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Optimization of GPS water vapor tomography technique with radiosonde and COSMIC historical data

机译:利用探空仪和COSMIC历史数据优化GPS水蒸气层析成像技术

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The near-real-time high spatial resolution of atmospheric water vapor distribution is vital in numerical weather prediction. GPS tomography technique has been proved effectively for three-dimensional water vapor reconstruction. In this study, the tomography processing is optimized in a few aspects by the aid of radiosonde and COSMIC historical data. Firstly, regional tropospheric zenith hydrostatic delay??(ZHD) models are improved and thus the zenith wet delay??(ZWD) can be obtained at a higher accuracy. Secondly, the regional conversion factor of converting the ZWD to the precipitable water vapor??(PWV) is refined. Next, we develop a new method for dividing the tomography grid with an uneven voxel height and a varied water vapor layer top. Finally, we propose a Gaussian exponential vertical interpolation method which can better reflect the vertical variation characteristic of water vapor. GPS datasets collected in Hong Kong in February 2014 are employed to evaluate the optimized tomographic method by contrast with the conventional method. The radiosonde-derived and COSMIC-derived water vapor densities are utilized as references to evaluate the tomographic results. Using radiosonde products as references, the test results obtained from our optimized method indicate that the water vapor density accuracy is improved by 15 and 12a?ˉ% compared to those derived from the conventional method below the height of 3.75a?ˉkm and above the height of 3.75a?ˉkm, respectively. Using the COSMIC products as references, the results indicate that the water vapor density accuracy is improved by 15 and 19a?ˉ% below 3.75a?ˉkm and above 3.75a?ˉkm, 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汽重建。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,改进了对流层天顶静水滞后Δθ(ZHD)模型,从而可以更高的精度获得天顶湿滞后Δθ(ZWD)。其次,细化了将ZWD转换成可沉淀水蒸气Δθ(PWV)的区域转换因子。接下来,我们开发了一种新的方法来分割具有不均匀体素高度和变化的水蒸气层顶部的层析成像网格。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。与传统方法相比,2014年2月在香港收集的GPS数据集用于评估优化的层析成像方法。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3.75a ?? km以下和更高高度处获得的水蒸气密度精度相比,水蒸气密度精度分别提高了15和12a?%%。分别为3.75a?ˉkm。使用COSMIC产品作为参考,结果表明在低于3.75a?km时和高于3.75a?km时,水蒸气密度精度分别提高了15和19a?%。

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