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Optimization of GPS water vapor tomography technique with radiosonde andCOSMIC historical data

机译:利用探空仪和探空仪优化GPS水蒸气层析成像技术。COSMIC历史数据

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摘要

The near-real-time high spatial resolution of atmospheric water vapordistribution is vital in numerical weather prediction. GPS tomographytechnique has been proved effectively for three-dimensional water vaporreconstruction. In this study, the tomography processing is optimized in afew aspects by the aid of radiosonde and COSMIC historical data. Firstly,regional tropospheric zenith hydrostatic delay (ZHD) models are improved andthus the zenith wet delay (ZWD) can be obtained at a higher accuracy.Secondly, the regional conversion factor of converting the ZWD to theprecipitable water vapor (PWV) is refined. Next, we develop a new method fordividing the tomography grid with an uneven voxel height and a varied watervapor layer top. Finally, we propose a Gaussian exponential verticalinterpolation method which can better reflect the vertical variationcharacteristic of water vapor. GPS datasets collected in Hong Kong inFebruary 2014 are employed to evaluate the optimized tomographic method bycontrast with the conventional method. The radiosonde-derived andCOSMIC-derived water vapor densities are utilized as references to evaluatethe tomographic results. Using radiosonde products as references, the testresults obtained from our optimized method indicate that the water vapordensity accuracy is improved by 15 and 12 % compared to those derived from theconventional method below the height of 3.75 km and above the height of3.75 km, respectively. Using the COSMIC products as references, the resultsindicate that the water vapor density accuracy is improved by 15 and 19 %below 3.75 km and above 3.75 km, respectively.
机译:大气水蒸气分布的近实时高空间分辨率对于数值天气预报至关重要。 GPS层析成像技术已被有效地用于三维水蒸气重建。在这项研究中,借助探空仪和COSMIC历史数据,在几个方面对层析成像处理进行了优化。首先,改进了对流层顶天顶静水滞后(ZHD)模型,从而可以更高的精度获得天顶湿滞后(ZWD)。接下来,我们开发一种新的方法来分割体素高度不均匀且水蒸气层顶部变化的层析X射线照片。最后,我们提出了一种高斯指数垂直插值方法,该方法可以更好地反映水蒸气的垂直变化特征。 2014年2月在香港收集的GPS数据集与常规方法进行了对比,以评估最佳层析成像方法。无线电探空仪和COSMIC派生的水蒸气密度被用作评估层析成像结果的参考。使用无线电探空仪产品作为参考,通过我们的优化方法获得的测试结果表明,与传统方法在3.75 km高度以下和在3.75 km高度以上的常规方法相比,水蒸气密度精度分别提高了15%和12%。用COSMIC产品作为参考,结果表明在低于3.75 km和高于3.75 km的情况下,水蒸气密度的准确度分别提高了15%和19%。

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