Water and sediment dynamics in the Red River mouth and adjacent coastal zone

2007 ◽  
Vol 29 (4) ◽  
pp. 508-522 ◽  
Author(s):  
D.S. van Maren
2011 ◽  
Vol 38 (4) ◽  
pp. 453-469 ◽  
Author(s):  
E. N. Dolgopolova ◽  
M. V. Isupova

Author(s):  
Nguyen Ngoc Tien ◽  
Dinh Van Uu ◽  
Nguyen Tho Sao ◽  
Do Huy Cuong ◽  
Nguyen Trung Thanh ◽  
...  

Author(s):  
Le Xuan Thuyen

A small mangrove colony growing for several decades on a mud flat on the left side of Balat River mouth has become today a large and healthy forest, containing a high ecosystem service value in the core of the Red River biosphere reserve. As a pioneer ecosystem located at land– water interface in the tropic, there exist always risks to mangroves, especially due to climate change and sea level rise. Sea level rise is a worldwide process, but subsidence is a local problem that can exacerbate these geo-hazards. A monitoring of shallow subsidence has been carried out by using SET-MH technique (developed by the United States Geological Survey) to track the both accretion and land sinking in the core zone of the National Park. The measurement shows the average sedimentation rate of 2.9 cm / yr and the sinking rate of 3.4 cm / yr, since Dec. 30th 2012. This is the first ground-based observation of shallow subsidence under mangroves in the Tonkin Gulf. As a simple and low cost method, so further expansion of this monitoring could provide more useful information to help identify the generally sinking trend of coastal areas in the Red River Delta and also to protect its own biosphere reserve.


2018 ◽  
Vol 23 (12) ◽  
pp. 05018020 ◽  
Author(s):  
George L. Mamede ◽  
Andreas Guentner ◽  
Pedro H. A. Medeiros ◽  
José Carlos de Araújo ◽  
Axel Bronstert

APAC 2019 ◽  
2019 ◽  
pp. 837-843
Author(s):  
Dang Thi Huyen ◽  
Le Nhu Da ◽  
Vu Duc Toan ◽  
Le Thi Phuong Quynh ◽  
Duong Thi Thuy

2020 ◽  
Vol 12 (18) ◽  
pp. 2875
Author(s):  
Mathieu Gentil ◽  
Gaël Many ◽  
Xavier Durrieu de Madron ◽  
Pierre Cauchy ◽  
Ivane Pairaud ◽  
...  

The recent integration of Acoustic Doppler Current Profilers (ADCPs) onto underwater gliders changes the way current and sediment dynamics in the coastal zone can be monitored. Their endurance and ability to measure in all weather conditions increases the probability of capturing sporadic meteorological events, such as storms and floods, which are key elements of sediment dynamics. We used a Slocum glider equipped with a CTD (Conductivity, Temperature, Depth), an optical payload, and an RDI 600 kHz phased array ADCP. Two deployments were carried out during two contrasting periods of the year in the Rhone River region of freshwater influence (ROFI). Coastal absolute currents were reconstructed using the shear method and bottom tracking measurements, and generally appear to be in geostrophic balance. The responses of the acoustic backscatter index and optical turbidity signals appear to be linked to changes of the particle size distribution in the water column. Significantly, this study shows the interest of using a glider-ADCP for coastal zone monitoring. However, the comparison between suspended particulate matter dynamics from satellites and gliders also suggests that a synoptic view of the processes involved requires a multiplatform approach, especially in systems with high spatial and temporal variability, such as the Rhone ROFI area.


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