塩水遡上が筑後川感潮河道の分派・合流に与える影響

Kaneko, Yu; Olap, Neriezza; Yokoyama, Kenichi

doi:10.2208/jscejhe.76.2_i_1405

Cited by 2 publications

(1 citation statement)

References 4 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Kaneko et al 9,10) explains that the Chikugo, Arakawa, and Sumida Rivers, where the meander differences between the main channel and branch (Chikugo: main channel: 1.03, branch: 1.17; Arakawa: main channel: 1.20, branch: 1.57) are small and counter-current flow is absent. In TRE, the meander difference (main channel: 1.1, branch: 2.1) are large and counter-current flow exist.…”

Section: ) Effect Of Topography On Counter-current Flowmentioning

confidence: 99%

Topography and Tidal Variations: Impact on Counter-Current Flow at the Confluence Area of Tanintharyi River Estuary

HLAING,

AZHIKODAN,

YOKOYAMA

2024

Journal of JSCE

Self Cite

View full text Add to dashboard Cite

The impact of topography and tidal forcing on counter-current flow formation in monsoon-affected multi-channel macrotidal river estuaries is seldom studied. This research investigates the occurrence of counter-current flow during the monsoon season, characterized by strong semi-diurnal tidal currents, at the confluence area of the complex multi-channel macrotidal Tanintharyi River estuary (TRE) in Myanmar. Continuous measurements of velocity and discharge, along with surveys of topography and water quality (salinity, turbidity), were conducted during a 12-hour intensive survey (30-minute intervals) at the upstream junction area of the main channel and the branch during the spring tide. The main channel's width, approximately four to five times larger than the branch's width, experiences counter-current flow during ebb tide when water levels between the two channels are similar. Despite the freshwater environment and stable turbidity indicated by vertical profiles, tidal effects still influence counter-current flow formation. The imbalance in area and discharge ratios between the main channel and branch can be attributed to another important factor: downstream topography. The main channel with wide (1.3 km), straight (SI: 1.1), and short (28 km) topography, is highly sensitive to tides compared to branch with the narrow (180 m), meandering (SI: 2.1), and long (40 km) topography. The difference in downstream topography between the main channel and branch, combined with tidal forcing, plays a crucial role in counter-current flow formation in the upstream junction area of the TRE.

show abstract

Section: ) Effect Of Topography On Counter-current Flowmentioning

confidence: 99%