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Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming

The Qilian Mountains are a climate-sensitive area in northwest China, and extreme precipitation events have an important impact on its ecological environment. Therefore, considering the global warming scenario, it is highly important to project the extreme precipitation indices over the Qilian Mount...

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Detalles Bibliográficos
Autores principales: Li, Yanzhao, Qin, Xiang, Jin, Zizhen, Liu, Yushuo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10049356/
https://www.ncbi.nlm.nih.gov/pubmed/36981875
http://dx.doi.org/10.3390/ijerph20064961
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author Li, Yanzhao
Qin, Xiang
Jin, Zizhen
Liu, Yushuo
author_facet Li, Yanzhao
Qin, Xiang
Jin, Zizhen
Liu, Yushuo
author_sort Li, Yanzhao
collection PubMed
description The Qilian Mountains are a climate-sensitive area in northwest China, and extreme precipitation events have an important impact on its ecological environment. Therefore, considering the global warming scenario, it is highly important to project the extreme precipitation indices over the Qilian Mountains in the future. This study is based on three CMIP6 models (CESM2, EC-Earth3, and KACE-1-0-G). A bias correction algorithm (QDM) was used to correct the precipitation outputs of the models. The eight extreme precipitation indices over the Qilian Mountains during the historical period and in the future were calculated using meteorological software (ClimPACT2), and the performance of the CMIP6 models to simulate the extreme precipitation indices of the Qilian Mountains in the historical period was evaluated. Results revealed that: (1) The corrected CMIP6 models could simulate the changes in extreme precipitation indices over the Qilian Mountains in the historical period relatively well, and the corrected CESM2 displayed better simulation as compared to the other two CMIP6 models. The CMIP6 models performed well while simulating R10mm (CC is higher than 0.71) and PRCPTOT (CC is higher than 0.84). (2) The changes in the eight extreme precipitation indices were greater with the enhancement of the SSP scenario. The growth rate of precipitation in the Qilian Mountains during the 21st century under SSP585 is significantly higher than the other two SSP scenarios. The increment of precipitation in the Qilian Mountains mainly comes from the increase in heavy precipitation. (3) The Qilian Mountains will become wetter in the 21st century, especially in the central and eastern regions. The largest increase in precipitation intensity will be observed in the western Qilian Mountains. Additionally, total precipitation will also increase in the middle and end of the 21st century under SSP585. Furthermore, the precipitation increment of the Qilian Mountains will increase with the altitude in the middle and end of the 21st century. This study aims to provide a reference for the changes in extreme precipitation events, glacier mass balance, and water resources in the Qilian Mountains during the 21st century.
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spelling pubmed-100493562023-03-29 Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming Li, Yanzhao Qin, Xiang Jin, Zizhen Liu, Yushuo Int J Environ Res Public Health Article The Qilian Mountains are a climate-sensitive area in northwest China, and extreme precipitation events have an important impact on its ecological environment. Therefore, considering the global warming scenario, it is highly important to project the extreme precipitation indices over the Qilian Mountains in the future. This study is based on three CMIP6 models (CESM2, EC-Earth3, and KACE-1-0-G). A bias correction algorithm (QDM) was used to correct the precipitation outputs of the models. The eight extreme precipitation indices over the Qilian Mountains during the historical period and in the future were calculated using meteorological software (ClimPACT2), and the performance of the CMIP6 models to simulate the extreme precipitation indices of the Qilian Mountains in the historical period was evaluated. Results revealed that: (1) The corrected CMIP6 models could simulate the changes in extreme precipitation indices over the Qilian Mountains in the historical period relatively well, and the corrected CESM2 displayed better simulation as compared to the other two CMIP6 models. The CMIP6 models performed well while simulating R10mm (CC is higher than 0.71) and PRCPTOT (CC is higher than 0.84). (2) The changes in the eight extreme precipitation indices were greater with the enhancement of the SSP scenario. The growth rate of precipitation in the Qilian Mountains during the 21st century under SSP585 is significantly higher than the other two SSP scenarios. The increment of precipitation in the Qilian Mountains mainly comes from the increase in heavy precipitation. (3) The Qilian Mountains will become wetter in the 21st century, especially in the central and eastern regions. The largest increase in precipitation intensity will be observed in the western Qilian Mountains. Additionally, total precipitation will also increase in the middle and end of the 21st century under SSP585. Furthermore, the precipitation increment of the Qilian Mountains will increase with the altitude in the middle and end of the 21st century. This study aims to provide a reference for the changes in extreme precipitation events, glacier mass balance, and water resources in the Qilian Mountains during the 21st century. MDPI 2023-03-11 /pmc/articles/PMC10049356/ /pubmed/36981875 http://dx.doi.org/10.3390/ijerph20064961 Text en © 2023 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
Li, Yanzhao
Qin, Xiang
Jin, Zizhen
Liu, Yushuo
Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title_full Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title_fullStr Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title_full_unstemmed Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title_short Future Projection of Extreme Precipitation Indices over the Qilian Mountains under Global Warming
title_sort future projection of extreme precipitation indices over the qilian mountains under global warming
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10049356/
https://www.ncbi.nlm.nih.gov/pubmed/36981875
http://dx.doi.org/10.3390/ijerph20064961
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AT jinzizhen futureprojectionofextremeprecipitationindicesovertheqilianmountainsunderglobalwarming
AT liuyushuo futureprojectionofextremeprecipitationindicesovertheqilianmountainsunderglobalwarming