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Erratum to: Implications from Subseasonal Prediction Skills of the Prolonged Heavy Snow Event over Southern China in Early 2008


doi: 10.1007/s00376-021-1017-y

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  • Figure 8.  As in Fig. 3 but for (a) 500-hPa geopotential height over (20°–90°N, 30°–180°E) and (b) OLR over (30°S–30°N, 30°–180°E).

  • [1] Keyue ZHANG, Juan LI, Zhiwei ZHU, Tim LI, 2021: Implications from Subseasonal Prediction Skills of the Prolonged Heavy Snow Event over Southern China in Early 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1873-1888.  doi: 10.1007/s00376-021-0402-x
    [2] ZUO Qunjie, GAO Shouting, LÜ Daren, 2014: The Effect of the Subtropical Jet on the Rainfall over Southern China in January 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 543-550.  doi: 10.1007/s00376-013-3077-0
    [3] ZUO Qunjie, GAO Shouting, and LÜ Daren, 2014: Eddy Kinetic Energy Study of the Snowstorm over Southern China in January 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 972-984.  doi: 10.1007/s00376-013-3122-z
    [4] HOU Tuanjie, Fanyou KONG, CHEN Xunlai, LEI Hengchi, HU Zhaoxia, 2015: Evaluation of Radar and Automatic Weather Station Data Assimilation for a Heavy Rainfall Event in Southern China, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 967-978.  doi: 10.1007/s00376-014-4155-7
    [5] ZUO Qunjie, GAO Shouting, Lü Daren, 2013: The Propagation of Wave Packets and Its Relationship with the Subtropical Jet over Southern China in January 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 67-76.  doi: 10.1007/s00376-012-1197-6
    [6] Jiehong XIE, Jinhua YU, Haishan CHEN, Pang-Chi HSU, 2020: Sources of Subseasonal Prediction Skill for Heatwaves over the Yangtze River Basin Revealed from Three S2S Models, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 1435-1450.  doi: 10.1007/s00376-020-0144-1
    [7] LIAO Zhijie, ZHANG Yaocun, 2013: Simulation of a Persistent Snow Storm over Southern China with a Regional Atmosphere-Ocean Coupled Model, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 425-447.  doi: 10.1007/s00376-012-2098-4
    [8] LI Yue, HUANG Jianping, JI Mingxia, RAN Jinjiang, 2015: Dryland Expansion in Northern China from 1948 to 2008, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 870-876.  doi: 10.1007/s00376-014-4106-3
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    [11] Jianhua LU, 2021: Chen-Chao Koo and the Early Numerical Weather Prediction Experiments in China, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 707-716.  doi: 10.1007/s00376-021-0268-y
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    [13] Gang LI, Daoyong YANG, Xiaohua JIANG, Jing PAN, Yanke TAN, 2017: Diagnosis of Moist Vorticity and Moist Divergence for a Heavy Precipitation Event in Southwestern China, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 88-100.  doi: 10.1007/s00376-016-6124-9
    [14] ZHANG Zongjie, QIAN Weihong, 2011: Identifying Regional Prolonged Low Temperature Events in China, ADVANCES IN ATMOSPHERIC SCIENCES, 28, 338-351.  doi: 10.1007/s00376-010-0048-6
    [15] Yangmei TIAN, John L. MCBRIDE, Fumin REN, Guoping LI, Tian FENG, 2022: Changes in Typhoon Regional Heavy Precipitation Events over China from 1960 to 2018, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 272-283.  doi: 10.1007/s00376-021-1015-0
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    [17] Na LI, Baofeng JIAO, Lingkun RAN, Xinyong SHEN, Yanbin QI, 2021: On the Mechanism of a Terrain-Influenced Snow Burst Event during Midwinter in Northeast China, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 800-816.  doi: 10.1007/s00376-020-0104-9
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通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Erratum to: Implications from Subseasonal Prediction Skills of the Prolonged Heavy Snow Event over Southern China in Early 2008

    Corresponding author: Juan LI, juanl@nuist.edu.cn
  • 1. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing 210044, China
  • 2. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
  • 3. International Pacific Research Center and Department of Atmospheric Sciences, University of Hawaii at Manoa, Honolulu 96822, Hawaii

Abstract: 

  • In the original publication of this article, the blue lines (PCC skill of 500-hPa geopotential height over mid-high latitudes between the observation and ECWMF) in Fig. 8a was misplaced. The correct Fig. 8 is shown below. The associated description of “other than in P2−P3” should be “other than in P2” in section 3.3. Neither the abstract nor the conclusions are impacted.

    Figure 8.  As in Fig. 3 but for (a) 500-hPa geopotential height over (20°–90°N, 30°–180°E) and (b) OLR over (30°S–30°N, 30°–180°E).

    The online version of this original article can be found at https://doi.org/10.1007/s00376-021-0402-x.

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