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DOI | 10.1175/JCLI-D-21-0214.1 |
Evaluation of CMIP6 Models over Two Third Pole Subregions with Contrasting Circulation Systems | |
Li, Ying; Wang, Chenghao; Su, Fengge | |
通讯作者 | Su, FG (通讯作者) |
发表日期 | 2021 |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
起始页码 | 9133 |
结束页码 | 9152 |
卷号 | 34期号:22 |
英文摘要 | Reliable simulations of historical and future climate are critical to assessing ecological and hydrological responses over the Third Pole region (TP; the area including the Himalaya-Hindu Kush mountain range and the Tibetan Plateau). In this study, we evaluate the historical and future temperature and precipitation simulations of 18 models from phase 6 of the Coupled Model Intercomparison Project (CMIP6) in southeastern TP (SETP) and the upstream area of the Amu Darya and Syr Darya (UAS) regions, two typical TP subregions dominated by the Indian summer monsoon system and westerlies, respectively. Comparison against station observations suggests that CMIP6 models generally capture the intra-annual variability and spatial pattern of historical climate over both subregions. However, the wetting and cold biases observed in CMIP5 still persist in CMIP6; annual temperature is underestimated by most models and annual precipitation is overestimated by all models. Multimodel average cold biases in SETP and UAS are 1.18 degrees and 0.32 degrees C, respectively, and wet biases in SETP and UAS are 119% and 46%, respectively. We further analyze climate projections under SSP1-2.6, SSP2-4.5, and SSP5-8.5 scenarios. Both SETP and UAS subregions are projected to experience significant warming in 2015-2100, with warming trends 34%-42% and 40%-50% higher than the global trend, respectively. Model projections suggest that the warming trend will slow down under SSP1-2.6 and SSP2-4.5 but further intensify under SSP5-8.5 in 2050-2100. Monsoon-dominated SETP is projected to experience a significant wetting trend stronger than UAS over the entire future period, especially in summer (cf. winter in westerlies-dominated UAS). Concurrently, a significant drying trend in summer is found in UAS during 2050-2100 under SSP5-8.5, suggesting the intensified uneven distributions of seasonal precipitation based on projections. |
关键词 | QINGHAI-TIBETAN PLATEAUCLIMATE-CHANGEREGIONAL CLIMATEWATER-RESOURCESPRECIPITATIONSIMULATIONSTEMPERATURESEASONALITYVARIABILITYRESOLUTION |
英文关键词 | Atmospheric circulation; Precipitation; Climate change; Temperature; Bias; Climate prediction; Ensembles; Model evaluation/performance |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000752646200018 |
来源期刊 | JOURNAL OF CLIMATE |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260389 |
推荐引用方式 GB/T 7714 | Li, Ying,Wang, Chenghao,Su, Fengge. Evaluation of CMIP6 Models over Two Third Pole Subregions with Contrasting Circulation Systems[J]. 中国科学院青藏高原研究所,2021,34(22). |
APA | Li, Ying,Wang, Chenghao,&Su, Fengge.(2021).Evaluation of CMIP6 Models over Two Third Pole Subregions with Contrasting Circulation Systems.JOURNAL OF CLIMATE,34(22). |
MLA | Li, Ying,et al."Evaluation of CMIP6 Models over Two Third Pole Subregions with Contrasting Circulation Systems".JOURNAL OF CLIMATE 34.22(2021). |
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