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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2020-11-01
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Online Access: | http://dx.doi.org/10.1080/16742834.2020.1808430 |
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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 |
work_keys_str_mv |
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