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- tide-induced bottom boundary layer 潮流边界层
- bottom boundary layer parameters 边界层参数
- ESTUARINE AND COASTAL BOTTOM BOUNDARY LAYER AND FINE SEDIMENT PROCESSES 河口海岸底部边界层和细颗粒泥沙过程
- Observations and modeling of the tidal bottom boundary layer on the southern flank of Georges Bank 对乔治滩岸南侧潮汐底边界层的观测和模拟
- Bottom boundary layer flow and salt injection from the continental shelf to slope 来自对斜坡而言的大陆架边界层流底部和盐注入
- Standing regular wave groups with oblique incidence: Phase averaging and bottom boundary layer in constant depth 倾斜入射的稳定正规波组:在固定深度中阶段平均和底部边界层
- Study on wave bottom boundary layers over a rippled bed 波浪作用下沙纹床面底层流动特性研究
- THE PROGRESS OF RESEARCH ON THE COHERENT STRUCTURE IN OSCILLATORY FLOW BOTTOM BOUNDARY LAYER AND ITS INTERACTION WITH THE SEDIMENT 振荡流底层拟序结构及其与泥沙相互作用研究
- bottom boundary layer 底边界层
- Sound Propagation in the Nocturnal Boundary Layer. 夜间边界层中的声传播。
- Detection of Boundary Layer Water Clouds by Spaceborne Cloud Radar. 用机载云雷达探测边界层含水云。
- Beyond the boundary layer, the motion is highly irregular. 超出边界层以外,流体的流动非常没有规律。
- The bottom boundary of Malan loess or the development of the first paleosol is chronologically different from place to place. 马兰黄土底界或第1古土壤层的发育是穿时的。
- Formulation of Turbulent Fluxes in the Stable Boundary Layer. 稳定边界层中湍流通量算法。
- Stull, R.B., 1988: An introduction to boundary layer meteorology. 任平,2003:影响大气污染物散布的气象条件。
- A numerical simulation of 3-D complicated turbulent flow in tailwater is studied.The effects of solid bottom boundary and free surface are considered in the simulation. 摘要对具有工程意义的挑射水流冲击射流导致的尾水河道三维紊流流场进行了数值模拟,计算中考虑了固体边界条件和自由水面条件对水流结构的影响。
- The bottom boundary of sequence 2 belongs to tectonically compressed unconformity that originates from the pressure of plates and decline of basin base. 层序2底界面是周缘板块强烈挤压、盆地挠曲下降作用结果,同期全球海平面快速上升;
- As the air proceeds along the test section the boundary layer thickens. 当空气沿着试验段流动时附面层逐渐变厚。
- The Contribution of Shear to the Evolution of a Convective Boundary Layer. 切变对对流边界层演变的作用。
- The bottom boundary of sequence 3, sequence 4 and sequence 5 results from integrated effect of change of climate, sediment source and tectonic activity under falling global eustacy. 层序3、层序4和层序5的底界面是在构造作用稳定、全球海平面下降背景之上由相对海平面次一级旋回变化形成的,是古气候变化、沉积物供给及构造沉降共同作用的结果。