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- Near surface wind field 近地面风场
- First, a horizontally two-dimensional dynamical diagnosis model is set up in Cartesian coordinates, which is used to calculate surface wind field based on grid pressure data from weather maps by a computer scanning technique. 首先建立一个简单的水平二维地面风场诊断模式 ,根据由微机支持的数字化仪输入的地面格点气压场 ,诊断出地面风场 ;
- The conclusions are as follows:The surface wind field is highly asymmetric;the variance components of asymmetric surface wind field depend mainly on the airflow direction of wavenumber 1 and 2. 结果表明:台风近地层风场分布具有明显的不对称性,其方差大部分产生于波数1和2的气流中,并且与波的方向有关。
- sea surface wind field retrieval 海面风场反演
- the sea surface wind field numerical forecast 业务化海面风场数值预报
- characteristic of the surface wind field 地面风场特征
- Technical Research on Sea Surface Wind Field Forecast 海面风场预报的技术研究
- A Numerical Modelling Study of the Surface Wind Field in Beijing District 北京地区地面风场的数值模拟研究
- Time Variation of Cloud Distribution near Surface Wind Convergence Zone in the Nobi Plain during Daytime on Summer Sunny Days Nobi平原夏季大晴天白天期间的近地面风辐合区云分布的时间变化
- It was a surface wound and soon healed. 那是一个表面伤,不久便长好了。
- A HISTORY AND CURRENT SITUATION ON NUMERICAL PREDICTION OF SEA SURFACE WIND FIELD 海面风场数值预报的历史和现状
- Influence of initializing on the sea surface wind field numerical forecasting model in limited areas 初始化方案对有限区域海面风场数值预报模式的影响
- Ocean Surface Wind Field Retrieval of the Yangtze River Outlet from Spaceborne ERS-2 SAR Image 利用星载ERS-2 SAR进行长江口海面风场反演研究
- Surface wind unstable, take-off with caution. 风不稳定,起飞注意。
- Weak as it is, the disturbance in the wind field is discernible. 该风场的扰动虽然很弱,但是还是可以看得出来。
- Sustained surface wind near its centre is estimated at 28 kilometres per hour,with minimum sea level pressure of 1008 hPa. 扰动中心风力约每小时28公里,中心最低海平面气压为1008百帕斯卡。
- The concentration of total alkalinity was high in the near surface layer of the shelf area and the shelf break area. 陆架区的近表层和陆架坡折区分别有一个高碱度区。
- Statistical compartmentalization of surface wind field over coastal seas using high-resolution SAR-derived winds 使用高分辨率SAR-得自风在海岸线上方地面风场的统计划分
- However, people"cognition about paralic zone is far not enough, and the near surface structure of paralic zone is not simple as people imagined. 然而,现在对滩浅海地区认识还不够,同时,滩浅海地区近地表结构并不是想象的那么简单。
- A sharp temperature increase across the mid-mantle transition zone inhibits a simple downward-extrapolation from the near surface data. 中地幔过渡带有一个温度突然增加,因此不能根据近地表数据向下做简单的外推。