Effects of River Discharge and Tide Driven Sea Level Variation on Saltwater Intrusion in Sumjin River Estuary: An Application of Finite-Volume Coastal Ocean Model

被引:32
作者
Shaha, Dinesh Chandra [1 ,2 ]
Cho, Yang-Ki [1 ]
Kim, Tae-Wan [3 ]
机构
[1] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul 151742, South Korea
[2] Bangabandhu Sheikh Mujibur Rahman Agr Univ, Fac Fisheries, Gazipur 1706, Bangladesh
[3] Korea Polar Res Inst KOPRI, Inchon, South Korea
关键词
Modeling; FVCOM; saltwater intrusion; river discharge; Sumjin River estuary; climate change; SUBTIDAL SALINITY; CIRCULATION; STRATIFICATION; BAY;
D O I
10.2112/JCOASTRES-D-12-00135.1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Shaha, D. C.; Cho, Y.-K., and Kim, T.-W., 2013. Effects of river discharge and tide driven sea level variation on saltwater intrusion in Sumjin River estuary: An application of finite-volume coastal ocean model. Journal of Coastal Research, 29(2), 460-470. Coconut Creek (Florida), ISSN 0749-0208. Salinity intrusion is one of the major problems in the Sumjin River Estuary (SRE). An unstructured-grid finite-volume coastal ocean model (FVCOM) was used to investigate the influence of different river discharges and tide driven sea level variation on salinity intrusion in the SRE. The variation of salt intrusion was predicted according to the variation of sea level driven by tide along the open boundary and the river discharge upstream. The model simulation results are in qualitative agreement with the available field data. The model provided a skilled reproduction of the observed temporal and spatial variability in salinity. The ebb flow is seaward from upstream to the mouth of the SRE. The river discharge is a dominant factor affecting salinity intrusion in this estuarine system during the wet season. A power law function has been established between the distance of salt intrusion and river discharge. The salt intrusion length responding to constant river discharges generally follows a power law of -0.14. In contrast, the salt intrusion length shows a better relationship with intratidal sea level variation at low river discharge. This model result allows us to predict salt intrusion in an estuary according to the variation of sea level and river discharge with climate change.
引用
收藏
页码:460 / 470
页数:11
相关论文
共 44 条
[1]  
[Anonymous], GREENHOUSE EFFECT SE
[2]   Long-term trend of precipitation and runoff in Korean river basins [J].
Bae, Deg-Hyo ;
Jung, Il-Won ;
Chang, Heejun .
HYDROLOGICAL PROCESSES, 2008, 22 (14) :2644-2656
[3]  
Bell C., 1999, POL PSMSL TIDAL ANAL, V20
[4]   A dynamic equation for the potential energy anomaly for analysing mixing and stratification in estuaries and coastal seas [J].
Burchard, Hans ;
Hofmeister, Richard .
ESTUARINE COASTAL AND SHELF SCIENCE, 2008, 77 (04) :679-687
[5]  
Burkett V, 2001, CLIMATE CHANGE 2001: IMPACTS, ADAPTATION, AND VULNERABILITY, P343
[6]  
Chen C., 2006, 060602 U MASS SCH MA
[7]   Complexity of the flooding/drying process in an estuarine tidal-creek salt-marsh system: An application of FVCOM [J].
Chen, Changsheng ;
Qi, Jianhua ;
Li, Chunyan ;
Beardsley, Robert C. ;
Lin, Huichan ;
Walker, Randy ;
Gates, Keith .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2008, 113 (C7)
[8]  
Chen CS, 2003, J ATMOS OCEAN TECH, V20, P159, DOI 10.1175/1520-0426(2003)020<0159:AUGFVT>2.0.CO
[9]  
2
[10]  
Dyer K., 1997, Estuaries: A Physical Introduction