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WRF模式气象数据在遥感反演PM_(2.5)中的应用研究 被引量:2

Application of WRF Model Meteorological Data in PM_(2.5) Remote Sensing Inversion
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摘要 利用MODIS气溶胶光学厚度产品AOD,结合地面台站气象观测数据和WRF模式气象模拟数据,对徐州环境监测国控级别站点的近地面PM_(2.5)质量浓度进行反演。根据不同气象要素在反演过程中的相关程度,对气象观测数据和WRF模拟数据在遥感反演中的效果进行分析评估。结果表明,气象观测值和WRF模拟气象数据均能有效应用于PM_(2.5)的遥感反演,在气象观测数据时空覆盖度较低的情况下,能够使用WRF模拟数据进行有效替代,为不同来源的气象数据对PM_(2.5)反演应用研究提供依据和参考。 Based on MODIS aerosol optical depth product, combined with meteorological observation data of ground stations and WRF model meteorological data, the PM_(2.5) mass concentration of Xuzhou environmental monitoring station was reconstructed in this paper. And according to the correlation degree of different meteorological elements in the inversion process, the effects of meteorological observation data and WRF simulation data in remote sensing inversion were analyzed and evaluated. The results show that the meteorological observation and WRF simulation data can be effectively applied to the remote sensing inversion of PM_(2.5), and under the objective condition of low coverage of meteorological observation data, it can be replaced by WRF simulation data. This study provides the basis and reference for the application of PM_(2.5) inversion from different sources of meteorological data.
出处 《地理空间信息》 2018年第2期45-47,共3页 Geospatial Information
基金 国家自然科学基金资助项目(41271116) 国家高新技术研究与发展计划资助项目(2013AA122002)
关键词 PM2.5 气溶胶光学厚度 WRF模式 气象要素 PM2.5 aerosol optical depth WRF model meteorological element
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  • 1牛生杰,孙照渤.春末中国西北沙漠地区沙尘气溶胶物理特性的飞机观测[J].高原气象,2005,24(4):604-610. 被引量:38
  • 2黄艇,陈长和,陈勇航,张武,张镭.利用MODIS卫星资料对比反演兰州地区气溶胶光学厚度[J].高原气象,2006,25(5):886-892. 被引量:19
  • 3Aekerman T P, Toon O B. Absorption of visible radiation in atmosphere containing mixtures of absorbing and nonabsorbing particles[J]. ApplOpt, 1981, 20(20): 3661-3667.
  • 4Charlson R J, Schwartz S E, Hales J M, et al. Climate Forcing by Anthropogenic Aerosols [J]. Science, 1992, 255 (5043):423-430.
  • 5IPCC. Climate Change 2007: The Physical Science Basis. Working Group I Contribution to the Intergovernmental Panel on Climate Change Fourth Assessment Report[R]//Solomon S, Qing D H, Manning M, et al. eds. Contribution of Working Group to the Fourth Assessment Report of the Intergovermental Pand on Climate change. Cambridge: Cambridge Univ. Press, 2007: 996.
  • 6Huang J, Minnis P, Chen B, et al. Long-range transport and vertical structure of Asian dust from CALIPSO and surface measurements during PACDEX [J]. J Geophys Res, 2008, 113, D23212, doi:10. 1029/2008JD010620.
  • 7Huang J, Fu Q, Su J, et al. Taklimakan dust aerosol radiative heating derived from CALIPSO observations using the Fu-Liou radiation model with CERES constraints [J]. Atmos Chem Phys, 2009, 9(12): 4011-4021.
  • 8Ramanathan V, Crutzen P J, Kiehl J T, et al. Aerosols, Climate, and the Hydrological Cycle [J]. Science, 2001, 294 (5549): 2119-2124.
  • 9Yang X, Wenig M. Study of columnar aerosol size distribution in HongKong[J]. Atmos Chem Phys, 2009, 9( 16): 6175-6189.
  • 10Lee K, Li Z, Wong M, et al. Aerosol single scattering albedo estimated aeross China from a combination of ground and satellite measurements[J]. J Geophys Res, 2007, 112, D22S15, doi: 10. 1029/2007JD009077.

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