Fu Xinshu, Tan Jianguo. Quality control of temperature and humidity profile retrievals from ground-based microwave radiometer. J Appl Meteor Sci, 2017, 28(2): 209-217. DOI:  10.11898/1001-7313.20170208.
Citation: Fu Xinshu, Tan Jianguo. Quality control of temperature and humidity profile retrievals from ground-based microwave radiometer. J Appl Meteor Sci, 2017, 28(2): 209-217. DOI:  10.11898/1001-7313.20170208.

Quality Control of Temperature and Humidity Profile Retrievals from Ground-based Microwave Radiometer

DOI: 10.11898/1001-7313.20170208
  • Received Date: 2016-10-10
  • Rev Recd Date: 2017-01-17
  • Publish Date: 2017-03-31
  • Ground-based microwave radiometer profiler (MWR) can continuously retrieve thermodynamic profiles of the atmosphere on a minute time scale. These profiles are important supplements to radiosonde observations. Since the presence of liquid water on the profiling radiometer, radio frequency interference and other events can cause errors, quality control procedures that can detect data-quality problems are of critical importance. QC procedures are proposed for ground-based MWR-retrieved atmospheric profiles of temperature and humidity using 10-year radiosonde soundings (January 2004 to December 2014) at Baoshan Station in Shanghai and observations from MP-3000A MWR (January 2012 to May 2014) at Shanghai Expo Station. QC procedures include three types of checks:Climatological test, time consistency test, and vertical consistency test. Climatological check aims to verify if the values of instantaneous data are within climatology range limits. Thresholds are set based on the seasonally varying statistics of 10-year radiosonde soundings. The time consistency check focus on the change rate of instantaneous data. If the difference between the current instantaneous value with the previous one exceeds a specific limit, the current value will be flagged as doubtful. The test is applied level by level, and the profile with suspected data at more than one level is flagged as doubtful. Vertical consistency checks operate on dTh and contain two tests: A test for the plausible value check of dThand a test for the standard deviation of dTh (σ (dTh)). dTh (unti:℃· (100 m)-1) is defined as the ratio of temperature difference to height difference at consecutive levels. The plausible value check of dTh is proposed to verify if there are spikes in a profile. The test for (σ (dTh)) is used to sort profiles with excessive level-to-level fluctuations throughout a sounding. Results show that QC methods can effectively identify various suspected observations, such as climatological outliers, temporal inconsistency and excessive vertical fluctuations in profiles. The frequency of suspected temperature and humidity profiles detected in rainy days is much higher than that in other weather conditions. The accuracy of MWR retrieved temperature and vapor density profiles is improved after applying these QC procedures. Correlation coefficients of both temperature and humidity observations between the MWR and radiosonde increase and corresponding root mean square error (RMSE) decrease after QC, especially those in rainy days. QC procedures for MWR-retrieved thermodynamic profiles are also proposed, through which various suspected profiles can be flagged. The accuracy of MWR retrievals is improved significantly after applying QC procedures.
  • Fig. 1  Minutely variations of air temperature from microwave radiometer at 50 m height from Jan 2012 to May 2014

    Fig. 2  Minutely variations of water vapor density from microwave radiometer at 50 m height from Jan 2012 to May 2014

    Fig. 3  Example of a suspected profile with excessive level-to-level fluctuations at 0601 BT 8 Oct 2013

    (a) temperature, (b) corresponding temperature differences between vertical adjacent levels

    Fig. 4  Probability distribution of standard deviation of temperature differences between consecutive levels

    Fig. 5  The correlation coefficient and root mean square error of temperature profiles between the microwave radiometer and radiosonde from Jan 2012 to Dec 2013 before and after quality control

    Fig. 6  The correlation coefficient and root mean square error of vapor density profiles between the microwave radiometer and radiosonde from Jan 2012 to Dec 2013 before and after quality control

    Table  1  Number of suspected temperature and vapor density profiles flagged by quality control in different weather conditions

    质量控制方法 温度疑误廓线样本量 湿度疑误廓线样本量
    降水天气 有云天气 晴空天气 降水天气 有云天气 晴空天气
    极值检查 32131 8332 6470 73528 1488 168
    时间一致性检查 9806 4043 2318 27873 12491 3569
    温度垂直变化率的极值检查 38733 149 170
    温度垂直变化率的标准差检查 52090 3232 3822
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    • Received : 2016-10-10
    • Accepted : 2017-01-17
    • Published : 2017-03-31

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