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Determination of the meteoroid ionization coefficient using high power large aperture radar.

机译:使用大功率大口径雷达确定流星电离系数。

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Most meteoroids have physical cross-sections too small to detect by ground based sensors. To overcome this problem we applied a radar [ARPA Long Range Tracking and Instrumentation Radar (ALTAIR)] with greater capabilities than made available by any other meteor radar to collect measurements from meteor electrons at the leading edge or head of their atmospheric flight path. These ALTAIR head echo data provided the foundation for us to develop new techniques and advance the science of meteoroid-atmosphere interactions. ALTAIR provides high-power, large aperture, high bandwidth, simultaneous UHF and VHF pulsed waveforms, high range resolution, monopulse angle, precise absolute calibration in range and angle and high sensitivity. Leveraging ALTAIR's assets, we collected a greater number of independent calibrated measurements than possible with other radar systems, thereby enhancing our estimates of meteoroid physical parameters (such as position, ionization coefficient, electron line density and mass) because of this reduction in the number of unknown quantities. Typical meteor radars collect fewer independent measurements at lower resolution (e.g. ∼kilometer to tens of kilometers in range). ALTAIR's periodic sampling at two frequencies also helped characterize and guard our investigation against wavelength dependent biases; the scattering characteristics of meteor electrons are a function of incident wavelength. Using these data we formulated a new approach to estimate a model for the meteor ionization coefficient using dynamical and radar cross section data. The ionization coefficient models the number of electrons produced during collisions between ablated meteoroid atoms and atmospheric constituents; it is central to the estimation of meteoroid parameters such as mass and density. Our approach adds missing information since the last estimate made by Jones (1997) because our value is valid for higher velocity meteors (near 56 km/sec), allows for values greater than unity and requires fewer assumptions. We also provide a comprehensive presentation of ALTAIR characteristics to illustrate the uncertainties in our meteoroid parameter estimates and to serve as a comparative guide for the interpretation of other meteor radar system capabilities.
机译:大多数流星体的物理横截面都太小,无法被地面传感器检测到。为了克服这个问题,我们使用了一种雷达[ARPA远程跟踪和仪器雷达(ALTAIR)],该雷达具有比任何其他流星雷达都更强大的功能,可以从其大气飞行路径的前沿或前端的流星电子收集测量值。这些ALTAIR头部回波数据为我们开发新技术和推进流星体与大气相互作用的科学奠定了基础。 ALTAIR提供高功率,大孔径,高带宽,同步UHF和VHF脉冲波形,高范围分辨率,单脉冲角度,范围和角度的精确绝对校准以及高灵敏度。利用ALTAIR的资产,与其他雷达系统相比,我们收集了更多的独立校准测量值,因此由于减少了天线数量,我们提高了对流星体物理参数(例如位置,电离系数,电子线密度和质量)的估计。数量未知。典型的流星雷达在较低的分辨率下(例如,千米到数十公里范围内)收集较少的独立测量值。 ALTAIR在两个频率上的定期采样还有助于表征和保护我们的研究免受波长相关偏差的影响;流星电子的散射特性是入射波长的函数。利用这些数据,我们制定了一种使用动态和雷达横截面数据估算流星电离系数模型的新方法。电离系数模拟了烧蚀的流星体原子与大气成分碰撞时产生的电子数。它对于流星体参数(例如质量和密度)的估计至关重要。自从Jones(1997)做出最后一次估计以来,我们的方法增加了缺失的信息,因为我们的值对于较高速度的流星(近56 km / sec)有效,允许值大于1且需要较少的假设。我们还提供ALTAIR特性的全面介绍,以说明流星体参数估计中的不确定性,并作为解释其他流星雷达系统功能的比较指南。

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