Seasonal Outlook of China for Summer 2019

Authors

• PENG Jingbei, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• BUEH Cholaw, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• ZHENG Fei, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• CHEN Hong, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• LANG Xianmei, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• ZHAN Yanling, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• LIN Zhaohui, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• ZHANG Qingyun, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• LIN Renping, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• LI Chaofan, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• MA Jiehua, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• TIAN Baoqiang, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• BAO Qing, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• MU Songning, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• LU Riyu, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• ZHU Jiang, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

Keywords

summer precipitation anomalies; climate prediction; landing typhoon

Abstract

The ENSO prediction system of Institute of Atmospheric Physics, Chinese Academy of Sciences (IAP, CAS) predicts that El Niño conditions are likely to continue through the Northern Hemisphere spring and summer 2019. According to the seasonally averaged rainfall prediction of IAP, a wetter-than-normal condition is predicted for most parts of southern China, North parts of Northeast China and the Xinjiang Uygur Autonomous Region. The other parts of China will experience a drier-than-normal condition during the boreal summer. The center of less-than-normal precipitation is located in the Hetao area. The landing typhoon will be more than normal in the summer of 2019.

First page

693

Last Page

699

Language

Chinese

Publisher

Bulletin of Chinese Academy of Sciences

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial-No Derivative Works 4.0 International License.

References

孔锋.应急管理部成立背景下中国综合气象防灾减灾现状、挑战与发展机遇.中国减灾, 2019, 34(3):34-37.

林朝晖, 李旭, 赵彦, 等.中国科学院大气物理研究所短期气候预测系统的改进及其对1998年全国汛期旱涝形势的预测.气候与环境研究, 1998, 3(4):52-61.

卫捷, 杨辉, 孙淑清.西太平洋副热带高压东西位置异常与华北夏季酷暑.气象学报, 2004, 62(2):308-316.

邹旭恺, 高辉. 2006年夏季川渝高温干旱分析.气候变化研究进展, 2007, 3(3):149-153.

彭京备, 张庆云, 布和朝鲁. 2006年川渝地区高温干旱特征及其成因分析.气候与环境研究, 2007, 12(3):464-474.

史军, 丁一汇, 崔林丽.华东极端高温气候特征及成因分析.大气科学, 2009, 33(2):347-358.

Ji L R, Sun S Q. Model study on the interannual variability of Asian winter monsoon and its influence. Advances in Atmospheric Sciences, 1997, 14(1):1-22.

张庆云, 陶诗言, 陈烈庭.东亚夏季风指数的年际变化与东亚大气环流.气象学报, 2003, 61:559-568.

穆松宁, 周广庆.冬季欧亚大陆北部新增雪盖面积变化与中国夏季气候异常的关系.大气科学, 2010, 34(1):213-226.

Recommended Citation

Jingbei, PENG; Cholaw, BUEH; Fei, ZHENG; Hong, CHEN; Xianmei, LANG; Yanling, ZHAN; Zhaohui, LIN; Qingyun, ZHANG; Renping, LIN; Chaofan, LI; Jiehua, MA; Baoqiang, TIAN; Qing, BAO; Songning, MU; Riyu, LU; and Jiang, ZHU (2019) "Seasonal Outlook of China for Summer 2019," Bulletin of Chinese Academy of Sciences (Chinese Version): Vol. 34 : Iss. 6 , Article 9.
DOI: https://doi.org/10.16418/j.issn.1000-3045.2019.06.010
Available at: https://bulletinofcas.researchcommons.org/journal/vol34/iss6/9