不同陆面模式亮温模拟与FY-4A/AGRI观测对比

Comparison of Brightness Temperature Simulations Under Different Land Surface Models with FY-4A/AGRI Measurements

  • 摘要: 基于WRF模式耦合的3个陆面模式(CLM4、RUC和Noah-MP)提供的地表温度(Ts)预测值,使用CRTM辐射传输模式对2022年4个典型月份(1月、4月、7月和10月)我国东部地区开展FY-4A/AGRI地表敏感通道(通道 11~13)亮温模拟试验,旨在评估基于模式不同陆面过程的亮温模拟表现。结果表明:采用Noah-MP时亮温模拟效果最佳,陆面模式对Ts预报的性能差异是导致AGRI亮温模拟日变化特征不同的重要原因之一,陆面模式模拟Ts的差异主要来源于地表吸收太阳辐射、地表感热和潜热通量及土壤热容量的差异。考虑地表发射率对模拟亮温的影响,对比采用不同地表发射率数据集时3个陆面模式的亮温模拟效果,发现不同发射率数据导致的亮温模拟差异小于不同陆面模式间差异,并通过相对敏感性分析揭示Ts是影响东部地区AGRI地表敏感通道亮温模拟的重要因素。

     

    Abstract: Recognized as part of China’s new generation of geostationary meteorological satellites, FY-4A/B is equipped with an advanced geostationary radiative imager (AGRI). The instrument provides high-resolution satellite measurements in near real-time for the Eastern Hemisphere. Before applying satellite data for atmospheric parameter retrieval or assimilation, it is essential to conduct a quantitative analysis of data biases. A quantitative assessment of simulated brightness temperature is offered for the surface-sensitive channels of FY-4A/AGRI, to improve the utilization of FY-4A/AGRI measurements over land in assimilation processes. The CRTM radiative transfer model, alongside land surface temperature (Ts) data from 3 land surface models (CLM4, RUC, Noah-MP) are employed, and monthly surface emissivity data are utilized to simulate brightness temperatures for 4 representative months: January, April, July, and October of 2022 over the eastern China. The research focuses on analyzing the spatial, diurnal, and surface-related variations in brightness temperature bias. Initially, the simulation performance in July is particularly superior, especially in the northern region of the eastern China. And the experiment utilizing Noah-MP model consistently provides the best and the most stable results. Secondly, results of the experiment utilizing Noah-MP model produces the most accuate simulations throughout most of 24 h cycle which is attributed to discrepancies in Ts accuracy. Further diagnostics indicate these differences in Ts simulations largely arise from variations in surface absorption of solar radiation, surface latent heat flux, surface sensible heat flux, and soil heat capacity. Additionally, considering the potential impact of land surface emissivity on simulated brightness temperatures, an analysis is conducted using 3 land surface models under varying land surface emissivity schemes. Results indicate that the simulations conducted under various land surface emissivity schemes are nearly identical. Through an analysis of relative sensitivity, it is revealed that land surface temperature is a significant factor influencing simulated brightness temperatures in AGRI surface-sensitive channels over the eastern China. Lastly, acknowledging the superior accuracy of experiment using Noah-MP model, the study statistically analyzes the brightness temperature biases and standard deviations of AGRI surface-sensitive channels across 5 typical surface types in the eastern China as a reference for quantifying errors and correcting biases in the assimilation of satellite data.

     

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