Xue Chenbin, Gong Jiandong, He Caifu, et al. Quality control of cloud derived wind vectors from geostationary meteorological satellites with its application to data assimilation system. J Appl Meteor Sci, 2013, 24(3): 356-364.
Citation: Xue Chenbin, Gong Jiandong, He Caifu, et al. Quality control of cloud derived wind vectors from geostationary meteorological satellites with its application to data assimilation system. J Appl Meteor Sci, 2013, 24(3): 356-364.

Quality Control of Cloud Derived Wind Vectors from Geostationary Meteorological Satellites with Its Application to Data Assimilation System

  • Received Date: 2012-09-13
  • Rev Recd Date: 2013-03-05
  • Publish Date: 2013-06-30
  • Cloud derived wind vectors can provide plenty of useful information for synoptic analysis and numerical weather prediction, because of their excellent spatial and temporal coverages. It is of great value to apply cloud derived wind vectors efficiently with the purpose of improving the initial fields and numerical forecasts. The quality control of cloud derived wind vectors from geostationary meteorological satellites has been one of the important and difficult problems to be solved in satellite data assimilation. It has a direct impact on the prediction level of numerical weather prediction model. On the basis of the statistical analysis of global cloud derived wind vectors for 14 months, the quality indicator threshold of the five channels of cloud derived wind vectors in tropics, north and south hemisphere extra-tropics in high, middle and low levels from five global geostationary meteorological satellites in business operation, is analyzed and calculated. The error characteristics of infrared, water vapor and visible channels in the space area of cloud derived wind vectors are investigated, and the corresponding QI thresholds are determined. On the basis of quality control and equal-distance thinning scheme, the vertical distribution characteristics of cloud derived wind vectors are analyzed. It shows that after quality control, the number of infrared channel accounts for the vast majority, water vapor channel follows, and visible light channel the least.Furthermore, the method of innovation vector and zero-order Bessel fitting function which is based on the theory of least square method are adopted together to partition background and observation error variances in the observation space, and thus estimate the observation error of cloud derived wind vectors and the quality control coefficient according to the statistical distribution of the innovation vectors. On this basis, in order to validate the assumption on uncorrelated observation errors required in three-dimensional variational method, observation errors are inflated to avoid the influence carried by correlated errors.Finally, three numerical simulation schemes are designed and the forecast improvement and impact of cloud derived wind vectors before and after quality control are analyzed. Results show that the cloud derived wind vectors after quality control can effectively reduce the error of analysis field at high level. And the global short-term and medium-term forecast ability can be improved obviously by assimilating cloud derived wind vectors after quality control. In particular, there is a clear improvement in forecast ability in terms of wind, geopotential height and temperature fields in tropics. The forecast improvement above high levels appears better than those of middle and low levels in northern and southern hemisphere extra-tropics.
  • Fig. 1  The mean and standard deviation for the u-component speed bias of MTSAT-2R cloud derived wind vectors against radiosonde observations in the Northern Hemisphere extra-tropics

    Fig. 2  Vertical distribution profile for the number of cloud derived wind vectors

    (a) before quality control, (b) after quality control

    Fig. 3  Vertical distribution for the u-component speed bias of analysis wind field against radiosonde observations

    Fig. 4  The same as in Fig. 2, but for standard bias

    Fig. 5  Improvement rate of forecast experiments

    Table  1  QI thresholds for cloud derived wind vectors (unit:%)

    卫星 通道 高层 中层 低层
    NH TR SH NH TR SH NH TR SH
    GOES-11 IR 50 70 50 60 50
    VIS
    WV3
    WV5 90 50 50 85 75
    WV7
    GOES-13 IR 50 50 50 70
    VIS 95 95
    WV3
    WV5 50 50 96
    WV7
    NETEOSAT-9 IR 95 79 98 96 78 91 81
    VIS
    WV3 96 80 98 98 84
    WV5 79 82 86 85 86 92 95 96
    WV7
    FY-2E IR 94 94 94 96
    VIS
    WV3
    WV5
    WV7 89 92 93 95
    MTSAT-2R IR 94 75 95 96 85 85 84 85
    VIS 85 75 84
    WV3 94 80 93
    WV5 94 84
    WV7
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    Table  2  Observation errors of cloud derived wind vectors at each level

    层次/hPa 云导风高度范围/hPa 观测误差均方差/(m·s-1)
    1000 (925, 1000] 4.6
    850 (775, 925] 5.4
    700 (600, 775] 6.2
    500 (450, 600] 6.8
    400 (350, 450] 7.2
    300 (275, 350] 7.8
    250 (225, 275] 6.3
    200 (175, 225] 6.6
    150 (125, 175] 7.3
    100 [75, 125] 6.6
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    • Received : 2012-09-13
    • Accepted : 2013-03-05
    • Published : 2013-06-30

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