Assimilation of global positioning system radio occultation observations into NCEP's global data assimilation system

被引:104
|
作者
Cucurull, L.
Derber, J. C.
Treadon, R.
Purser, R. J.
机构
[1] NASA, NOAA, DOD Joint Ctr Satellite Data Assimilat, Washington, DC 20546 USA
[2] Univ Corp Atmospher Res, Boulder, CO USA
[3] Natl Ctr Environm Predict Environm Modeling Ctr, Washington, DC USA
[4] Sci Applicat Int Corp, Beltsville, MD USA
关键词
D O I
10.1175/MWR3461.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) mission launched six small satellites in April 2006, each carrying a GPS radio occultation (RO) receiver. At final orbit, COSMIC will provide similar to 2500-3000 RO soundings per day uniformly distributed around the globe in near-real time. In preparation for the assimilation of COSMIC data in an operational framework, the NCEP/Environmental Modeling Center (EMC) has successfully developed the capability of assimilating profiles of refractivity and bending angle. Each forward operator has been implemented with its own quality control and error characterization. In this paper, the infrastructure developed at NCEP/EMC to assimilate GPS RO observations, including forward models, observational and representativeness errors, and quality control procedures, is described. The advantages of using a forward operator for bending angle versus refractivity are discussed and some preliminary results on the benefits of the GPS RO in weather analysis and forecasts are presented. The different strategies adopted at NCEP/EMC to assimilate GPS RO data are aimed to select the most appropriate forward operator in the operational data assimilation system when COSMIC products are stable and routinely available to the Numerical Weather Centers. In the meantime, data from the Challenging Minisatellite Payload (CHAMP) satellite is available in non-real time and has been used in the assimilation tests to examine the potential benefits of the GPS RO-derived products. In the preliminary results presented in this study, the use of GPS RO observations slightly improves anomaly correlation scores for temperature (by similar to 0.01-0.03) in the Southern Hemisphere and Tropics throughout the depth of the atmosphere while a slight degradation is found in the upper troposphere and stratosphere in the Northern Hemisphere. However, significant reduction of the temperature and humidity biases is found for all latitudes. The benefits from assimilating GPS RO data also extend to other fields, such as 500-hPa geopotential heights and tropical winds, demonstrating the potential use of GPS RO data in operational forecasting.
引用
收藏
页码:3174 / 3193
页数:20
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