量,可应用于天气雷达反射率基数据质量控制。
It can be applied to quality control CINRAD reflectivity data.
模拟的CAPE和雷达反射率因子等物理量均对此次降水过程有较好的指示意义。
The precipitation process can be explored through the simulation of the CAPE and radar reflectivity factor and other physic index from the WRF model.
利用模拟雷达反射率因子检验了模拟的正确性,结果表明模拟的暴雪的分布和强度都是可信的。
The simulation of radar reflectivity factor indicates that the simulation of snowstorm's precipitation distribution and intensity were reasonable.
该文介绍了一种自动识别和移除雷达反射率因子资料中亮带的算法,并对该算法进行了初步测试。
An automatic identification algorithm for the removal of bright band from radar reflectivity data is introduced and tested by case analysis and pre-operational run.
在介绍测雨雷达反演雷达反射率因子的标准算法的基础上,对雷达反射率因子反演算法进行了改进。
Precipitation radar's standard algorithms of retrieving radar reflectivity factor are introduced first and an improved method is brought forward.
请勿包括雷达基本反射率图像,因为它可能会使精确定位地区变得更困难。
Do not include the radar base reflectivity image as it can make precise area location more difficult.
最常用的雷达能量回程测绘形式是基本反射率图。
The most commonly used form of radar energy return mapping is the Base Reflectivity graph.
反射率偏移法(RDM)是合成孔径雷达(SAR)自聚焦的经典算法,当场景对比度较低时,RDM自聚焦效果变差。
Reflectivity Displacement Method (RDM) is a classical algorithm of Synthetic Aperture Radar (SAR) autofocus processing, whose performance degenerates with low contrast of the scene.
激光雷达系统的作用距离由下列因素决定:脉冲能量、脉冲宽度、光束发散角、大气衰减、目标反射率和接收机灵敏度等。
The operating distance of a laser radar system is determined on pulse energy, pulse width, beam divergence angular, atmosphere attenuation, target reflection, receiver sensitivity and so on.
通常非相干的常规天气雷达的应用仅仅是通过雷达回波强度的探测来提供天气目标物的位置和其反射率的信息。
Usually, conventional incoherent weather radar is used to provide only the information on the position of a weather target and its radar reflectivity by detecting echo intensity.
在外场用已知半球反射率的靶板作为标准靶板,反演测定目标靶板激光雷达散射截面和半球反射率。
Using a plate whose hemisphere reflectivity is known as a standard plate, the lidar scattering cross section (LRCS) and hemisphere reflectivity of a target plate are measured inversely.
分析结果表明:宁夏中北部气候干旱区强对流降水过程中,雷达组合反射率图像与中国南方相比,数值具有明显的差异。
Results showed that there are obvious differences of texture between the remote sense images of precipitation in Ningxia and that in south China.
地物和超折射等非降水回波是影响雷达定量探测降水和其他产品的重要因素,利用降水和非降水回波反射率三维结构特征可以对雷达数据进行质量控制。
Non-precipitation echo from radar such as ground objects echo and super refraction and so on are important to explore quantitatively precipitation and the other products.
利用多普勒天气雷达探测的反射率因子Z与含水量M的Z-M经验关系式,反演雨水含量。
This paper using the Z-M experience relations of the Doppler weather radar reflectivity factor Z and moisture content M to inverse the moisture content.
雷达组合反射率因子图上,MCS 表现为回波组织性强、模态清晰,或移动,或静止,MCS 雷达回波分布特征决定雨带走向和落区;
The radar echoes for those MCSs are organized well, and some MCSs are moving, others are quasi-stationary. The echo distributions of MCSs indicate the precipitation areas.
雷达组合反射率因子图上,MCS 表现为回波组织性强、模态清晰,或移动,或静止,MCS 雷达回波分布特征决定雨带走向和落区;
The radar echoes for those MCSs are organized well, and some MCSs are moving, others are quasi-stationary. The echo distributions of MCSs indicate the precipitation areas.
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