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Meteor radar estimation of Gravity Wave Variances and Momentum Fluxes in the mesosphere lower thermosphere: Evaluation of different methods using simulations and observations over three tropical locations

机译:流星雷达估计中层低层热圈中的重力波方差和动量通量:通过对三个热带地区的模拟和观测,对不同方法进行评估

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Meteor Radar is widely used to study Gravity wave (GW) variances and their Momentum Fluxes (MFs) at mesospheric altitudes. However, the accuracy of meteor radar observations of GWMF should be evaluated before they can be used for research applications. In this regard, the present study evaluates the meteor radar observations of GWMF obtained from Thumba [8.5°N, 77°E (2006- 2015)], Kototabang [0.2°S, 100.3°E (2002-2017)] and Tirupati [13.63°N, 79.4°E (2013-2018)]. These radars provide hourly zonal and meridional wind observations round the clock in 80-100 km height domain known as mesosphere lower thermosphere region. Three methods are employed to evaluate the meteor radar performance in estimating the simulated GWMFs, Viz., 1) Day by day analysis, which is traditional Hocking method 2) Composite day analysis and 3) Modified Composite day analysis. After evaluating these methods by employing GW simulations, it is found that modified composite day analysis shows good agreement and the same is used for constructing the GWMF climatologies over the observational locations. The significance of the present study lies in evaluating the three different methods for estimating GWMF by employing GW simulations and meteor radar observations.
机译:流星雷达广泛用于研究MeSospheric海拔高度的重力波(GW)差异及其动量助熔剂(MFS)。然而,在可以用于研究应用之前,应该评估GWMF的流星雷达观测的准确性。在这方面,本研究评估了由缩略图获得的GWMF的流星雷达观察[8.5°N,77°E(2006-2015)],Kototabang [0.2°S,100.3°E(2002-2017)]和Tirupati [ 13.63°N,79.4°E(2013-2018)]。这些雷达提供了每小时的地形和子午线,在80-100km高度域名的时钟圆形,称为Mesosphere下热层区域。采用三种方法评估估计模拟的GWMFS,VIZ的流星雷达性能,即,1)日期分析,即传统的霍普方法2)复合日分析和3)改良复合日分析。通过采用GW模拟评估这些方法之后,发现修饰的复合日分析显示了良好的一致性,并且该分析具有良好的一致性,而且用于在观测位置构建GWMF气候。本研究的重要性在于通过采用GW仿真和流星雷达观测来评估用于估计GWMF的三种不同方法。

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