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太平洋副热带高压及南亚高压在NCEP/NCAR和ECMWF再分析资料中的对比研究

陈雯 智协飞

陈雯, 智协飞. 太平洋副热带高压及南亚高压在NCEP/NCAR和ECMWF再分析资料中的对比研究[J]. 热带气象学报, 2008, (2): 189-194.
引用本文: 陈雯, 智协飞. 太平洋副热带高压及南亚高压在NCEP/NCAR和ECMWF再分析资料中的对比研究[J]. 热带气象学报, 2008, (2): 189-194.
CHEN Wen, ZHI Xie-fei. ECMWF REANALYSIS DATASETS COMPARISONS OF THE WEST PACIFIC SUBTROPICAL HIGH AND OF THE SOUTH ASIA HIGH BETWEEN NCEP/NCAR AND ECMWF REANALYSIS DATASETS[J]. Journal of Tropical Meteorology, 2008, (2): 189-194.
Citation: CHEN Wen, ZHI Xie-fei. ECMWF REANALYSIS DATASETS COMPARISONS OF THE WEST PACIFIC SUBTROPICAL HIGH AND OF THE SOUTH ASIA HIGH BETWEEN NCEP/NCAR AND ECMWF REANALYSIS DATASETS[J]. Journal of Tropical Meteorology, 2008, (2): 189-194.

太平洋副热带高压及南亚高压在NCEP/NCAR和ECMWF再分析资料中的对比研究

基金项目: 江苏省自然灾害重点实验室(KLME050210)项目资助

ECMWF REANALYSIS DATASETS COMPARISONS OF THE WEST PACIFIC SUBTROPICAL HIGH AND OF THE SOUTH ASIA HIGH BETWEEN NCEP/NCAR AND ECMWF REANALYSIS DATASETS

  • 摘要: 利用NCEP/NCAR和ECMWF 1961~2000年北半球逐月平均的500 hPa和100 hPa高度场再分析资料对影响我国天气、气候的重要系统——北半球西太平洋副热带高压以及南亚高压做了对比研究,发现两者在不同的再分析资料中虽然具有一定的相似性,但也存在着明显的区别。在1980年以前两者存在较大差异。NCEP/NCAR再分析资料分析出的副高明显偏弱,而其所反映的副高的变化在幅度和强度上均大于ECMWF再分析资料的结果。进一步分析发现,NCEP/NCAR再分析资料所得出的副高的年代际变化可能是不真实的。在1969年、1979~1991年间,NCEP/NCAR再分析资料中的南亚高压中心强度明显比ECMWF的强,特别是1992~1995年间,NCEP/NCAR再分析资料中的南亚高压中心强度更强且中心范围更大。此外,NCEP/NCAR再分析资料所反映的南亚高压的变化在幅度和强度上也都大于ECMWF再分析资料的结果。

     

  • [1] 何金海,温敏,施晓晖,等.南海夏季风建立期间副高带断裂和东撤及其可能机制[J].南京大学学报,2002,38(3):318-330.
    [2] 陶诗言,赵思雄,周晓平,等.天气学和天气预报的研究进展[J].大气科学,2003,27(4):451-467.
    [3] 吴国雄,毛江玉,段安民,等.青藏高原影响亚洲夏季气候研究的最新进展[J].气象学报,2004,62(5):528-540.
    [4] 钱永甫,张琼,张学洪.南亚高压与我国盛夏气候异常[J].南京大学学报,2002,38(3):295-307.
    [5] STERL A.On (in) homogeneity of reanalysis products[J].Journal of climate,2004,17(19):3 866-3 873.
    [6] POCARD I,JANICOT S,CAMBERLIN P.Comparison of rainfall structures between NCEP/NCAR reanalysis and observed data over tropical Africa[J].Climate Dynamics,2000,16 (12):897-916.
    [7] DELL'AQUILA A,LUCARINI V,RUTI P M,et al.Hayashi spectra of the northern hemisphere mid-latitude atmospheric variability in the NCEP/NCAR and ECMWF reanalysis[J].Climate Dynamics,2005,25(6):639-652.
    [8] JOSEY S A.A comparison of ECMWF,NCEP/NCAR and SOC surface heat fluxes with Moored Buoy Measurements in Subdnction Region of the Northeast Atlantic[J].Journal of Climate,2001,14(8):1 780-1 789.
    [9] TRIGO I F.Climatology and Interannual variability of storm-tracks in the Euro-Atlantic sector:a comparison between ERA-40 and NCEP/NCAR reanalysis[J].Climate Dynamics,2006,26(2/3):127-143.
    [10] DAVID H B,RYAN L F.Strong trends in the skill of the ERA-40 and NCEP/NCAR Reanalysis in the high and midlatitudes of the southern hemisphere,1958-2001[J].Journal of Climate,2004,17(23):4 603-4 619.
    [11] ANNAMALAI H,SLINGO J M,SPERBER K R.The mean evolution and variability of the Asian Summer Monsoon:Comparison of ECMWF and NCEP/NCAR Reanalysis[J].Monthly Weather Review,1999,127(6):1 157-1 186.
    [12] INOUE T,MATSUMOTO J.A comparison of summer sea level pressure over east Eurasia between NCEP-NCAR reanalysis and ERA-40 for the Period 1960-1999[J].Journal of the Meteorological Society of Japan,2004,82(3):951-958.
    [13] CUI Maochang (崔茂常),FENG Ming (冯明),LIAN Shumin (练树民).Evaluation of daily precipitation in China from ECMWF and NCEP Reanalysis[J].Chinese Journal of Oceanology and Limnology,2000,18(1):35-41.
    [14] 岳阳,管兆勇,王盘兴.两种再分析资料间Hadley环流双层结构的差异[J].南京气象学院学报,2005,28(5):695-703.
    [15] 魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,1999:35-63.
    [16] MANN H B.Nonparametric tests against trend[J].Econometrica,1945,13(3):245-259.
    [17] KENDALL M G.Rank correlation methods[M].London:Charles Griffin,1970:125-130.
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出版历程
  • 收稿日期:  2006-10-25
  • 修回日期:  2007-05-28

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