Meng Chunlei, Li Huoqing
Institute of Urban Meteorology, China Meteorological Administration, 100089, Beijing, China.
Institute of Desert Meteorology, China Meteorological Administration, 830002, Urumqi, Xinjiang, China.
Sci Rep. 2019 Dec 20;9(1):19567. doi: 10.1038/s41598-019-55733-3.
Fengyun-4A is the new generation of Chinese geostationary meteorological satellites. Land surface albedo, land surface emissivity and land surface temperature are key states for land surface modelling. In this paper, the land surface albedo, land surface emissivity and land surface temperature data from Fengyun-4A were assimilated into the Integrated Urban land Model. The Fengyun-4A data are one of the data sources for the land data assimilation system which devoted to produce the high spatial and temporal resolution, multiple parameters near real-time land data sets. The Moderate-Resolution Imaging Spectroradiometer (MODIS) LSA and LSE data, the Institute of Atmospheric Physics, China Academy of Sciences (IAP) 325 m tower observation data and the observed 5 cm and 10 cm soil temperature data in more than 100 sites are used for validation. The results indicate the MODIS land surface albedo is much smaller than the Fengyun-4A and is superior to the Fengyun-4A for the Institute of Atmospheric Physics, China Academy of Sciences 325 m tower site. The Moderate-Resolution Imaging Spectroradiometer land surface emissivity is smaller than the Fengyun-4A in barren land surface and the differences is relatively small for other land use and land cover categories. In most regions of the research area, the Fengyun-4A land surface albedo and land surface emissivity are larger than those of the simulations. After the land surface albedo assimilation, in most regions the simulated net radiation was decreased. After the land surface emissivity assimilation, in most regions the simulated net radiation was increased. After the land surface temperature assimilation, the biases of the land surface temperature were decreased apparently; the biases of the daily average 5 cm and 10 cm soil temperature were decreased.
风云四号A星是中国新一代静止气象卫星。陆地表面反照率、陆地表面发射率和陆地表面温度是陆地表面建模的关键状态。本文将风云四号A星的陆地表面反照率、陆地表面发射率和陆地表面温度数据同化到综合城市土地模型中。风云四号A星数据是致力于生成高时空分辨率、多参数近实时陆地数据集的陆地数据同化系统的数据源之一。利用中分辨率成像光谱仪(MODIS)的陆地表面反照率(LSA)和陆地表面发射率(LSE)数据、中国科学院大气物理研究所(IAP)325米高塔观测数据以及100多个站点观测的5厘米和10厘米土壤温度数据进行验证。结果表明,MODIS陆地表面反照率比风云四号A星小得多,在中国科学院大气物理研究所325米高塔站点处优于风云四号A星。中分辨率成像光谱仪陆地表面发射率在裸土地表面比风云四号A星小,在其他土地利用和土地覆盖类型中差异相对较小。在研究区域的大部分地区,风云四号A星陆地表面反照率和陆地表面发射率比模拟值大。陆地表面反照率同化后,大部分地区模拟的净辐射减少。陆地表面发射率同化后,大部分地区模拟的净辐射增加。陆地表面温度同化后,陆地表面温度偏差明显减小;5厘米和10厘米土壤日均温度偏差减小。