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DOI | 10.1007/s00382-018-4085-7 |
On the role of horizontal resolution over the Tibetan Plateau in the REMO regional climate model | |
Xu, Jingwei1,2,3; Koldunov, Nikolay4,5; Remedio, Armelle Reca C.2; Sein, Dmitry V.5,6; Zhi, Xiefei1; Jiang, Xi1; Xu, Min7; Zhu, Xiuhua8; Fraedrich, Klaus1,3; Jacob, Daniela2 | |
2018-12-01 | |
发表期刊 | CLIMATE DYNAMICS |
ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2018 |
卷号 | 51页码:4525-4542 |
文章类型 | Article;Proceedings Paper |
语种 | 英语 |
国家 | Peoples R China; Germany; Russia |
英文摘要 | A number of studies have shown that added value is obtained by increasing the horizontal resolution of a regional climate model to capture additional fine-scale weather processes. However, the mechanisms leading to this added value are different over areas with complicated orographic features, such as the Tibetan Plateau (TP). To determine the role that horizontal resolution plays over the TP, a detailed comparison was made between the results from the REMO regional climate model at resolutions of 25 and 50km for the period 1980-2007. The model was driven at the lateral boundaries by the European Centre for Medium-Range Weather Forecasts Interim Reanalysis data. The experiments differ only in representation of topography, all other land parameters (e.g., vegetation characteristics, soil texture) are the same. The results show that the high-resolution topography affects the regional air circulation near the ground surface around the edge of the TP, which leads to a redistribution of the transport of atmospheric water vapor, especially over the Brahmaputra and Irrawaddy valleysthe main water vapor paths for the southern TPincreasing the amount of atmospheric water vapor transported onto the TP by about 5%. This, in turn, significantly decreases the temperature at 2m by >1.5 degrees C in winter in the high-resolution simulation of the southern TP. The impact of topography on the 2m temperature over the TP is therefore by influencing the transport of atmospheric water vapor in the main water vapor paths. |
英文关键词 | REMO regional climate model Validation High-resolution Added value Tibetan Plateau |
领域 | 气候变化 |
收录类别 | SCI-E ; ISTP |
WOS记录号 | WOS:000451725600036 |
WOS关键词 | ERA-INTERIM ; PRECIPITATION ; PERFORMANCE ; MONSOON ; SCHEME ; VARIABILITY ; SENSITIVITY ; SIMULATION ; HIMALAYA ; IMPACT |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/36112 |
专题 | 气候变化 |
作者单位 | 1.Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster,Joint Ctr Data Assimila, Minist Educ KLME,Collaborat Innovat Ctr Forecast, Joint Int Res Lab Climate & Environm Change ILCEC, Nanjing 210044, Jiangsu, Peoples R China; 2.HZG, Climate Serv Ctr Germany GERICS, D-20095 Hamburg, Germany; 3.Max Planck Inst Meteorol, Bundesstr 53, D-20146 Hamburg, Germany; 4.MARUM Ctr Marine Environm Sci, Bremen, Germany; 5.AWI, D-27568 Bremerhaven, Germany; 6.Russian Acad Sci, Shirshov Inst Oceanol, 36 Nahimovskiy Prospect, Moscow 117997, Russia; 7.Meteorol Bur Jiangsu Prov, Nanjing 210008, Jiangsu, Peoples R China; 8.Univ Hamburg, Ctr Earth Syst Res & Sustainabil, CliSAP, D-20144 Hamburg, Germany |
推荐引用方式 GB/T 7714 | Xu, Jingwei,Koldunov, Nikolay,Remedio, Armelle Reca C.,et al. On the role of horizontal resolution over the Tibetan Plateau in the REMO regional climate model[J]. CLIMATE DYNAMICS,2018,51:4525-4542. |
APA | Xu, Jingwei.,Koldunov, Nikolay.,Remedio, Armelle Reca C..,Sein, Dmitry V..,Zhi, Xiefei.,...&Jacob, Daniela.(2018).On the role of horizontal resolution over the Tibetan Plateau in the REMO regional climate model.CLIMATE DYNAMICS,51,4525-4542. |
MLA | Xu, Jingwei,et al."On the role of horizontal resolution over the Tibetan Plateau in the REMO regional climate model".CLIMATE DYNAMICS 51(2018):4525-4542. |
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