Advanced Search
Article Contents

Evaluation of the Twentieth Century Reanalysis Dataset in Describing East Asian Winter Monsoon Variability

Fund Project:

doi: 10.1007/s00376-012-2226-1

  • The Twentieth Century Reanalysis (20thCR) dataset released in 2010 covers the period 1871-2010 and is one of the longest reanalysis datasets available worldwide. Using ERA-40, ERA-Interim and NCEP-NCAR reanalysis data, as well as HadSLP2 data and meteorological temperature records over eastern China, the performances of 20thCR in reproducing the spatial patterns and temporal variability of the East Asian winter monsoon (EAWM) are examined. Results indicate that 20thCR data: (1) can accurately reproduce the most typical configuration patterns of all sub-factors involved in the EAWM system, albeit with some differences in the main circulation fields over East Asia in comparison to ERA-40 reanalysis data; (2) is reliable and stable in describing the temporal variability of EAWM since the 1930s; and (3) can describe the high-frequency variability of EAWM better than the low-frequency fluctuations, especially in the early period. In conclusion, caution should be taken when using 20thCR data to study interdecadal variabilities or long-term trends of the EAWM, especially prior to the 1930s.
  • 1. Allan, R., and T. Ansell,2006:A new globally complete monthly historical mean sea level pressure data set (HadSLP2): 1850-2004. J. Climate, 19, 5816-5842.
    2. Chang, C. P., and K. M. Lau,1982:Short-term planetary-scale interaction over the tropics and the mid-latitudes during northern winter. Part I: Contrast between active and inactive periods.Mon. Wea. Rev., 110, 933-946.
    3. Chen, W.,H. F. Graf, and R. H. Huang,2000:The interannual variability of East Asian winter monsoon and its relation to the summer monsoon.Adv. Atmos. Sci., 17, 48-60.
    4. Compo, G. P.,G. N. Kiladis, and P. J. Webster,1999:The horizontal and vertical structure of East Asian winter monsoon pressure surges.Quart. J. Roy. Meteor. Soc., 125, 29-54.
    5. Compo, G. P., and Coauthors,2011:The twentieth century reanalysis project.Quart. J. Roy. Meteor. Soc., 137, 1-28.
    6. Dee, D. P., and Coauthors,2011:The ERA-Interim reanalysis: Configuration and performance of the data assimilation system.Quart. J. Roy. Meteor. Soc., 137, 553-597.
    7. Ding, Y. H., and T. N. Krishnamurti,1987:Heat budget of the Siberian high and the winter monsoon.Mon. Wea. Rev., 115, 2428-2449.
    8. Gong, D. Y., and C. H. Ho,2002:The Siberian High and climate change over middle to high latitude Asia.Theor. Appl. Climatol., 72, 1-9.
    9. Guo,Q. Y,1994:Relationship between the variations of East Asian winter monsoon and temperature anomalies in China.Quarterly Journal of Applied Meteorology, 5, 218-224. (in Chinese)
    10. Huang, R. H.,W. Chen,B. L. Yang, and R. H. Zhang,2004:Recent advances in studies of the interaction between the East Asian winter and summer monsoon and ENSO cycle.Adv. Atmos. Sci., 21, 407-424.
    11. Huang, R. H.,J. L. Chen,L. Wang, and Z. D. Lin,2012:Characteristics, processes and causes of the spatio-temporal variabilities of the East Asian monsoon system.Adv. Atmos. Sci., 29, 910-942, doi: 10.1007/s00376-012-2015-x.
    12. Jhun, J., and E. Lee,2004:A new East Asian winter monsoon index and associated characteristics of the winter monsoon.J. Climate, 17, 711-726.
    13. Ji, L. R.,S. Q. Sun,K. Arpe, and L. Bengtsson,1997:Model study on the interannual variability of Asian winter monsoon and its influence.Adv. Atmos. Sci., 14, 1-22.
    14. Kalnay, E., and Coauthors,1996:The NCEP/NCAR 40-year reanalysis project.Bull. Amer. Meteor. Soc., 77, 437-471.
    15. Lau, K. M., and M. T. Li,1984:The monsoon of East Asia and its global associations-A survey.Bull. Amer. Meteor. Soc., 65, 114-125.
    16. Li, C. Y., and M. Q. Mu,2000:Relationship between East Asian winter monsoon, warm pool situation and ENSO cycle.Chinese Science Bulletin, 45, 1448-1455.
    17. Shi, N.,1996:Features of the East Asian winter monsoon intensity on multiple time scale in recent 40 years and their relation to climate.Quarterly Journal of Applied Meteorology, 7, 175-182. (in Chinese)
    18. Uppala, S. M., and Coauthors,2005:The ERA-40 re-analysis.Quart. J. Roy. Meteor. Soc., 131, 2961-3012.
    19. Wang, B., and Coauthors,2008:How to measure the strength of the East Asian summer monsoon.J. Climate, 21, 4449-4463.
    20. Wang, L., and W. Chen,2010:How well do existing indices measure the strength of the East Asian winter monsoon?Adv. Atmos. Sci., 27, 855-870, doi: 10.1007/s00376-009-9094-3.
    21. Wang, L.,R. H. Huang,L. Gu,W. Chen, and L. H. Kang,2009a:Interdecadal variations of the East Asian winter monsoon and their association with quasi-stationary planetary wave activity.J. Climate., 22, 4860-4872.
    22. Wang, S. W., and Coauthors,2009b:Atlas of Seasonal Temperature and Precipitation Anomalies over China (1880-2007). China Meteorological Press, 257pp.
    23. Zhang, Y.,K. Sperber, and J. Boyle,1997:Climatology and interannual variation of the East Asian winter monsoon: Results from the 1979-95 NCEP/NCAR reanalysis. Mon. Wea. Rev., 125, 2605-2619.
    24. Zhang, Z. Y.,D. Y. Gong,M,Hu, and Y. N. Lei,2012:Comparisons of the multiple East Asian winter monsoon indices and their relations to climate over eastern China.Geographical Research,31, 987-1003. (in Chinese)
    25. Zhou, L. T.,2011:Impact of East Asian winter monsoon on rainfall over southeastern China and its dynamical process.Int. J. Climatol., 31, 677-686.
  • [1] Wu Bingyi, Wang Jia, 2002: Possible Impacts of Winter Arctic Oscillation on Siberian High, the East Asian Winter Monsoon and Sea-Ice Extent, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 297-320.  doi: 10.1007/s00376-002-0024-x
    [2] FENG Juan*, CHEN Wen, 2014: Interference of the East Asian Winter Monsoon in the Impact of ENSO on the East Asian Summer Monsoon in Decaying Phases, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 344-354.  doi: 10.1007/s00376-013-3118-8
    [3] CHEN Shangfeng, CHEN Wen, WEI Ke, 2013: Recent Trends in Winter Temperature Extremes in Eastern China and their Relationship with the Arctic Oscillation and ENSO, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1712-1724.  doi: 10.1007/s00376-013-2296-8
    [4] Chen Wen, Hans-F. Graf, Huang Ronghui, 2000: The Interannual Variability of East Asian Winter Monsoon and Its Relation to the Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 48-60.  doi: 10.1007/s00376-000-0042-5
    [5] YAN Hongming, YANG Hui, YUAN Yuan, LI Chongyin, 2011: Relationship Between East Asian Winter Monsoon and Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 1345-1356.  doi: 10.1007/s00376-011-0014-y
    [6] LI Fei, WANG Huijun, 2012: Predictability of the East Asian Winter Monsoon Interannual Variability as Indicated by the DEMETER CGCMS, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 441-454.  doi: 10.1007/s00376-011-1115-3
    [7] Se-Hwan YANG, LU Riyu, 2014: Predictability of the East Asian Winter Monsoon Indices by the Coupled Models of ENSEMBLES, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 1279-1292.  doi: 10.1007/s00376-014-4020-8
    [8] ZENG Gang, Wei-Chyung WANG, SUN Zhaobo, LI Zhongxian, 2011: Atmospheric Circulation Cells Associated with Anomalous East Asian Winter Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 913-926.  doi: 10.1007/s00376-010-0100-6
    [9] Hoffman H. N. CHEUNG, Wen ZHOU, 2016: Simple Metrics for Representing East Asian Winter Monsoon Variability: Urals Blocking and Western Pacific Teleconnection Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 695-705.  doi: 10.1007/s00376-015-5204-6
    [10] Jiapeng MIAO, Tao WANG, Huijun WANG, Yongqi GAO, 2018: Influence of Low-frequency Solar Forcing on the East Asian Winter Monsoon Based on HadCM3 and Observations, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1205-1215.  doi: 10.1007/s00376-018-7229-0
    [11] YANG Hui, SUN Shuqing, 2005: The Characteristics of Longitudinal Movement of the Subtropical High in the Western Pacific in the Pre-rainy Season in South China, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 392-400.  doi: 10.1007/BF02918752
    [12] WEI Ke, BAO Qing, 2012: Projections of the East Asian Winter Monsoon under the IPCC AR5 Scenarios Using a Coupled Model: IAP-FGOALS, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 1200-1214.  doi: 10.1007/s00376-012-1226-5
    [13] LI Fei, WANG Huijun, 2013: Relationship between Bering Sea Ice Cover and East Asian Winter Monsoon Year-to-Year Variations, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 48-56.  doi: 10.1007/s00376-012-2071-2
    [14] Wen CHEN, Lin WANG, Juan FENG, Zhiping WEN, Tiaojiao MA, Xiuqun YANG, Chenghai WANG, 2019: Recent Progress in Studies of the Variabilities and Mechanisms of the East Asian Monsoon in a Changing Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 887-901.  doi: 10.1007/s00376-019-8230-y
    [15] LI Qiaoping, DING Yihui, DONG Wenjie, YAN Guanhua, 2007: A Numerical Study on the Winter Monsoon and Cold Surge over East Asia, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 664-678.  doi: 10.1007/s00376-007-0664-y
    [16] Wen CHEN, Renhe ZHANG, Renguang WU, Zhiping WEN, Liantong ZHOU, Lin WANG, Peng HU, Tianjiao MA, Jinling PIAO, Lei SONG, Zhibiao WANG, Juncong LI, Hainan GONG, Jingliang HUANGFU, Yong LIU, 2023: Recent Advances in Understanding Multi-scale Climate Variability of the Asian Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1429-1456.  doi: 10.1007/s00376-023-2266-8
    [17] Tae-Won PARK, Jee-Hoon JEONG, Chang-Hoi HO, Seong-Joong KIM, 2008: Characteristics of Atmospheric Circulation Associated with Cold Surge Occurrences in East Asia: A Case Study During 2005/06 Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 791-804.  doi: 10.1007/s00376-008-0791-0
    [18] WEI Ke, CHEN Wen, ZHOU Wen, 2011: Changes in the East Asian Cold Season since 2000, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 69-79.  doi: 10.1007/s00376-010-9232-y
    [19] Qian LU, Jian RAO, Chunhua SHI, Dong GUO, Ji WANG, Zhuoqi LIANG, Tian WANG, 2022: Observational Subseasonal Variability of the PM2.5 Concentration in the Beijing-Tianjin-Hebei Area during the January 2021 Sudden Stratospheric Warming, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 1623-1636.  doi: 10.1007/s00376-022-1393-y
    [20] LU Riyu, LI Ying, Buwen DONG, 2007: Arctic Oscillation and Antarctic Oscillation in Internal Atmospheric Variability with an Ensemble AGCM Simulation, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 152-162.  doi: 10.1007/s00376-007-0152-4

Get Citation+

Export:  

Share Article

Manuscript History

Manuscript received: 11 September 2012
Manuscript revised: 02 November 2012
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Evaluation of the Twentieth Century Reanalysis Dataset in Describing East Asian Winter Monsoon Variability

    Corresponding author: ZHANG Ziyin; 
  • 1. Beijing Meteorological Bureau, Beijing 100089; 
  • 2. State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875; 
  • 3. Korea Polar Research Institute, Incheon 406-840, Korea
Fund Project:  This work was supported by the State Key Laboratory of Earth Surface Processes and Resource Ecology (Grant No. 2013-KF-05) and the National Basic Research Program of China (Grant Nos. 2012CB955401 and 2010CB428506). Seong-Joong KIM was supported by the project Reconstruction and Observation of Components for the Southern and Northern Annular Mode to Investigate the Cause of Polar Climate Change (PE13010) of the Korea Polar Research Institute.

Abstract: The Twentieth Century Reanalysis (20thCR) dataset released in 2010 covers the period 1871-2010 and is one of the longest reanalysis datasets available worldwide. Using ERA-40, ERA-Interim and NCEP-NCAR reanalysis data, as well as HadSLP2 data and meteorological temperature records over eastern China, the performances of 20thCR in reproducing the spatial patterns and temporal variability of the East Asian winter monsoon (EAWM) are examined. Results indicate that 20thCR data: (1) can accurately reproduce the most typical configuration patterns of all sub-factors involved in the EAWM system, albeit with some differences in the main circulation fields over East Asia in comparison to ERA-40 reanalysis data; (2) is reliable and stable in describing the temporal variability of EAWM since the 1930s; and (3) can describe the high-frequency variability of EAWM better than the low-frequency fluctuations, especially in the early period. In conclusion, caution should be taken when using 20thCR data to study interdecadal variabilities or long-term trends of the EAWM, especially prior to the 1930s.

Reference

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint