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Homogenizing surface pressure time-series from operational numerical weather prediction models for geodetic applications

机译:均质化表面压力时间序列来自地理位置应用的操作数值天气预报模型

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Global surface pressure grids from 14.5 years of 6-hourly analyses out of both the operational ECMWF weather prediction model and ERA-Interim are mapped to a common reference orography by means of ECMWF’s mean sea-level pressure diagnostic. The approach reduces both relative biases and residual variability by about one order of magnitude and thereby achieves a consistency among both data sets at the level of about 1 hPa. Remaining differences rather reflect temperature biases and also resolution limitations of the reanalysis data set, but are not anymore related to the local roughness in orography or to changes in the spatial resolution of the operational model. The presented reduction method therefore allows to obtain surface pressure time series with the long-time consistency of a reanalysis from an operational numerical weather model with much higher resolution and much shorter latency, making the results suitable for geodetic near realtime applications requiring continuously updated time series that are homogeneous over many years.
机译:通过ECMWF的平均海平压力诊断,全局表面压力网14.5年6小时分析出来的操作ECMWF天气预报模型和ERA临时分析。该方法通过大约一个级别来降低相对偏置和残差变化,从而在大约1 HPA的水平下实现两个数据集之间的一致性。剩余的差异相当反映了再分析数据集的温度偏差以及分辨率限制,但不再与局部粗糙度或操作模型的空间分辨率变化有关。因此,所提出的还原方法允许从具有高得多的分辨率和更短的延迟的操作数值天气模型中获得表面压力时间序列,其具有更高的分辨率和更短的延迟,这使得适用于需要连续更新时间序列的实时应用附近的大地测量仪的结果多年来是同质的。

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