SOME METEO - HYDRO - DYNAMICAL FEATURES IN MEKONG RIVER MOUTH AREA
SOME METEO - HYDRO - DYNAMICAL FEATURES IN MEKONG RIVER MOUTH AREA
复制标题
湄公河口地区的一些气象-水力-动力特征
DOI:
10.15625/1859-3097/11/3/377
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发表时间:
2012
期刊:
影响因子:
--
通讯作者:
Nguyen Ba Xuan
中科院分区:
文献类型:
--
作者:
L. D. Mau;Pham Sy Hoan;V. Anh;N. C. Công;Nguyen Ba Xuan
This paper provides some meteo-hydro-dynamical feat ur s in Mekong River Mouth area which were based on statistical results from longtime measurement data such as wind, wave, sea water level, and river discharge. S tudy results show that distribution features of wind and wave characteristics are corresponding to seasonal variation. Predominant wind and wave directions during NE Monsoon period is NE, and in W, SW directions during SW Monsoon period. NE Monsoon period is from November to April (strongest in December and January), SW Monsoon period is from June to Septemb er (strongest in August). During NE Monsoon period the wind velocity and wave height we re higher than that of SW Monsoon period. Variation of SWL at Vungtau Station shows t hat he tide is semi-diurnal with maximum value occurred during NE monsoon period (highest in November), and minimum value occurred during SW Monsoon period (lowest in June). Variation of river discharge is similarly at two stations (Mythuan and Cantho). Dur ing flood season (from July to December) average monthly discharge was ranged from 4,000 to 15,800 m/s. During dry season (from January to May) average monthly discharge at both s tations was less than 4,000 m /s. Statistical data show that Mekong River Mouth area is a region of strong and complicated hydro-dynamical interaction processes between river and sea.