Cargando…

Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland

Based on the downscaling data of multi-model ensembles of 26 global climate models (GCMs) from the Coupled Model Intercomparison Project Phase 6, this study calculated the extreme climate indices defined by the Expert Team on Climate Change Detection and Indices and the warm winter extreme grade ind...

Descripción completa

Detalles Bibliográficos
Autores principales: Yi, Xiuping, Zou, Ling, Niu, Zigeng, Jiang, Daoyang, Cao, Qian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9141196/
https://www.ncbi.nlm.nih.gov/pubmed/35627439
http://dx.doi.org/10.3390/ijerph19105902
_version_ 1784715285822963712
author Yi, Xiuping
Zou, Ling
Niu, Zigeng
Jiang, Daoyang
Cao, Qian
author_facet Yi, Xiuping
Zou, Ling
Niu, Zigeng
Jiang, Daoyang
Cao, Qian
author_sort Yi, Xiuping
collection PubMed
description Based on the downscaling data of multi-model ensembles of 26 global climate models (GCMs) from the Coupled Model Intercomparison Project Phase 6, this study calculated the extreme climate indices defined by the Expert Team on Climate Change Detection and Indices and the warm winter extreme grade indices to explore winter climate response on the Chinese mainland under different shared socioeconomic pathways (SSPs) and representative concentration pathways. The results showed that the temperature in winter increased overall, with the highest temperature increases of 0.31 °C/10a (Celsius per decade) (SSP245) and 0.51 °C/10a (SSP585) and the lowest temperature increases of 0.30 °C/10a (SSP245) and 0.49 °C/10a (SSP585). Warm-related extreme weather events such as warm days and warm spell duration indices showed an increasing trend, whereas cold-related extreme weather events such as cold spell duration indices, cold nights, ice days, and frost days showed a decreasing trend. On the regional scale, the maximum temperature increased by more than 2 °C/10a (SSP245) and 0.4 °C/10a (SSP585), except in South China, and the minimum temperature increased faster in Qinghai-Tibet and Northeast China compared to elsewhere on the Chinese mainland. Compared with that under SSP585, the frequency and intensity of warm winters in the latter half of the 21st century were lower under SSP245. At the end of the 21st century, under the SSP245 scenario, warm winter frequency in most regions will be reduced to below 60%, but under the SSP585 scenario, it will be more than 80%. Population exposures all showed a downward trend, mainly due to the reduction of warm winter events and the decline of the population under the SSP245 and SSP585 scenarios, respectively. If the greenhouse gas emission path is controlled in the SSP245 scenario, the population exposure risk in warm winters can be decreased by 25.87%. This study observed a consistent warming trend on the Chinese mainland under all SSPs in the 21st century and found that stricter emission reduction policies can effectively decrease the population exposure to warm winters.
format Online
Article
Text
id pubmed-9141196
institution National Center for Biotechnology Information
language English
publishDate 2022
publisher MDPI
record_format MEDLINE/PubMed
spelling pubmed-91411962022-05-28 Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland Yi, Xiuping Zou, Ling Niu, Zigeng Jiang, Daoyang Cao, Qian Int J Environ Res Public Health Article Based on the downscaling data of multi-model ensembles of 26 global climate models (GCMs) from the Coupled Model Intercomparison Project Phase 6, this study calculated the extreme climate indices defined by the Expert Team on Climate Change Detection and Indices and the warm winter extreme grade indices to explore winter climate response on the Chinese mainland under different shared socioeconomic pathways (SSPs) and representative concentration pathways. The results showed that the temperature in winter increased overall, with the highest temperature increases of 0.31 °C/10a (Celsius per decade) (SSP245) and 0.51 °C/10a (SSP585) and the lowest temperature increases of 0.30 °C/10a (SSP245) and 0.49 °C/10a (SSP585). Warm-related extreme weather events such as warm days and warm spell duration indices showed an increasing trend, whereas cold-related extreme weather events such as cold spell duration indices, cold nights, ice days, and frost days showed a decreasing trend. On the regional scale, the maximum temperature increased by more than 2 °C/10a (SSP245) and 0.4 °C/10a (SSP585), except in South China, and the minimum temperature increased faster in Qinghai-Tibet and Northeast China compared to elsewhere on the Chinese mainland. Compared with that under SSP585, the frequency and intensity of warm winters in the latter half of the 21st century were lower under SSP245. At the end of the 21st century, under the SSP245 scenario, warm winter frequency in most regions will be reduced to below 60%, but under the SSP585 scenario, it will be more than 80%. Population exposures all showed a downward trend, mainly due to the reduction of warm winter events and the decline of the population under the SSP245 and SSP585 scenarios, respectively. If the greenhouse gas emission path is controlled in the SSP245 scenario, the population exposure risk in warm winters can be decreased by 25.87%. This study observed a consistent warming trend on the Chinese mainland under all SSPs in the 21st century and found that stricter emission reduction policies can effectively decrease the population exposure to warm winters. MDPI 2022-05-12 /pmc/articles/PMC9141196/ /pubmed/35627439 http://dx.doi.org/10.3390/ijerph19105902 Text en © 2022 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Yi, Xiuping
Zou, Ling
Niu, Zigeng
Jiang, Daoyang
Cao, Qian
Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title_full Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title_fullStr Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title_full_unstemmed Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title_short Multi-Model Ensemble Projections of Winter Extreme Temperature Events on the Chinese Mainland
title_sort multi-model ensemble projections of winter extreme temperature events on the chinese mainland
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9141196/
https://www.ncbi.nlm.nih.gov/pubmed/35627439
http://dx.doi.org/10.3390/ijerph19105902
work_keys_str_mv AT yixiuping multimodelensembleprojectionsofwinterextremetemperatureeventsonthechinesemainland
AT zouling multimodelensembleprojectionsofwinterextremetemperatureeventsonthechinesemainland
AT niuzigeng multimodelensembleprojectionsofwinterextremetemperatureeventsonthechinesemainland
AT jiangdaoyang multimodelensembleprojectionsofwinterextremetemperatureeventsonthechinesemainland
AT caoqian multimodelensembleprojectionsofwinterextremetemperatureeventsonthechinesemainland