您的位置: 专家智库 > >

国家自然科学基金(40476008)

作品数:4 被引量:21H指数:2
相关作者:宋金宝陈小刚孙群管长龙丁赟更多>>
相关机构:中国科学院中国海洋大学更多>>
发文基金:国家自然科学基金国家教育部博士点基金国家高技术研究发展计划更多>>
相关领域:天文地球更多>>

文献类型

  • 4篇中文期刊文章

领域

  • 4篇天文地球

主题

  • 2篇海洋动力
  • 2篇波浪
  • 1篇东中国海
  • 1篇应力
  • 1篇应力影响
  • 1篇有效波高
  • 1篇中国海
  • 1篇卫星高度计
  • 1篇海面
  • 1篇海面风
  • 1篇海洋动力学
  • 1篇风浪
  • 1篇风速
  • 1篇概率分布
  • 1篇高度计
  • 1篇RELATI...
  • 1篇TURBUL...
  • 1篇BETWEE...

机构

  • 1篇中国科学院
  • 1篇中国海洋大学

作者

  • 1篇丁赟
  • 1篇管长龙
  • 1篇孙群
  • 1篇陈小刚
  • 1篇宋金宝

传媒

  • 2篇海洋科学
  • 2篇Chines...

年份

  • 1篇2008
  • 2篇2007
  • 1篇2006
4 条 记 录,以下是 1-4
排序方式:
利用TOPEX卫星高度计资料分析东中国海的风、浪场特征被引量:14
2006年
利用TOPEX卫星高度计和日本气象厅浮标观测资料,对东中国海的有效波高和风速进行比较,分析了卫星高度计资料的有效性。利用有效波高和风速的3种概率密度函数分布,结合TOPEX卫星高度计资料,并采用最大似然方法对统计分布参数进行估计,结果表明,有效波高的对数-正态概率密度分布与观测资料的直方图在有效波高的整个范围内符合较好,风速的直方图与Weibul概率密度分布符合较好。同时,分析了有效波高大于4 m的巨浪在东中国海的时空分布特征,表明巨浪多出现在冬、秋两季,平均有效波高最大值出现在夏季,且主要分布在东中国海东南部。
孙群宋金宝陈小刚
关键词:卫星高度计有效波高风速概率分布
风浪状态对海面风应力影响的初步研究被引量:1
2007年
利用新近提出的海面风应力系数线性参数化理论,定性地分析了已有风应力和风浪的观测数据。分析发现这些观测数据表明在小波陡的情形下海面风应力系数随风速的变化较大波陡的情形更加迅速。结果定性地倾向于支持Toba等的结果,即成熟的风浪较年轻的风浪更加粗糙。
丁赟管长龙
关键词:风浪
A relationship between wave steepness and wave age for wind waves in deep water
2007年
Studying the relationship between wave steepness and wave age is important for describing wind wave growth with energy balance equation of significant waves. After invoking the dispersion rela- tion of surface gravity wave in deep water, a new relationship between wave steepness and wave age is revealed based on the “3/2-power law” (Toba, 1972), in which wave steepness is a function of wave age with a drag coefficient as a parameter. With a given wave age, a larger drag coefficient would lead to larger wave steepness. This could be interpreted as the result of interaction between wind and waves. Comparing with previous relationships, the newly proposed one is more consistent with observational data in field and laboratory.
刘斌丁赟管长龙
关键词:海洋动力学波浪
Wave breaking on turbulent energy budget in the ocean surface mixed layer被引量:6
2008年
As an important physical process at the air-sea interface, wave movement and breaking have a significant effect on the ocean surface mixed layer (OSML). When breaking waves occur at the ocean surface, turbulent kinetic energy (TKE) is input downwards, and a sublayer is formed near the surface and turbulence vertical mixing is intensively enhanced. A one-dimensional ocean model including the Mellor-Yamada level 2.5 turbulence closure equations was employed in our research on variations in turbulent energy budget within OSML. The influence of wave breaking could be introduced into the model by modifying an existing surface boundary condition of the TKE equation and specifying its input. The vertical diffusion and dissipation of TKE were effectively enhanced in the sublayer when wave breaking was considered. Turbulent energy dissipated in the sublayer was about 92.0% of the total depth-integrated dissipated TKE, which is twice higher than that of non-wave breaking. The shear production of TKE decreased by 3.5% because the mean flow fields tended to be uniform due to wave-enhanced turbulent mixing. As a result, a new local equilibrium between diffusion and dissipation of TKE was reached in the wave-enhanced layer. Below the sublayer, the local equilibrium between shear production and dissipation of TKE agreed with the conclusion drawn from the classical law-of-the-wall (Craig and Banner, 1994).
孙群管长龙宋金宝
关键词:波浪海洋动力
共1页<1>
聚类工具0