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An Observational Study of Sea- and Land-Breeze Circulation in an Area of Complex Coastal Heating

机译:沿海复杂供热地区海陆风环流的观测研究

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摘要

The diurnal evolution of the three-dimensional structure of a mesoscale circulation system frequently occurring in the area of Kennedy Span Center-Cape Canaveral has been studied using the data from the Kennedy Space Center Atmospheric Boundary Layer Experiment (KABLE). The case was chosen from the spring intensive data-collection period when the greatest daytime temperature difference between land and water (sea and inland rivers) occurs and the local circulations are most intense. The daytime flow structure was determined primarily by the mesoscale pressure-gradient form created by the temperature contrast between land and water. A strong sea-breeze circulation, the dominant feature of the daytime flow field, was modified by a local inland river breeze known as the Indian River breeze, in that divergent flow over the river enhanced the sea-breeze convergence on the seaward side and generated additional convergence on the landward side of the river. The rivers near the coastline also modified the initial flow field by enhancing convergence in the surrounding areas and speeding up the movement of the sea-breeze front. The nighttime flow structure was dominated by a large-scale land breeze that was relatively uniform over the area and became quasi-stationary after midnight. The nonuniformity of the wind-vector rotation rate suggests that mesoscale forcing significantly modifies the Coriolis-induced oscillation. No clear convergence patterns associated with the rivers were observed at night. Detailed characteristics over a diurnal cycle of the sea-land breeze and of the river breeze onset time, strength, depth, propagation speed and both landward and seaward extension, are documented in this study. Some boundary-layer characteristics needed for predicting diffusion of pollutants released from coastal launch pads, including atmospheric stability, depth of the thermal internal boundary layer, and turbulent mixing are also discussed.
机译:利用肯尼迪航天中心大气边界层实验(KABLE)的数据研究了肯尼迪跨度中心-卡纳维拉尔角频繁发生的中尺度环流系统三维结构的日变化。该案例是从春季密集数据收集时段中选取的,当时春季陆地和水(海洋和内陆河流)之间出现最大的日温差,并且当地的环流最为强烈。白天的流量结构主要由陆与水之间的温度对比产生的中尺度压力梯度形式决定。强烈的海风循环是白天流场的主要特征,被当地的内陆河风(称为印度河风)所改变,因为河道上的分叉流增强了海风在朝海一侧的汇聚并产生了在河的陆侧有更多的汇合。海岸线附近的河流还通过增强周围地区的汇聚和加快海风锋的移动来改变初始流场。夜间的流动结构主要由大规模的陆风主导,该陆风在该地区相对均匀,并在午夜后变为准平稳状态。风矢量旋转速率的不均匀性表明,中尺度强迫显着改变了科里奥利引起的振荡。晚上没有观察到与河流有关的清晰收敛模式。在这项研究中,记录了海陆风和河风起伏时间,强度,深度,传播速度以及陆向和向海延伸的昼夜周期的详细特征。还讨论了预测从沿海发射台释放的污染物扩散所需的一些边界层特征,包括大气稳定性,内部热边界层深度和湍流混合。

著录项

  • 作者单位
  • 年度 1992
  • 总页数
  • 原文格式 PDF
  • 正文语种 en
  • 中图分类
  • 入库时间 2022-08-20 20:23:37

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