Advanced Search
Article Contents

Delayed Impacts of the El Nino Episodes in the Central Pacific on the Summertime Climate Anomalies of Eastern China in 2003 and 2007


doi: 10.1007/s00376-009-0553-7

  • In the summers of 2003 and 2007, eastern China suffered similar climate disasters with severe flooding in the Huaihe River valley and heat waves in the southern Yangtze River delta and South China. Using SST data and outgoing longwave radiation (OLR) data from NOAA along with reanalysis data from NCEP/NCAR, the 2002/03 and 2006/07 El Nino episodes in the central Pacific and their delayed impacts on the following early summertime climate anomalies of eastern China were analyzed. The possible physical progresses behaved as follows: Both of the moderate El Nino episodes matured in the central equatorial Pacific during the early winter. The zonal wind anomalies near the sea surface of the west-central equatorial Pacific excited equatorial Kelvin waves propagating eastward and affected the evolution of the El Ni\~no episodes. From spring to early summer, the concurring anomalous easterly winds in the central equatorial Pacific and the end of upwelling Kelvin waves propagating eastward in the western equatorial Pacific, favored the equatorial warm water both of the SST and the subsurface temperature in the western Pacific. These conditions favored the warm state of the western equatorial Pacific in the early summer for both cases of 2003 and 2007. Due to the active convection in the western equatorial Pacific in the early summer and the weak warm SST anomalies in the tropical western Pacific from spring to early summer, the convective activities in the western Pacific warm pool showed the pattern in which the anomalous strong convection only appeared over the southern regions of the tropical western Pacific warm pool, which effects the meridional shift of the western Pacific subtropical high in the summer. The physical progress of the delayed impacts of the El Ni\~no episodes in the central equatorial Pacific and their decaying evolution on the climate anomalies in eastern China were interpreted through the key role of special pattern for the heat convection in the tropical western Pacific warm pool and the response of the western North Pacific anomalous anticyclone.
  • [1] Dai Xiaosu, Ding Yihui, 1994: A Modeling Study of Climate Change and Its Implication for Agriculture in China Part II: The Implication of Climate Change for Agriculture in China, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 499-506.  doi: 10.1007/BF02658171
    [2] WANG Geli, YANG Peicai, LIU Chuanxi, LIU Yi, LU Daren, 2010: Impacts of Future NOx and CO Emissions on Regional Chemistry and Climate over Eastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 750-760.  doi: 10.1007/s00376-009-9101-8
    [3] ZENG Xiaodong, 2010: Evaluating the Dependence of Vegetation on Climate in an Improved Dynamic Global Vegetation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 27, 977-991.  doi: 10.1007/s00376-009-9186-0
    [4] LI Yunying, YU Rucong, XU Youping, ZHOU Tianjun, 2005: AREM Simulations of Cloud Features over Eastern China in February 2001, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 260-270.  doi: 10.1007/BF02918515
    [5] Yali ZHU, Tao WANG, Jiehua MA, 2016: Influence of Internal Decadal Variability on the Summer Rainfall in Eastern China as Simulated by CCSM4, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 706-714.  doi: 10.1007/s00376-016-5269-x
    [6] Hemin SUN, Guojie WANG, Xiucang LI, Jing CHEN, Buda SU, Tong JIANG, 2017: Regional Frequency Analysis of Observed Sub-Daily Rainfall Maxima over Eastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 209-225.  doi: 10.1007/s00376-016-6086-y
    [7] Yue ZHANG, Wen ZHOU, Ruhua ZHANG, 2024: Decadal Changes in Dry and Wet Heatwaves in Eastern China: Spatial Patterns and Risk Assessment, ADVANCES IN ATMOSPHERIC SCIENCES.  doi: 10.1007/s00376-024-3261-4
    [8] Chujie GAO, Gen LI, 2023: Enhanced Seasonal Predictability of Spring Soil Moisture over the Indo-China Peninsula for Eastern China Summer Precipitation under Non-ENSO Conditions, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 1632-1648.  doi: 10.1007/s00376-023-2361-x
    [9] Jingrui YAN, Wenjun ZHANG, Suqiong HU, Feng JIANG, 2024: Different ENSO Impacts on Eastern China Precipitation Patterns in Early and Late Winter Associated with Seasonally-Varying Kuroshio Anticyclonic Anomalies, ADVANCES IN ATMOSPHERIC SCIENCES, 41, 1691-1703.  doi: 10.1007/s00376-023-3196-1
    [10] Zhiyan ZUO, Renhe ZHANG, 2016: Influence of Soil Moisture in Eastern China on the East Asian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 151-163.  doi: 10.1007/s00376-015-5024-8
    [11] YUAN Weihua, YU Rucong, LI Jian, 2013: Changes in the Diurnal Cycles of Precipitation over Eastern China in the Past 40 Years, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 461-467.  doi: 10.1007/s00376-012-2092-x
    [12] Zhang Renhe, Akimasa Sumi, Masahide Kimoto, 1999: A Diagnostic Study of the Impact of El Nino on the Precipitation in China, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 229-241.  doi: 10.1007/BF02973084
    [13] LIU Yimin, BAO Qing, DUAN Anmin, QIAN Zheng'an, WU Guoxiong, 2007: Recent Progress in the Impact of the Tibetan Plateau on Climate in China, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 1060-1076.  doi: 10.1007/s00376-007-1060-3
    [14] Ni Yunqi, Lin Wuyin, Wang Wanqiu, Yuan Chongguang, Zhang Qin, 1993: Numerical Study for Potential Predictability of Short-Term Anomalous Climate Change Caused by El Nino, ADVANCES IN ATMOSPHERIC SCIENCES, 10, 1-10.  doi: 10.1007/BF02656949
    [15] Shi Neng, Luo Boliang, 1991: Telecorrelation of the 500 hPa Polar Circulation and El Nino / SO with the Temperature Fields in China, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 289-298.  doi: 10.1007/BF02919611
    [16] Li Chongyin, 1988: ACTIONS OF TYPHOONS OVER THE WESTERN PACIFIC (INCLUDING THE SOUTH CHINA SEA) AND EL NINO, ADVANCES IN ATMOSPHERIC SCIENCES, 5, 107-116.  doi: 10.1007/BF02657352
    [17] Yuanpu LI, Wenshou TIAN, 2017: Different Impact of Central Pacific and Eastern Pacific El Niño on the Duration of Sudden Stratospheric Warming, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 771-782.  doi: 10.1007/s00376-017-6286-0
    [18] Gao Ge, Huang Chaoying, 2001: Climate Change and Its Impact on Water Resources in North China, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 718-732.  doi: 10.1007/BF03403497
    [19] ZHOU Mengzi, WANG Huijun, 2015: Potential Impact of Future Climate Change on Crop Yield in Northeastern China, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 889-897.  doi: 10.1007/s00376-014-4161-9
    [20] Song Yukuan, Chen Longxun, Dong Min, 1994: Numerical Simulation for the Impact of Deforestation on Climate in China and Its Neighboring Regions, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 212-223.  doi: 10.1007/BF02666547

Get Citation+

Export:  

Share Article

Manuscript History

Manuscript received: 10 May 2009
Manuscript revised: 10 May 2009
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

Delayed Impacts of the El Nino Episodes in the Central Pacific on the Summertime Climate Anomalies of Eastern China in 2003 and 2007

  • 1. Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190; School of Atmospheric Sciences, Nanjing University, Nanjing 210093;National Climate Center, Beijing 100081

Abstract: In the summers of 2003 and 2007, eastern China suffered similar climate disasters with severe flooding in the Huaihe River valley and heat waves in the southern Yangtze River delta and South China. Using SST data and outgoing longwave radiation (OLR) data from NOAA along with reanalysis data from NCEP/NCAR, the 2002/03 and 2006/07 El Nino episodes in the central Pacific and their delayed impacts on the following early summertime climate anomalies of eastern China were analyzed. The possible physical progresses behaved as follows: Both of the moderate El Nino episodes matured in the central equatorial Pacific during the early winter. The zonal wind anomalies near the sea surface of the west-central equatorial Pacific excited equatorial Kelvin waves propagating eastward and affected the evolution of the El Ni\~no episodes. From spring to early summer, the concurring anomalous easterly winds in the central equatorial Pacific and the end of upwelling Kelvin waves propagating eastward in the western equatorial Pacific, favored the equatorial warm water both of the SST and the subsurface temperature in the western Pacific. These conditions favored the warm state of the western equatorial Pacific in the early summer for both cases of 2003 and 2007. Due to the active convection in the western equatorial Pacific in the early summer and the weak warm SST anomalies in the tropical western Pacific from spring to early summer, the convective activities in the western Pacific warm pool showed the pattern in which the anomalous strong convection only appeared over the southern regions of the tropical western Pacific warm pool, which effects the meridional shift of the western Pacific subtropical high in the summer. The physical progress of the delayed impacts of the El Ni\~no episodes in the central equatorial Pacific and their decaying evolution on the climate anomalies in eastern China were interpreted through the key role of special pattern for the heat convection in the tropical western Pacific warm pool and the response of the western North Pacific anomalous anticyclone.

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return