期刊文献+

黄河三角洲半日潮无潮区位置及水文特征分析 被引量:11

THE ANALYSIS OF HYDROGRAPHICAL CHARACTERISTICS IN THE NONTIDAL REGION M2 NEAR THE DELTA OF THE HUANGHE RIVER
下载PDF
导出
摘要 It is very important to study the nontidal region, because characteristics in this area are very useful to us, for example, the tide range is small and the tide current is very strong. Suspended load isn’t easy to deposite and the bed load is easy to move along the sea bed. Since 1936 many scientists think that there is a nontidal point M2 in the old eatuary (38°-38°10′N, 119°-119°20′E), and have determined the location of nontidal point. According to our observation, it isn’t a nontidal point but a nontidal line. This line is located near the section B.On the 15th day of lunar calendar this line is just located at section B, and in other days this line moves toward section A, but does’nt arrive in seetion A. The tide data that,have been observed on coast tide stations give eloquent proof of fact of nontidal line. In this region of near nontidal line the current speed is more than 90cm/sec., and the maximum is 120cm/sec. The minimum of tide range is about 30cm and the maximum is about 100cm. During the flood tide the current direction is south-east, and north-weat during the ebb tide. The residual current speed on section B is about 0.2 knot,and flow into north-west. It is very important to study the nontidal region, because characteristics in this area are very useful to us, for example, the tide range is small and the tide current is very strong. Suspended load isn't easy to deposite and the bed load is easy to move along the sea bed.Since 1936 many scientists think that there is a nontidal point M2 in the old eatuary (38°-38°10'N, 119°-119°20'E), and have determined the location of nontidal point. According to our observation, it isn't a nontidal point but a nontidal line. This line is located near the section B. On the 15th day of lunar calendar this line is just located at section B, and in other days this line moves toward section A, but does'nt arrive in section A. The tide data that have been observed on coast tide stations give eloquent proof of fact of nontidal line. In this region of near nontidal line the current speed is more than 10 cm/see., :and the maximum is 120 cm/see The minimum of tide range is about HO cm and the maximum is about 100 cm. During the flood tide the current direction is south-east, and north-weat during the ebb tide. The residual current speed on section B is about 0.2 knot,and flow into north-west.
出处 《山东海洋学院学报》 1985年第1期127-136,共10页
  • 相关文献

同被引文献154

引证文献11

二级引证文献103

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部