首页> 外文会议>2014 31st URSI General Assembly and Scientific Symposium >MST radar (53 MHz) observation of atmospheric polarized scatterers: A great implication for astronomical observations
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MST radar (53 MHz) observation of atmospheric polarized scatterers: A great implication for astronomical observations

机译:MST雷达(53 MHz)对大气极化散射体的观测:对天文观测的重要意义

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The present work reports that the Earth's atmosphere can sometimes exhibit polarized characteristics such that any polarized light coming from the outer space can get modulated easily by these polarized refractive index structures of the atmosphere. Utilizing the Mesosphere Stratosphere Troposphere (MST) radar operating at a very high frequency of 53 MHz in the Indian tropical region of Gadanki, two sets of data are collected for the heights of 2–20 km during (a) 09–10 February 2009 and 06–07 June 2011. The data comprise of atmospheric scattering properties like signal to noise ratio (SNR), Doppler spectral width of the echoes and the atmospheric dynamical parameters like all the three components of wind velocities and their vertical shears. The wind dynamics has been utilized to determine whether the atmosphere was in dynamically unstable conditions that would lead to the generation of turbulence in the atmosphere, Since the MST radar has two sets of 1024 orthogonally polarized antennae aligned along the zonal and meridional directions, it is possible to transmit polarized narrow beams and get echoes accordingly. From these two data sets, one (2009) has been identified as a normally observed echoes and the other data (2011) contain the polarized signals received.
机译:本工作报告说,地球大气层有时会表现出偏振特性,这样,来自外层空间的任何偏振光都可以通过大气层的这些偏振折射率结构轻松调制。利用印度加丹基热带地区以53 MHz的非常高频率运行的中层平流层对流层(MST)雷达,在(a)2009年2月9日至10日期间,收集了2至20 km高度的两组数据。 2011年6月6日至7日。数据包括大气散射特性,如信噪比(SNR),回波的多普勒频谱宽度以及大气动力学参数,如风速的所有三个分量及其垂直切变。利用风动力学来确定大气层是否处于动态不稳定条件下,从而导致大气湍流的产生。由于MST雷达具有两组沿纬向和子午线方向排列的1024个正交极化天线,因此可以透射偏振窄光束并获得相应的回声。从这两个数据集中,一个(2009)已被识别为正常观察到的回波,另一个数据(2011)包含了接收到的极化信号。

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