An Intruduction of WMO 8th Radiosondes Intercomparison and Integrated Remote Instruments Experiment
Received date: 2011-12-19
Revised date: 2012-05-31
Online published: 2012-08-10
WMO 8th international radiosondes inter-comparison and integrated remote instruments experiment provide abundant high quality data, which help to analyze the capability of radiosondes, and evaluate infrared-radiation impact on temperature sensor and humidity sensor bias. By this experimentation, the advantages and disadvantages of China-made X-band polarize radar and Ka-band cloud radar and laser radar, MPL, Ceilometer etc. are evaluated. Some studies were devoted to improve the key algorithms such as microwave radiometer temperature and humidity measurement, the X-band and Ka-band radars echo attenuation correction, Doppler wind field inversion,cloud classification and upper air wind measurement. Furthermore, the local clouds,tropical convective system and sea-land wind systems are detected by using the remote instruments and the results are delighting. Similarly, this experiment also provides a good case for researching how to organize preferably integrated remote instruments observation test for the future.
Key words: WMO; Radiosondes inter-comparison; Remote experiment
Li Feng
,
Li Bai
,
Wu Lei
,
Yang Rongkang
,
Xing Yi
,
Huang Xingyou
,
Xiao Hui
,
Wang Bin
.
An Intruduction of WMO 8th Radiosondes Intercomparison and Integrated Remote Instruments Experiment[J]. Advances in Earth Science, 2012
, 27(8)
: 916
-924
.
DOI: 10.11867/j.issn.1001-8166.2012.08.0916
[1]Ivanov A,Kats A,Kumosen Kos,et al. WMO International Radiosonde IntereomParison Phasem(Dzhambul, USSR,1989 ) Final Report[R]. WMO/TD No.451, Instruments and Observing Methods Report No.40. Geneva:WMO,1991.
[2]Yagi S,Mita A,Xnoue N. WMO International Radiosondes Inter-Comparison Phase Vl(Tsukuba, Japan,1993) Final Report[R]. WMO/TD No .742,Instruments and Observing Methods Report No.59.Geneva:WMO,1996.
[3]Da Silveira, Fiseh R G, Maehadol, et al. WMO Inter-comParison of GPS Radiosondes, Aleantara,Brazil,2001[R].WMO/ TD No.1314,Instruments and Observing Methods Report No. 90. Geneva:WMO, 2006.
[4]Nash J, Smout R, Oakley T, et al. WMO Intercomparison of High Quality Radiosonde Systems Final Report (Vaeao S,Mauritius,2005)[R].Geneva:WMO,2006.
[5]Li Wei,Zhao Peitao, Guo Qiyun, et al. The results of China-made radiosonde intercompared with high quality radiosonde systems[J].Journal of Applied Meteorology,2011,2(4):453-462.[李伟,赵培涛,郭启云,等. 国产GPS 探空仪国际比对试验结果[J].应用气象学报, 2011, 2(4):453-462.]
[6]Nash J, Oakley T,Vmel H,et al. WMO Intercomparison of High Quality Radiosonde Systems[R].Yangjiang, China,12 July-3 August 2010, Instruments and Observing Methods RePort No. 107:66-179. Geneva:WMO,2011.
[7]Meteorological Observation Center, CMA. The Collection of the Theses for Research on WMO 8th Intercomparison of High Quality Radiosonde Systems[C].Beijing,2011:216.[中国气象局气象探测中心.WMO 8th 阳江国际探空比对成果交流会文集[C].北京,2011:216.]
[8]Poore K D, Wang J, Rossow W B. Cloud layer thickness from a combination of surface and upper-air observations[J]. Journal of Climate, 1995,8:550-568.
[9]Keenan T. Hydrometeor classification with a C-band polarimetric radar[J]. Australian Meteorological Magazine, 2003,52:23-31.
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