地表高度检测阈值对青藏高原微波湿度计资料同化影响

Influence of Surface Height Detection Threshold on the Assimilation of Microwave Hygrometer Data over the Tibetan Plateau

  • 摘要: 为了改善风云三号微波湿度计观测资料在青藏高原东侧复杂地形区域数值模式中的同化应用效果,提高数值模式相对湿度初始场及预报质量,本文基于WRFDA同化模块,针对我国风云三号D星(FY-3D)微波湿度计(MWHS-2)观测资料,进行地表高度检测的敏感性试验,将卫星资料同化的地表高度检测阈值由800~1500 m改为2000~4000 m,以保留更多MWHS-2数据,并评估MWHS-2观测资料在青藏高原区域模式同化的适用性。结果表明:采用新地表高度阈值方案后,青藏高原区域内进入同化的MWHS-2数据量较原方案增加2~3倍;基于三维变分同化方法(3DVar)同化MWHS-2观测资料能有效减少初始场偏差,使初始场模拟的亮温更趋近于观测;MWHS-2观测资料同化后青藏高原北部青海、新疆南部地区初始场湿度均有调整,卫星观测资料能为青藏高原常规站点稀疏地区起到观测补充;采用新方案后,同化MWHS-2观测资料减小了对流层中低层(400 hPa以下)相对湿度的预报偏差;随着预报时效的延长,采用4000 m高度阈值方案的资料同化方案预报效果更好。

     

    Abstract: In order to improve the assimilation effect of Fengyun-3 (FY-3) Microwave Humidity Sounder-2 (MWHS-2) data in numerical models over the complex terrain region of the eastern Tibetan Plateau and enhance the initial humidity field and the forecast accuracy, this study conducts sensitivity experiments on surface height detection thresholds using the Weather Research and Forecasting Data Assimilation (WRFDA) assimilation system. The original surface height detection threshold (800–1500 m) for satellite data assimilation was adjusted to 2000–4000 m to retain more MWHS-2 observations. The applicability of MWHS-2 data assimilation over the Tibetan Plateau was then evaluated. The results show that the number of assimilated MWHS-2 observations over the Tibetan Plateau increased by 2–3 times compared with the original scheme after adopting the new surface height threshold. The assimilation of MWHS-2 observations based on Three-Dimensional Variational Assimilation (3Dvar) effectively reduced the bias of initial field, making the simulated brightness temperature closer to observations. The assimilation of MWHS-2 observations adjusted the initial humidity fields in Qinghai and southern Xinjiang in the northern Tibetan Plateau, and the satellite observation data served as a supplementary observation for sparse conventional stations in the Tibetan Plateau. The new scheme reduced relative humidity forecast biases in the mid-to-lower troposphere (below 400 hPa). With the extension of the forecasting time, the data assimilation scheme with a 4000m height threshold exhibited superior performance.

     

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