Zhong Jiqin, Chen Min, Fan Shuiyong, et al. Assimilation application of AMDAR data to the operational NWP system of Beijing. J Appl Meteor Sci, 2010, 21(1): 19-28.
Citation: Zhong Jiqin, Chen Min, Fan Shuiyong, et al. Assimilation application of AMDAR data to the operational NWP system of Beijing. J Appl Meteor Sci, 2010, 21(1): 19-28.

Assimilation Application of AMDAR Data to the Operational NWP System of Beijing

  • Received Date: 2008-11-07
  • Rev Recd Date: 2009-11-05
  • Publish Date: 2010-02-28
  • AMDAR data has been widely proved valuable in improving accuracy of numerical weather forecast. But assimilation application of AMDAR data in operational NWP model is seldom accessed in China. BJ RUC, the operational rapid update and cycling NWP system of Beijing Meteorological Bureau, is used to evaluate the impacts of assimilating AMDAR data on forecast performance. Durative experiments with and without AMDAR data are conducted from 15 Jul to 15 Aug, 2007. The average RMSE difference and average precipitation scores difference of AMDAR and NOAMDAR experiments are compared to discuss the impacts of AMDAR on short range numerical weather forecast.Analysis shows that the assimilation of aircraft data has remarkable positive impacts on the first 9 hours forecast especially on upper levels. Forecasts of wind on the levels of 925 hPa to 250 hPa and temperature on the levels of 850 hPa to 400 hPa are improved. The assimilation of AMDAR data contributes more in rapid updated cycle mode than in cold start mode. It has positive impacts on the threshold score of accumulated precipitation forecast of 0—12 hours, 0—24 hours, 12—18 hours, and 18—24 hours. It also improves the overestimating in the NOAMDAR experiments. The increment analysis shows parallel characteristics with the horizontal distribution of AMDAR data and the vertical improvement characteristic of the 3 hours forecast. The comparability indicates the improvement of wind and temperature in first guess field made by assimilating AMDAR data. The relative observation errors of AMDAR against Beijing radiosonde are discussed and proved reliable. It suggests that determining AMDAR observation errors properly in assimilation can help make better use of AMDAR data.Experiments on AMDAR data assimilating application in the operational BJ RUC system show that AMDAR assimilating has important positive impacts on improving the upper temperature, wind and precipitation forecast. Reasonable amendment of observation errors will bring more efficient utilization of AMDAR data, so priority is assigned to adjusting the AMDAR observation errors in BJ RUC.
  • Fig. 1  AMDAR distribution from 15 July to 15 August 2007

    (a) AMDAR spatial distribution in domain of 27 km resolution at 12:00 15 Jul 2007, (b) averaged vertical distribution of AMDAR data in D3, (c) averagedtemporal distribution of AMDAR data in domain of D3

    Fig. 2  Vertical profiles of averaged root mean square error of 3, 6, 9-hour valid wind and tempe rature fo recast against 54511 RAOB o bserv ation from 15 Jul to 15 Aug 2007

    Fig. 3  Vertical profile of averaged root mean square error of wind (a, c) and temper ature (b, d)6-hour valid forecast within the duration of 15 Jul to 15 Aug 2007 under cold start mode (a, b) and warm start mode (c, d) respectively

    Fig. 4  Thresh score of 24-hour, 12-hour and 6-hour accumulated precipitation

    Fig. 5  Cross-section at 40°N and horizontal distribution of analysis increment of AMDAR obser vationin D3

    Fig. 6  Root mean square error of AMDAR obser vation relative to the radiosonde observ ationin Beijing

    Table  1  Input and assimilated AMDAR report of different time on 1 Aug 2007 in D2 and D3

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    • Received : 2008-11-07
    • Accepted : 2009-11-05
    • Published : 2010-02-28

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