New seismic data support Cenozoic rifting in George VI Sound, Antarctic Peninsula

New multifold seismic-reflection and wide-angle reflection/refraction data across George VI Sound, Antarctic Peninsula, show the presence of graben and horst structures indicating an extensional origin. The data suggest that rocks of an accretionary complex and fore-arc basin underlie the Sound and are in faulted contact along its eastern boundary with volcanic and plutonic rocks of the associated Mesozoic arc of western Palmer Land. A cover of possible syn- and postglacial Cenozoic deposits drapes the structures. The combination of new seismic, synthetic-aperture radar and previously acquired data suggests subduction-related rifting in the Sound was segmented, with opening in the south predominately by normal extension whilst in the north, dextral transtension predominated.     

双线偏振雷达的设计问题

双线偏振雷达作为一种实用的特种天气雷达正日益受到人们的关注，对双线偏振雷达设计中特有的天线系统，发射接收系统，数据处理系统等应注意的一些问题及设计指标进行了讨论，其结果对双线偏振雷达的研制有一定的参考价值。     

由单Doppler雷达资料反演水平风场的简单共轭函数方法的改进方案

该文改进了Qiu和Xu提出的由单个Doppler雷达探测的资料反演水平风场的简单共轭（simple adjoint）函数方法。其基本做法是将控制方程中的状态变量改用其时间距平量代替，并加入一待反演的方程误差项。利用1988年夏季在美国丹佛机场所作的一次下击暴流的双Doppler雷达观测试验资料对新方法作了检验，结果表明其对反演结果的改善是显著的。     

冷涡条件下雹云的雷达回波分析及冰雹预报

利用一次冷涡南下引起的两次强对流天气的数字化雷达回波资料，结合黄河三角洲地区的天气学资料，对比分析了两交冰雹及冰雹和暴雨回波的异同点，为强对流天气的临近预报和人工防雹提供参考。     

用机载多普勒雷达资料进行三维风场解析反演 I. 多重解析多普勒方法在机载雷达情况下的推广及模拟验证

多重解析多普勒（MANDOP）方法是用解析表达式进行三维风场反演。它成功地应用于处理地基多普勒雷达资料，获取对流系统层状降水区域的风场结构。本文将MANDOP方法在机载雷达情况下的进行推广并通过模拟研究径向速度测量中信号噪声、雨滴降落速度估计误差、平流速度估计误差、尤其是由于机载特性的引入产生的雷达束定位误差等对方法的影响。模拟结果显示，在机载雷达的技术参数下，MANDOP方法能够提供误差可以接受的三维风场反演。这为利用MANDOP方法处理在CaPE实验中获取的历史上第一次机载双束多普勒雷达资料建立了可靠的基础。     

一种卫星和雷达资料结合的强降水临近预报方法

在短期和短时天气预报的基础上，通过对气象卫星红外数字资料的定量处理和统计分析，作出降水云系的实时降雨量估计，并根据降水云系生命史的演变和移动、传播等特征，结合天气系统分型和雷达回波资料，提出一种北京密云水库上游潮河，白河流域区域性０－３小时强降水临近预报方法。     

数字化3cm天气雷达定量测量降水的结果和讨论

本文讨论了3cm天气雷达在兰州地区定量测量降水及其精度;分析了不同降水类型和衰减等对测量的影响;讨论了地面雨量计订正雷达测量值的方法和效果。     

Wind fluctuations near a cold vortex-tropopause funnel system observed by the MU radar

Vertical and temporal variations of three-dimensional wind velocity associated with an upper-tropospheric cold vortex-tropopause funnel system were observed by an MST radar in Japan (the MU radar). Marked changes of vertical velocity and horizontal wind direction were found between the inside and outside of the cold vortex. The vertical velocity activity outside the vortex was asymmetric; it was most active in a sector before the vortex. Unsaturated internal gravity waves in their generation stage contribute predominantly to the vertical velocity activity, suggesting that tropospheric occluded cyclones may be a possible source of middle-atmospheric gravity waves through the geostrophic adjustment process.     

Internal gravity wave selection in the upper troposphere and lower stratosphere observed by the MU radar: Preliminary results

Marked wavelike variations of the lower stratospheric wind observed on 7–10 May, 1985 by an MST radar in Japan (by the MU radar) are analyzed assuming that they are induced by monochromatic internal inertio-gravity waves. These variations are mainly composed of two modes (periods: 22 and 24 hours), both of which have zonal phase velocities (C _X ) slower than the mean westerly wind (). A statistical analysis of the zonal phase velocity shows thatC _X above andC _X below the tropopause jet stream, which is considered to be a vivid proof of wave selection due to the tropospheric mean flow and upward wave emission from the tropopause jet. A comparison between the MU radar results and routine meteorological observations leads to the conclusion that the marked waves appear when the jet stream takes a maximum wind speed.     

A study on the sensitivity of the radar scattering coefficient to oceanic winds

Sensitivity of the radar scattering coefficient to the oceanic wind vector in the midangular range for frequencies from L- to Ku- band is studied. This is based on computations of scattering coefficient via the two-scale scattering theory employing a semi-empirical model for the ocean spectrum suggested by Fung and Lee and the slope distribution by Cox and Munk. Higher frequency and incident angles of over 45 degrees seem to yield better wind sensitivity.