本文基于SWEM(Shallow Water Equation Model)三维水沙盐模式,考虑潮汐、径流、风场和波浪影响,在长江口与杭州湾及其邻近海域建立了一个高分辨的三维水沙盐模型。分析了一般天气条件下,舟山群岛海域在潮汐、径流、风场、波浪共同作用...本文基于SWEM(Shallow Water Equation Model)三维水沙盐模式,考虑潮汐、径流、风场和波浪影响,在长江口与杭州湾及其邻近海域建立了一个高分辨的三维水沙盐模型。分析了一般天气条件下,舟山群岛海域在潮汐、径流、风场、波浪共同作用下的地形冲淤与悬沙含量分布特征,并对比分析了一般天气条件下与台风天气条件下波浪对泥沙冲淤过程的影响。一般天气条件下,舟山群岛海域东西向水道为冲刷特征,舟山群岛东侧海域以及舟山群岛内部南北向水道为淤积特征。舟山群岛海域暖半年冲刷增强,冷半年淤积增强。海域悬沙含量由西北向东南迅速降低,群岛“虑沙”效果明显。悬沙含量3月份最大,8月份最小。波浪对舟山群岛海域泥沙冲淤过程的总体影响在秋冬季较强,春夏季较弱。一般天气条件下与台风天气条件下,波浪对研究海域泥沙冲淤过程影响显著的区域均为朱家尖东侧海域,且波浪的影响特征均表现为促进淤积和增加悬沙含量。一般天气条件下波浪引起最大淤积约占总淤积量的10%。台风天气条件下波浪引起的淤积量约是同时段一般天气条件下的6倍。展开更多
The characteristics of the roughness coefficient are very important for practical application. Some experiments are conducted to study the variation of Manning＇s n with flow depth, mean velocity, and density of veget...The characteristics of the roughness coefficient are very important for practical application. Some experiments are conducted to study the variation of Manning＇s n with flow depth, mean velocity, and density of vegetation,. An assumed velocity distribution to describe the vegetative flow of submerged vegetation is confirmed by experimental results. The measured velocities in this study seem to have little effect on the curve of n ~ h, and a new linear relationship between Manning＇s n and flow depths is observed clearly. According to the arguments that the flow resistance of densely unsubmerged vegetation is dominated by the resistance exerted on vegetations, the influence of the density of vegetation on Manning＇s n is estimated. On the basis of the velocity distribution, the n - h curve under submerged condition is theoretically obtained from the n - h curve under unsubmerged condition. These results are also well confirmed by experimental results and very significant for practical applications.展开更多
文摘本文基于SWEM(Shallow Water Equation Model)三维水沙盐模式,考虑潮汐、径流、风场和波浪影响,在长江口与杭州湾及其邻近海域建立了一个高分辨的三维水沙盐模型。分析了一般天气条件下,舟山群岛海域在潮汐、径流、风场、波浪共同作用下的地形冲淤与悬沙含量分布特征,并对比分析了一般天气条件下与台风天气条件下波浪对泥沙冲淤过程的影响。一般天气条件下,舟山群岛海域东西向水道为冲刷特征,舟山群岛东侧海域以及舟山群岛内部南北向水道为淤积特征。舟山群岛海域暖半年冲刷增强,冷半年淤积增强。海域悬沙含量由西北向东南迅速降低,群岛“虑沙”效果明显。悬沙含量3月份最大,8月份最小。波浪对舟山群岛海域泥沙冲淤过程的总体影响在秋冬季较强,春夏季较弱。一般天气条件下与台风天气条件下,波浪对研究海域泥沙冲淤过程影响显著的区域均为朱家尖东侧海域,且波浪的影响特征均表现为促进淤积和增加悬沙含量。一般天气条件下波浪引起最大淤积约占总淤积量的10%。台风天气条件下波浪引起的淤积量约是同时段一般天气条件下的6倍。
基金the National Natural Science Foundation of China (Grant No.50139029)the Chinese Offshore Investigation and Assessment 908 (PJ9:Study on effect of the Yangtze estuary flow field to the important sea project of shanghai).
文摘The characteristics of the roughness coefficient are very important for practical application. Some experiments are conducted to study the variation of Manning＇s n with flow depth, mean velocity, and density of vegetation,. An assumed velocity distribution to describe the vegetative flow of submerged vegetation is confirmed by experimental results. The measured velocities in this study seem to have little effect on the curve of n ~ h, and a new linear relationship between Manning＇s n and flow depths is observed clearly. According to the arguments that the flow resistance of densely unsubmerged vegetation is dominated by the resistance exerted on vegetations, the influence of the density of vegetation on Manning＇s n is estimated. On the basis of the velocity distribution, the n - h curve under submerged condition is theoretically obtained from the n - h curve under unsubmerged condition. These results are also well confirmed by experimental results and very significant for practical applications.
