submitted to Marine Geology</strong></p> <p>Contact information: Dr. Liu, F., School of Ocean Engineering and Technology, Sun Yat-sen University, Guangzhou, 510275, China.</p> <p>Email: <a href="mailto:liuf53@mail.sysu.edu.cn">liuf53@mail.sysu.edu.cn</a> (Liu, Feng)</p> <p><strong><em>Brief view of the dataset</em></strong></p> <p>Hydrodynamics, suspended sediment concentration and salinity distribution were measured&nbsp;at three fixed stations along the longitudinal direction of the estuary.&nbsp;The stations were located at Guadingjiao (M1), inside the bar (M2), and outside the bar (M3), and sampling was simultaneously conducted at neap tide (NT) from July 31 to August 1 and spring tide (ST) from August 8 to August 9 in 2017. All observation data has been compiled to include data from the surface to the bottom six layers within 26 hours. This directory contains the following datasets.</p> <p><strong>M10731.xlsx: </strong>Current velocity, current direction, salinity and SSC during neap tide at Station M1&nbsp;</p> <p><strong>M10808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M1&nbsp;</p> <p><strong>M20731.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during neap tide at Station M2</p> <p><strong>M20808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M2</p> <p><strong>M30731.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during neap tide at Station M3</p> <p><strong>M30808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M3</p>