Evaluation of air stagnation in China by CMIP5 models

被引:3
|
作者
Wu Jie [1 ,2 ]
Xu Ying [2 ]
Zhou Bo-Tae [2 ,3 ]
机构
[1] Chinese Acad Meteorol Sci, Beijing 100081, Peoples R China
[2] Natl Climate Ctr, Beijing 100081, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Jiangsu, Peoples R China
来源
关键词
Air stagnation days; CMIP5; Model evaluation; UNITED-STATES IMPLICATIONS; PARTICULATE MATTER PM2.5; QUALITY; SENSITIVITY; REANALYSIS; TEMPERATURE; VARIABILITY; DATASET; US;
D O I
10.6038/cjg20170406
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The change of air stagnation days is closely related with the variation of air pollutant concentration, while evaluating the performance of simulating air stagnation days will provide a basis for projection. In this paper, we calculated the number of air stagnation days during 1961-2005 by employing the outputs from 15 Coupled Model Intercomparison Project phase 5 (CMIP5) models and observation data. Then the models' ability to simulate air stagnation days was assessed. The statistical approach we used is listed as follows: standard deviation, root-mean square error, time evolution of each sectors, trend pattern and EOF (Empirical Orthogonal Function). We found that the performance of multi-model ensemble (MME) is high, but that of individual models varies widely. The CanESM2, IPSL-CM5B-LR and MME work well over the most parts of China. And MME can reproduce the spatial pattern of observed air stagnation days in summer and winter well. While the observed time evolutions of spatial averaging fluctuate greater than the simulated ones over China and its eight sub-regions, and MME values of most sectors in China are higher than the corresponding observed values. In winter, MME values are higher than the observed ones over most sectors. There is a good agreement in air stagnation trends pattern between the observational and model data over the Eastern part of China and most part of Xinjiang, but the spread of simulated trends is smaller than the one of observed trends. MME has the ability to capture the spatial distribution of EOF1 and EOF2; however, it fails to reproduce the observed time coefficient series of EOFs.
引用
收藏
页码:1293 / 1304
页数:12
相关论文
共 31 条
  • [1] Assessing the performance of Intergovernmental Panel on Climate Change AR5 climate models in simulating and projecting wind speeds over China
    Chen, Lian
    Pryor, S. C.
    Li, Dongliang
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2012, 117
  • [2] A comprehensive evaluation of precipitation simulations over China based on CMIP5 multimodel ensemble projections
    Chen, Liang
    Frauenfeld, Oliver W.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2014, 119 (10) : 5767 - 5786
  • [3] [陈晓晨 Chen Xiaochen], 2014, [气候变化研究进展, Progressus Inquisitiones de Mutatione Climatis], V10, P217
  • [4] Global air quality and climate
    Fiore, Arlene M.
    Naik, Vaishali
    Spracklen, Dominick V.
    Steiner, Allison
    Unger, Nadine
    Prather, Michael
    Bergmann, Dan
    Cameron-Smith, Philip J.
    Cionni, Irene
    Collins, William J.
    Dalsoren, Stig
    Eyring, Veronika
    Folberth, Gerd A.
    Ginoux, Paul
    Horowitz, Larry W.
    Josse, Beatrice
    Lamarque, Jean-Francois
    MacKenzie, Ian A.
    Nagashima, Tatsuya
    O'Connor, Fiona M.
    Righi, Mattia
    Rumbold, Steven T.
    Shindell, Drew T.
    Skeie, Ragnhild B.
    Sudo, Kengo
    Szopa, Sophie
    Takemura, Toshihiko
    Zeng, Guang
    [J]. CHEMICAL SOCIETY REVIEWS, 2012, 41 (19) : 6663 - 6683
  • [5] Performance metrics for climate models
    Gleckler, P. J.
    Taylor, K. E.
    Doutriaux, C.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D6)
  • [6] Changes in near-surface wind speed in China: 1969-2005
    Guo, Hua
    Xu, Ming
    Hu, Qi
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2011, 31 (03) : 349 - 358
  • [7] Horton DE, 2014, NAT CLIM CHANGE, V4, P698, DOI [10.1038/nclimate2272, 10.1038/NCLIMATE2272]
  • [8] Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO
  • [9] 2
  • [10] Kistler R, 2001, B AM METEOROL SOC, V82, P247, DOI 10.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO