Xing Caiying, Wu Sheng'an, Zhu Jingjing. Comparison on the circulation background of tropical cyclone affecting the South China Sea based upon different reanalysis datasets. J Appl Meteor Sci, 2023, 34(2): 179-192. DOI:  10.11898/1001-7313.20230205.
Citation: Xing Caiying, Wu Sheng'an, Zhu Jingjing. Comparison on the circulation background of tropical cyclone affecting the South China Sea based upon different reanalysis datasets. J Appl Meteor Sci, 2023, 34(2): 179-192. DOI:  10.11898/1001-7313.20230205.

Comparison on the Circulation Background of Tropical Cyclone Affecting the South China Sea Based upon Different Reanalysis Datasets

DOI: 10.11898/1001-7313.20230205
  • Received Date: 2022-08-05
  • Rev Recd Date: 2022-12-20
  • Publish Date: 2023-03-31
  • China Meteorological Administration launched China's Global atmospheric reanalysis program in November 2013, and the global atmospheric reanalysis product (CMA-RA) has been successfully developed. The performance of CMA-RA on describing the circulation background of tropical cyclone activity affecting the South China Sea is analyzed and compared with ERA5 and NCEP-Ⅰ, exploring the applicability of CMA-RA in tropical cyclone activity analysis, based on the tropical cyclone best track dataset compiled by Shanghai Typhoon Research Institute of China Meteorological Administration, CMA-RA, the fifth generation ECMWF atmospheric reanalysis dataset (ERA5) and the first generation atmospheric monthly reanalysis dataset of National Center for Environmental Prediction(NCEP) and National Center for Atmospheric Research(NCAR) from 1981 to 2020. The results are shown as follows. Three reanalysis datasets can basically depict the anomaly circulation characteristics of the key influence regions closely related to tropical cyclone activity affecting the South China Sea from July to October, including the Southern Oscillation, low-level zonal wind field in the Philippines to the eastern sea of the South China Sea, reverse distribution pattern of low-level zonal wind filed in the tropics, low-level vorticity from the Philippines to the central and eastern part of the South China Sea, environmental vertical wind shear in the tropical western Pacific, and mid-level humidity field from the South China Sea to the eastern sea of the Philippines. All datasets are highly similar in describing the Southern Oscillation, low-level zonal wind field and mid-level humidity field of key regions. CMA-RA and ERA5 have high agreement on the Southern Oscillation, low-level zonal wind characteristics and their relationship with tropical cyclone activity, which are closer than NCEP-Ⅰ. However, their characterization of low-level meridional wind field, relative vorticity and vertical wind shear are relatively different. Some circulations in the tropical Indian Ocean are relatively different with each other too. All datasets have similar ability to depict the key regions circulations in the extreme years of tropical cyclone activity, but they are different in area and intensity. They are highly consistent in the sea level pressure and low-level zonal wind characteristics, with CMA-RA and ERA5 being the most similar. The mid-level humidity of CMA-RA is consistent with ERA5, and they are both lower than NCEP-Ⅰ. But the characteristics of low-level relative vorticity and vertical wind shear are significantly different. CMA-RA has comparable performance with ERA5 and NCEP-Ⅰ in describing the circulation background of tropical cyclone activity affecting the South China Sea, and it's highly consistent with ERA5 on the whole. Therefore, it can provide an alternative atmospheric reanalysis dataset for the research of tropical cyclone activity in the South China Sea.
  • Fig. 1  Impact region of tropical cyclone in the South China Sea

    Fig. 2  Comparison of different datasets in correlations between sea level pressure and tropical cyclone frequency of the South China Sea from Jul to Oct

    (the shaded denotes passing the test of 0.05 level, the same hereinafter)

    Fig. 3  Comparison of different datasets in correlations of 850 hPa zonal wind, 850 hPa meridional wind to tropical cyclone frequency of the South China Sea from Jul to Oct

    Fig. 4  Comparison of different datasets in correlations of 850 hPa relative vorticity, vertical wind shear to tropical cyclone frequency of the South China Sea from Jul to Oct

    Fig. 5  Comparison of different datasets in correlations between 600 hPa relative humidity and tropical cyclone frequency of the South China Sea from Jul to Oct

    Fig. 6  Sea level pressure difference between different datasets in extreme tropical cyclone frequency years of the South China Sea from Jul to Oct

    Fig. 7  The same as in Fig 6, but for 850 hPa wind

    (the arrow denotes wind vector, the shaded denotes wind speed difference)

    Fig. 8  850 hPa relative vorticity difference and vertical wind shear difference between different datasets from Jul to Oct in 2004

    Fig. 9  The same as in Fig. 6, but for 600 hPa relative humidity

    Table  1  Comparison of different datasets in variance contributions of the first two EOF modes of 850 hPa zonal wind anomaly in tropical region from Jul to Oct (unit:%)

    模态 CMA-RA ERA5 NCEP-Ⅰ
    EOF1 60.9 61.8 52.8
    EOF2 10.2 10.3 13.3
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  • [1]
    Zhao T B, Fu C B, Ke Z J, et al. Global atmosphere reanalysis datasets: Current status and recent advances. Adv Earth Sci, 2010, 25(3): 242-254. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201003002.htm
    [2]
    Wang J C, Lu H J, Han W, et al. Improvements and performances of the operational GRAPES_GFS 3DVar system. J Appl Meteor Sci, 2017, 28(1): 11-24. doi:  10.11898/1001-7313.20170102
    [3]
    Kalnay E, Kanamitsu M, Kistler R, et al. The NCEP/NCAR 40-year reanalysis project. Bull Amer Meteor Soc, 1996, 77(3): 437-471. doi:  10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2
    [4]
    Kanamitsu M, Ebisuzaki W, Woollen J, et al. NCEP/DOE AMIP-Ⅱ reanalysis(R-2). Bull Amer Meteor Soc, 2002, 83(1): 1631-1644.
    [5]
    Dee D P, Uppala S M, Simmons A J, et al. The ERA-Interim reanalysis: Configuration and performance of the data assimilation system. Quart J Royal Meteor Soc, 2011, 137: 553-597. doi:  10.1002/qj.828
    [6]
    Hersbach H, Bell B, Berrisford P, et al. The ERA5 global reanalysis. Quart J Roy Meteor Soc, 2020, 146(730): 1999-2049. doi:  10.1002/qj.3803
    [7]
    Gelaro R, Mccarty W, Suárez M, et al. The modern-era retrospective analysis for research and applications, version 2(MERRA-2). J Climate, 2017, 30(14): 5419-5454. doi:  10.1175/JCLI-D-16-0758.1
    [8]
    Kobayashi S, Ota Y, Harada Y, et al. The JRA-55 reanalysis: General specifications and basic characteristics. J Meteor Soc, 2015, 93(1): 5-48. doi:  10.2151/jmsj.2015-001
    [9]
    Wei F F, Tang J P, Wang S Y. A reliability assessment of upper-level reanalysis datasets over China. Chinese J Geophys, 2015, 58(2): 383-397. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201502004.htm
    [10]
    Brunke M A, Stegall S T, Zeng X B. A climatology of tropospheric humidity inversions in five reanalyzes. Atmos Res, 2015, 153: 165-187. doi:  10.1016/j.atmosres.2014.08.005
    [11]
    Huo Z H, Li X L, Chen J, et al. CMA global ensemble prediction using singular vectors from background field. J Appl Meteor Sci, 2022, 33(6): 655-667. doi:  10.11898/1001-7313.20220602
    [12]
    Guo Y J, Zhang S Q, Yan J H, et al. A comparison of atmosphere temperature over China between radiosonde observations and multiple reanalysis datasets. Acta Meteor Sinica, 2016, 74(2): 271-284. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXB201602009.htm
    [13]
    Zhang M, Yu H P, Huang J P, et al. Assessment on unsystematic errors of GRAPES_GFS2.0. J Appl Meteor Sci, 2019, 30(3): 332-344. doi:  10.11898/1001-7313.20190307
    [14]
    Li Z, Chen J, Ma Z S, et al. Deviation distribution features of CMA-GFS cloud prediction. J Appl Meteor Sci, 2022, 33(5): 527-540. doi:  10.11898/1001-7313.20220502
    [15]
    Zhu Z, Shi C X, Zhang T, et al. Applicability analysis of various reanalyzed land surface temperature datasets in China. J Glaciol and Geocryology, 2015, 37(3): 614-624. https://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201503007.htm
    [16]
    Zhu J, Hu A, Yan D Q, et al. Can reanalysis datasets describe the persistent temperature and precipitation extremes over China?. Theor Appl Climatol, 2017, 130(1/2): 655-671.
    [17]
    Ding L, Li Q Q, Liu Y Y. The tropical atmospheric intra-seasonal oscillation with different reanalysis data. J Appl Meteor Sci, 2013, 24(3): 314-322. http://qikan.camscma.cn/article/id/20130307
    [18]
    Huang Y L, Chen H S, Jiang W, et al. Multi-spatial modes of East Asian summer monsoon activity: Comparative analysis of various reanalysis data. Chinese J Atmos Sci, 2015, 39(1): 145-160. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXK201501012.htm
    [19]
    Liu G, Xu S Q, Lian Y. Recognition results of blocking high in Asia during summer and its possible impacts on climate anomalies in Northeast China: Comparison of various reanalysis data. Acta Meteor Sinica, 2019, 77(2): 303-314. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXB201902011.htm
    [20]
    Qin H, Zheng F Q, Wu L Q. The interaction between intensity and rainfall of Typhoon Rammasun(1409). J Appl Meteor Sci, 2022, 33(4): 477-488. doi:  10.11898/1001-7313.20220408
    [21]
    Kong L S, Zhang X Z. Sensitive experiments on reconstruction model of historical typhoon wind field in the Northwest Pacific ocean. J Appl Meteor Sci, 2022, 33(1): 56-68. doi:  10.11898/1001-7313.20220105
    [22]
    Murakami H. Tropical cyclones in reanalysis data sets. Geophys Res Lett, 2014, 41(6): 2133-2141.
    [23]
    Deng S R, Wu L G, Wang R F, et al. Analysis of tropical cyclone genesis potential index with multiple reanalysis data. J Meteor Sci, 2014, 34(3): 243-251. https://www.cnki.com.cn/Article/CJFDTOTAL-QXKX201403002.htm
    [24]
    Malakar P, Kesarkar A P, Bhate J N, et al. Comparison of reanalysis datasets to comprehend the evolution of tropical cyclones over North Indian Ocean. Earth Space Sci, 2020, 7(2): e2019EA000978.
    [25]
    Li Y, Jin R, Gao X. Outflow-jet interaction analysis of tropical cyclone Roke(2011) within different atmospheric reanalysis datasets. Trans Atmos Sci, 2020, 43(3): 525-536. https://www.cnki.com.cn/Article/CJFDTOTAL-NJQX202003010.htm
    [26]
    Schenkel B A, Hart R E. An examination of tropical cyclone position, intensity and intensity life cycle within atmospheric reanalysis datasets. J Climate, 2012, 25(10): 3453-3475.
    [27]
    Yan J M, Zhao B K, Zhang S, et al. Observation analysis and application evaluation of wind profile radar to diagnosing the boundary layer of landing typhoon. J Appl Meteor Sci, 2021, 32(3): 332-346. doi:  10.11898/1001-7313.20210306
    [28]
    Hodges K, Cobb A, Vidale P L. How well are tropical cyclones represented in reanalysis datasets. J Climate, 2017, 30(14): 5243-5264.
    [29]
    Wu H, Xing C Y, Wu S A, et al. Frequency prediction of tropical cyclones affecting Hainan in summer. J Trop Meteor, 2016, 32(3): 377-384. https://www.cnki.com.cn/Article/CJFDTOTAL-RDQX201603009.htm
    [30]
    Xing C Y, Wu H, Hu D Q, et al. Application of CFSv2 products in tropical cyclone frequency prediction model in Hainan during flood season. J Meteor Sci, 2017, 37(5): 666-672. https://www.cnki.com.cn/Article/CJFDTOTAL-QXKX201705011.htm
    [31]
    Wang M Y, Yao S, Jiang L P, et al. Collection and pre-processing of satellite remote-sensing data in CRA-40(CMA's Global Atmospheric ReAnalysis). Adv Meteor Sci Tech, 2018, 8(1): 158-163. https://www.cnki.com.cn/Article/CJFDTOTAL-QXKZ201801038.htm
    [32]
    Li C X, Zhao T B, Shi C X, et al. Assessment of precipitation from the CRA40 dataset and new generation reanalysis datasets in the global domain. Int J Climatol, 2021, 41(11): 5243-5263.
    [33]
    Zhou Z J, Cao L J, Liao J, et al. Overview of hydrometeorological information: Observation, data fusion and reanalysis. Meteor Mon, 2022, 48(3): 272-283. https://www.cnki.com.cn/Article/CJFDTOTAL-QXXX202203002.htm
    [34]
    Li C X, Zhao T B, Shi C X, et al. Evaluation of daily precipitation product in China from the CMA global atmospheric interim reanalysis. J Meteor Res, 2020, 34: 117-136.
    [35]
    Yang J X, Huang M T, Zhai P M. Performance of the CRA-40/Land, CMFD, and ERA-Interim datasets in reflecting changes in surface air temperature over the Tibetan Plateau. J Meteor Res, 2021, 35(4): 663-672.
    [36]
    Zhang D J, Shi C X, Zhang T, et al. Comparative analysis of the total cloud cover products of various data in China. Plateau Meteor, 2022, 41(3): 803-813. https://www.cnki.com.cn/Article/CJFDTOTAL-GYQX202203021.htm
    [37]
    Liu M J, Zhang W X, Zhang Z Y, et al. On the applicability of CRA40 in GNSS precipitable water vapor retrieval over China. Journal of Nanjing University of Information Science & Technology(Nat Sci Ed), 2021, 13(2): 138-144. https://www.cnki.com.cn/Article/CJFDTOTAL-NJXZ202102003.htm
    [38]
    Yu X J, Zhang L X, Zhou T J, et al. The Asian subtropical westerly jet stream in CRA-40, ERA5, and CFSR reanalysis data: Comparative assessment. J Meteor Res, 2021, 35(1): 46-63.
    [39]
    Lu X, Yu H, Ying M, et al. Western North Pacific tropical cyclone database created by the China Meteorological Administration. Adv Atmos Sci, 2021, 38(4): 690-699.
    [40]
    Cheng Z Q, Lin L X, Yang G J, et al. Rapid intensification and associated large-scale circulation of super Typhoon Rammasun in 2014. J Appl Meteor Sci, 2017, 28(3): 318-326. doi:  10.11898/1001-7313.20170306
    [41]
    Zheng Q, Gao M. An objective prediction model for tropical cyclone genesis in the Northwest Pacific. J Appl Meteor Sci, 2022, 33(5): 594-603. doi:  10.11898/1001-7313.20220507
    [42]
    Gao S Z, Zhang S J, Lü X Y, et al. Circulation characteristics and thermal and dynamic conditions 48 hours before typhoon formation in the South China Sea. J Appl Meteor Sci, 2021, 32(3): 272-288. doi:  10.11898/1001-7313.20210302
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    • Received : 2022-08-05
    • Accepted : 2022-12-20
    • Published : 2023-03-31

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