Seasonal Outlook for 2018 Summer over China

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
YU Yue, 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
WANG Jun, 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

Document Type

Article

Abstract

The ENSO prediction system of Institute of Atmospheric Physics, Chinese Academy of Sciences (IAPCAS) predicts that La Niñalike condition will disappear by mid-spring, then the tropical Pacific will return to a normal state by summer. According to the seasonally averaged rainfall prediction of IAP, a wetter-than-normal condition is predicted for most parts of southeastern China, North China, south part of Northeast China, east part of Northwest China. The other parts of China will experience a drier-than-normal condition during the boreal summer. The landing Typhoon will be less than normal in 2018.

First page

630

Last Page

636

Language

Chinese

Publisher

Bulletin of Chinese Academy of Sciences

References

吴吉东, 傅宇, 张洁, 等. 1949—2013年中国气象灾害灾情变化趋势分析.自然资源学报, 2014, 29(9):1520-1530.

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.

国家气候中心. 全球海洋监测预测简报(2018年第23期). [2018-05-18].

张庆云, 陶诗言, 陈烈庭. 2003: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(5):559-568.

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.

卫捷, 孙建华.华北地区夏季高温闷热天气特征的分析.气候与环境研究, 2007, 12(3):453-463.

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.

张顺利, 陶诗言.青藏高原积雪对亚洲夏季风影响的诊断及数值研究.大气科学, 2001, 25(3):372-390.

陈烈庭.青藏高原异常雪盖和ENSO在1998年长江流域洪涝中的作用.大气科学, 2001, 25(2):184-192.

陈烈庭, 吴仁广.青藏高原雪盖与我国季风雨年际和年代际变化的关系, 东亚季风和中国暴雨:庆贺陶诗言院士八十华诞.北京:气象出版社, 1998:230-239.

许立言, 武炳义.欧亚大陆春季融雪量与东亚夏季风的可能联系.大气科学, 2012, 36(6):1180-1190.

杨秋明.冬半年欧亚雪盖变化对东亚环流的影响.气象学报, 1998, 56(5):627-634.

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; Yue, YU; Zhaohui, LIN; Qingyun, ZHANG; Renping, LIN; Chaofan, LI; Jun, WANG; Baoqiang, TIAN; Qing, BAO; Songning, MU; Riyu, LU; and Jiang, ZHU (2018) "Seasonal Outlook for 2018 Summer over China," Bulletin of Chinese Academy of Sciences (Chinese Version): Vol. 33 : Iss. 6 , Article 12.
DOI: https://doi.org/10.16418/j.issn.1000-3045.2018.06.012
Available at: https://bulletinofcas.researchcommons.org/journal/vol33/iss6/12