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Comparison of Integrated Precipitable Water Derived from Cosmic Occultation Data and Ground GPS Measurements

机译:来自宇宙掩星数据和地面GPS测量的综合可沉淀水的比较

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The integrated Precipitable Water (PW) derived from ground IGS stations is considered as reference because of its high accuracy and long-term stability to validate the PW derived from COSMIC RO sounding data. The one-year comparisons show that both PW are quite consistent for PW below 20 mm, and the PW derived from COSMIC has systemic low bias than ground-GPS PW for PW >40 mm. In general, the rms of PW difference between COSMIC and IGS is about 1.5-3.0mm, and the mean difference is less than 0.5mm, which is acceptable. In addition, the variations of PW difference in the southern hemisphere are obviously fluctuant due to fewer IGS stations over this region, while the mean PW difference is more stable and smaller around 0.5 mm for latitude higher than 25°N and the standard deviation of PW difference is gradually decreases with higher latitude in the northern hemisphere.
机译:来自地面IGS站的综合可沉淀水(PW)被认为是参考,因为它具有很高的准确性和长期稳定性,可验证从COSMIC RO测深数据得出的PW。一年的比较表明,对于20 mm以下的PW,两个PW都非常一致,并且对于大于40 mm的PW,从COSMIC衍生的PW具有比地面GPS PW更低的系统性偏差。通常,COSMIC和IGS之间的PW差的均方根值约为1.5-3.0mm,平均差小于0.5mm,这是可以接受的。此外,由于该地区IGS台数减少,南半球的PW差异变化明显波动,而对于高于25°N的纬度和PW的标准偏差,平均PW差异更稳定且更小,约为0.5 mm。随着北半球纬度的提高,差异逐渐减小。

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