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首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Accurate Estimation of Atmospheric Water Vapor Using GNSS Observations and Surface Meteorological Data
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Accurate Estimation of Atmospheric Water Vapor Using GNSS Observations and Surface Meteorological Data

机译:利用GNSS观测值和地面气象数据准确估算大气水汽

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摘要

Remote sensing data have been increasingly used to measure the content of water vapor in the atmosphere and to characterize its temporal and spatial variations. In this paper, we use observations from Global Navigation Satellite System(s) (GNSS) to estimate time series of precipitable water vapor (PWV) by applying the technique of precise point positioning. For an accurate quantification of the absolute PWV, it is necessary to combine the GNSS observations with meteorological data measured directly or inferred at the GNSS site. In addition, measurements of the surface temperature are used to calculate the empirical constant required to convert the GNSS-based delay into water vapor. Our results show strong agreement between the total precipitable water estimated based on GNSS observations and that measured by the sensor MEdium Resolution Imaging Spectrometer with a mean RMS value of 0.98 mm. In a similar way, we compared the GNSS-based total PWV estimates with those produced by the Weather Research and Forecasting (WRF) Modeling System. We found that the WRF model simulations agree well with the GNSS estimates with a mean RMS value of 0.97 mm.
机译:遥感数据已越来越多地用于测量大气中水蒸气的含量并表征其时间和空间变化。在本文中,我们使用来自全球导航卫星系统(GNSS)的观测值,通过应用精确点定位技术来估算可沉淀水汽(PWV)的时间序列。为了精确定量绝对PWV,有必要将GNSS观测结果与直接测量或在GNSS站点推断出的气象数据结合起来。另外,表面温度的测量值用于计算将基于GNSS的延迟转换为水蒸气所需的经验常数。我们的结果表明,基于GNSS观测值估算的总可沉淀水与由传感器平均分辨率成像光谱仪(平均RMS值为0.98 mm)测量的总可沉淀水之间存在强烈的一致性。以类似的方式,我们将基于GNSS的总PWV估算值与由天气研究和预报(WRF)建模系统得出的估算值进行了比较。我们发现,WRF模型模拟与GNSS估计值非常吻合,均方根值为0.97 mm。

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