Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China

Using the historical simulations from 27 models in phase 5 of the Coupled Model Intercomparison Project (CMIP5) and 27 models in phase 6 (CMIP6), the authors evaluated the differences between CMIP5 and CMIP6 models in simulating the climate mean of extreme temperature over China through comparison w...

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Main Authors: Neng LUO, Yan GUO, Zhibo GAO, Kexin CHEN, Jieming CHOU
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2020-11-01
Series:Atmospheric and Oceanic Science Letters
Subjects:
Online Access:http://dx.doi.org/10.1080/16742834.2020.1808430
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spelling doaj-d63921e4a94c4886bdafe0f163cf3e5e2021-04-02T13:02:08ZengKeAi Communications Co., Ltd.Atmospheric and Oceanic Science Letters1674-28342376-61232020-11-0113658959710.1080/16742834.2020.18084301808430Assessment of CMIP6 and CMIP5 model performance for extreme temperature in ChinaNeng LUO0Yan GUO1Zhibo GAO2Kexin CHEN3Jieming CHOU4Beijing Normal UniversityBeijing Normal UniversityBeijing Normal UniversityChinese Academy of SciencesBeijing Normal UniversityUsing the historical simulations from 27 models in phase 5 of the Coupled Model Intercomparison Project (CMIP5) and 27 models in phase 6 (CMIP6), the authors evaluated the differences between CMIP5 and CMIP6 models in simulating the climate mean of extreme temperature over China through comparison with observations during 1979–2005. The CMIP6 models reproduce well the spatial distribution of annual maxima of daily maximum temperature (TXx), annual minima of daily minimum temperature (TNn), and frost days (FD). The model spread in CMIP6 is reduced relative to CMIP5 for some temperature indices, such as TXx, warm spell duration index (WSDI), and warm days (TX90p). The multimodel median ensembles also capture the observed trend of extreme temperature. However, the CMIP6 models still have low skill in capturing TX90p and cold nights (TN10p) and have obvious cold biases or warm biases over the Tibetan Plateau. The ability of individual models varies for different indices, although some models outperform the others in terms of the average of all indices considered for different models. By comparing different version models from the same organization, the updated CMIP6 models show no significant difference from their counterparts from CMIP5 for some models. Compared with individual models, the median ensembles show better agreement with the observations for temperature indices and their means.http://dx.doi.org/10.1080/16742834.2020.1808430temperature extremeschinacmip6cmip5model evaluation
collection DOAJ
language English
format Article
sources DOAJ
author Neng LUO
Yan GUO
Zhibo GAO
Kexin CHEN
Jieming CHOU
spellingShingle Neng LUO
Yan GUO
Zhibo GAO
Kexin CHEN
Jieming CHOU
Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
Atmospheric and Oceanic Science Letters
temperature extremes
china
cmip6
cmip5
model evaluation
author_facet Neng LUO
Yan GUO
Zhibo GAO
Kexin CHEN
Jieming CHOU
author_sort Neng LUO
title Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
title_short Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
title_full Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
title_fullStr Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
title_full_unstemmed Assessment of CMIP6 and CMIP5 model performance for extreme temperature in China
title_sort assessment of cmip6 and cmip5 model performance for extreme temperature in china
publisher KeAi Communications Co., Ltd.
series Atmospheric and Oceanic Science Letters
issn 1674-2834
2376-6123
publishDate 2020-11-01
description Using the historical simulations from 27 models in phase 5 of the Coupled Model Intercomparison Project (CMIP5) and 27 models in phase 6 (CMIP6), the authors evaluated the differences between CMIP5 and CMIP6 models in simulating the climate mean of extreme temperature over China through comparison with observations during 1979–2005. The CMIP6 models reproduce well the spatial distribution of annual maxima of daily maximum temperature (TXx), annual minima of daily minimum temperature (TNn), and frost days (FD). The model spread in CMIP6 is reduced relative to CMIP5 for some temperature indices, such as TXx, warm spell duration index (WSDI), and warm days (TX90p). The multimodel median ensembles also capture the observed trend of extreme temperature. However, the CMIP6 models still have low skill in capturing TX90p and cold nights (TN10p) and have obvious cold biases or warm biases over the Tibetan Plateau. The ability of individual models varies for different indices, although some models outperform the others in terms of the average of all indices considered for different models. By comparing different version models from the same organization, the updated CMIP6 models show no significant difference from their counterparts from CMIP5 for some models. Compared with individual models, the median ensembles show better agreement with the observations for temperature indices and their means.
topic temperature extremes
china
cmip6
cmip5
model evaluation
url http://dx.doi.org/10.1080/16742834.2020.1808430
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AT kexinchen assessmentofcmip6andcmip5modelperformanceforextremetemperatureinchina
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