El Niño teleconnections in CMIP5 models

被引:0
作者
Bryan C. Weare
机构
[1] University of California,Atmospheric Science Program, Land, Air and Water Resources
来源
Climate Dynamics | 2013年 / 41卷
关键词
El Niño; ENSO; CMIP5; Models; Teleconnections;
D O I
暂无
中图分类号
学科分类号
摘要
Teleconnections associated with warm El Niño/southern oscillation (ENSO) events in 20 climate model intercomparison project 5 (CMIP5) models have been compared with reanalysis observations. Focus has been placed on compact time and space indices, which can be assigned a specific statistical confidence. Nearly all of the models have surface temperature, precipitation and 250 hPa geopotential height departures in the Tropics that are in good agreement with the observations. Most of the models also have realistic anomalies of Northern Hemisphere near-surface temperature, precipitation and 500 hPa geopotential height. Model skill for these variables is significantly related to the ability of a model to accurately simulate Tropical 250 hPa height departures. Additionally, most models have realistic temperature and precipitation anomalies over North America, which are linked to a model’s ability to simulate Tropical 250 hPa and Northern Hemisphere 500 hPa height departures. The skills of temperature and precipitation departures over the Northern Hemisphere and North America are associated with the ability to realistically simulate realistic ENSO frequency and length. Neither horizontal nor vertical resolution differences for either the model atmosphere or ocean are significantly related at the 95 % level to variations in El Niño simulation quality. Overall, recent versions of earlier models have improved in their ability to simulate El Niño teleconnections. For instance, the average model skills of temperature and precipitation for the Tropics, Northern Hemisphere and North America for 11 CMIP5 models are all larger than those for prior versions.
引用
收藏
页码:2165 / 2177
页数:12
相关论文
共 50 条
[41]   Revisiting the Influence of ENSO on the Arctic Stratosphere in CMIP5 and CMIP6 Models [J].
Hu, Jinggao ;
Shen, Yifan ;
Deng, Jiechun ;
Jia, Yanpei ;
Wang, Zixu ;
Li, Anqi .
ATMOSPHERE, 2023, 14 (05)
[42]   Uncertainty of ENSO-amplitude projections in CMIP5 and CMIP6 models [J].
Beobide-Arsuaga, Goratz ;
Bayr, Tobias ;
Reintges, Annika ;
Latif, Mojib .
CLIMATE DYNAMICS, 2021, 56 (11-12) :3875-3888
[43]   Evaluation of the Antarctic Circumpolar Wave Simulated by CMIP5 and CMIP6 Models [J].
Lu, Zhichao ;
Zhao, Tianbao ;
Zhou, Weican .
ATMOSPHERE, 2020, 11 (09)
[44]   Comparison of Indian Ocean warming simulated by CMIP5 and CMIP6 models [J].
Li Jingyi ;
Su Jingzhi .
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2020, 13 (06) :604-611
[45]   An Evaluation of Precipitation in Dongting Lake Basin on CMIP5 Models [J].
Yin, Yiwen ;
Jiang, Shuai ;
Peng, Jie ;
Zhu, Hao ;
Ruan, Neng ;
Wang, Wei .
ATMOSPHERE, 2022, 13 (10)
[46]   Activity Characteristics of the East Asian Trough in CMIP5 Models [J].
Chen, Xiong ;
Liu, Xing ;
Li, Xin ;
Liu, Mingyang ;
Yang, Minghao .
ATMOSPHERE, 2018, 9 (02)
[47]   Winter and Summer Rossby Wave Sources in the CMIP5 Models [J].
Nie, Yu ;
Zhang, Yang ;
Yang, Xiu-Qun ;
Ren, Hong-Li .
EARTH AND SPACE SCIENCE, 2019, 6 (10) :1831-1846
[48]   Understanding MJO Teleconnections to the Southern Hemisphere Extratropics During El Niño, La Niña, and Neutral Years [J].
Roy, Raina ;
Arblaster, Julie M. ;
Wheeler, Matthew C. ;
Lim, Eun-Pa. .
GEOPHYSICAL RESEARCH LETTERS, 2025, 52 (09)
[49]   Diverse influences of spring Arctic Oscillation on the following winter El Nino-Southern Oscillation in CMIP5 models [J].
Zheng, Yuqiong ;
Chen, Shangfeng ;
Chen, Wen ;
Yu, Bin .
CLIMATE DYNAMICS, 2021, 56 (1-2) :275-297
[50]   Changes in Independency between Two Types of El Nino Events under a Greenhouse Warming Scenario in CMIP5 Models [J].
Ham, Yoo-Geun ;
Jeong, Yerim ;
Kug, Jong-Seong .
JOURNAL OF CLIMATE, 2015, 28 (19) :7561-7575