Seasonal distribution of suspended sediments in the water northeast to Shandong Peninsula and its controlling factors
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摘要:
基于2018年山东半岛东北部海域冬、夏两季悬浮体浓度、浊度及水温和盐度调查资料,分析了研究区水体悬浮体浓度的季节性变化,探讨了其控制因素。结果表明:夏季浊度在0.2~37.8FTU之间变化,冬季浊度在1.5~100.1FTU之间变化,均表现为底高表低、东高西低的特征。夏季水温分层明显,表现为表层高、底层低的特征,盐度整体无明显变化;冬季温盐垂向上混合均匀,平面上表现为近岸低温低盐水体向远岸高温高盐水体的过渡。悬浮体浓度分布受潮流、波浪、温跃层和温盐锋面等因素影响。夏季,悬浮体垂向上受到温跃层影响,底层悬浮体难以向表层输运;平面上潮混合和波浪差异性作用阻碍了悬浮体的水平输运。冬季,强风浪促使悬浮体垂向混合剧烈,表层悬浮体浓度明显较夏季变高;平面上沿岸流和黄海暖流形成的温、盐锋面阻碍了水团间悬浮体的输运。
Abstract:Based on the characteristics of suspended matter, such as sediment content, turbidity, temperature and salinity, acquired in the summer and winter of 2018 in the water northeast to the Shandong Peninsula, we studied the seasonal variation of suspended sediment and it’s controlling factors. The results show that the turbidity varies from 0.2 to 37.8 FTU in summer, 1.5 to 100.1 FTU in winter, of which both are high on the bottom and low on the surface and high in the east and low in the west. Concerning water temperature, it is obviously stratified in summer, high on the surface and low on the bottom. However, there is no obvious changes as far as salinity is considered. In the winter time, both the temperature and salinity show a transition from the low temperature and low salinity water mass near the shore to the high temperature and high salinity water mass off the coast on plane, and evenly mixed in vertical direction. The distribution of suspended sediment content is controlled by various factors, such as tide, wave, thermocline, temperature and salinity fronts. In summer, affected by the thermocline vertically, the suspended sediments in bottom water are difficult to move into the upper layer, while tidal mixing and wave differentiation will accelerate the exchange of suspended sediment between the near shore and the far shore areas. However, the content of surface suspended matter is significantly higher in winter, because of the intensification of vertical mixing by strong wind and waves. The temperature and salinity front, formed by the coastal current and the Yellow Sea warm current, will block the exchanges of suspended sediments between water masses.
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Key words:
- suspended sediment content /
- thermocline /
- fronts /
- Shandong Peninsula
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图 1 黄海冬季环流及夏季冷水团分布图[23]
Figure 1.
图 13 黄海M2分潮潮流椭圆及最大潮流分布图[25]
Figure 13.
表 1 夏季温度、盐度
Table 1. Water temperature and salinity in summer
层位 表层 中层 底层 温度/℃ 盐度/PSU 温度/℃ 盐度/PSU 温度/℃ 盐度/PSU 最大值 28.8 32.28 21.7 32.25 21.0 32.31 最小值 20.4 31.71 15.0 31.70 14.2 31.85 平均值 25.4 32.00 18.6 31.98 17.4 31.99 表 2 冬季水温和盐度特征值
Table 2. Water temperature and salinity in winter
层位 表层 中层 底层 温度/℃ 盐度/PSU 温度/℃ 盐度/PSU 温度/℃ 盐度/PSU 最大值 9.9 31.97 9.9 31.99 9.9 31.99 最小值 6.4 31.13 6.3 31.19 6.3 31.15 平均值 7.4 31.36 7.4 31.39 7.4 31.38 表 3 冬季和夏季水体浊度特征值
Table 3. Water turbidity in winter and summer
FTU 夏季 冬季 表层 中层 底层 表层 中层 底层 最大值 2.3 8.9 37.8 22.4 44.0 100.1 最小值 0.2 0.2 2.9 1.5 2.3 3.9 平均值 0.6 2.5 9.3 9.2 13.0 23.4 -
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