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张海玲, 王斌, 毛嘉富. 陆面气温资料的一种推广三维变分同化方法及其在简化情形的检验[J]. 气候与环境研究, 2009, 14(3): 273-283. DOI: 10.3878/j.issn.1006-9585.2009.03.04
引用本文: 张海玲, 王斌, 毛嘉富. 陆面气温资料的一种推广三维变分同化方法及其在简化情形的检验[J]. 气候与环境研究, 2009, 14(3): 273-283. DOI: 10.3878/j.issn.1006-9585.2009.03.04
Zhang Hailing, Wang Bin, Mao Jiafu. A Generalized Approach of Three dimensional Variational Data Assimilation for Land Surface Air Temperature and Its Tests under Simplification Cases[J]. Climatic and Environmental Research, 2009, 14(3): 273-283. DOI: 10.3878/j.issn.1006-9585.2009.03.04
Citation: Zhang Hailing, Wang Bin, Mao Jiafu. A Generalized Approach of Three dimensional Variational Data Assimilation for Land Surface Air Temperature and Its Tests under Simplification Cases[J]. Climatic and Environmental Research, 2009, 14(3): 273-283. DOI: 10.3878/j.issn.1006-9585.2009.03.04

陆面气温资料的一种推广三维变分同化方法及其在简化情形的检验

A Generalized Approach of Three dimensional Variational Data Assimilation for Land Surface Air Temperature and Its Tests under Simplification Cases

  • 摘要: 发展了一种同化窗口为1个月的陆面气温推广三维变分资料同化方法,并建立了逐日资料到月平均资料的观测算子。作为对该同化方法的初步检验,以2000年1月中国陆地区域时间分辨率低、空间分辨率较高且在高原地区与台站观测资料比较接近的CRU(Climate Research Unit)月平均陆面气温资料作为观测,以时间分辨率高、空间分辨率较低且在高原地区与台站资料有较大误差的NCEP逐日气温资料作为背景场,采用背景误差协方差矩阵(简称B矩阵)的两种简化对角形式进行同化试验,得到高时空分辨率的格点陆面气温分析场,并进行对比分析和均方根误差检验。结果显示,由两种简化形式得到的逐日资料和月平均资料的质量均得到改善,在我国东南和中部大部分地区与台站观测基本一致,在青藏高原、新疆等台站稀疏地区与地形对应良好,为M-SDGVM模型或其他陆面过程模式高质量陆面气象驱动场的准备提供了一种新的手段。尤其在B矩阵中考虑了方差逐日变化的简化形式所得到的分析场整体上要优于不考虑的,这为最终在B矩阵中考虑协方差(即对推广三维变分同化不作简化)进一步改进同化效果打下了基础。

     

    Abstract: A generalized approach of threedimensional variational data assimilation (G-3DVar) with 1month assimilation window for land surface air temperature data was developed. As preliminary tests on this approach, two simplified forms of background error covariance matrix (B matrix for short) were applied to generate a high spacetime resolution grid analysis field of land surface air temperature in January 2000 in China through incorporating the CRU monthly mean data into the NCEP daily reanalysis data based on an observation operator associating the daily data and monthly mean data. The CRU monthly mean land surface air temperature data have low temporal resolution, but higher spatial resolution and better approximation to the station observations on the Tibetan Plateau, while the NCEP daily reanalysis data have high temporal resolution, but lower spatial resolution and worse approximation to station observations in these areas. A comparison shows that the qualities of both the daily and monthly mean data of the generated grid analysis fields from both simplified forms are all improved, which are basically consistent with the station observations in the south eastern and central areas of China and well match the topography in the Tibetan Plateau,Xinjiang and so on, where the observation stations are sparse. It indicates that the G3DVar is a new efficient approach for preparing meteorological driving field for land ecological model or land surface model. Further comparison also shows that the analysis field from the simplified form with daily variance in the B matrix is better than that from the simplified without considering daily variance in the B matrix. It is an important basis for further improvement of assimilation performance of G-3DVar without any simplification, ie. covariance is considered in the B matrix.

     

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