Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s00704-020-03093-8 |
Added value of the regionally coupled model ROM in the East Asian summer monsoon modeling | |
Zhu, Shoupeng1,2,3; Remedio, Armelle Reca C.2; Sein, Dmitry V.4,5; Sielmann, Frank6; Ge, Fei3,7; Xu, Jingwei1; Peng, Ting1; Jacob, Daniela2; Fraedrich, Klaus1,3; Zhi, Xiefei1 | |
通讯作者 | Zhi, Xiefei |
来源期刊 | THEORETICAL AND APPLIED CLIMATOLOGY
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ISSN | 0177-798X |
EISSN | 1434-4483 |
出版年 | 2020 |
卷号 | 140期号:1-2页码:375-387 |
英文摘要 | The performance of the regional atmosphere-ocean coupled model ROM (REMO-OASIS-MPIOM) is compared with its atmospheric component REMO in simulating the East Asian summer monsoon (EASM) during the time period 1980-2012 with the following results being obtained. (1) The REMO model in the standalone configuration with the prescribed sea surface conditions produces stronger low-level westerlies associated with the South Asian summer monsoon, an eastward shift of the western Pacific subtropical high (WPSH) and a wetter lower troposphere, which jointly lead to moisture pathways characterized by stronger westerlies with convergence eastward to the western North Pacific (WNP). As a consequence, the simulated precipitation in REMO is stronger over the ocean and weaker over the East Asian continent than in the observational datasets. (2) Compared with the REMO results, lower sea surface temperatures (SSTs) feature the ROM simulation with enhanced air-sea exchanges from the intensified low-level winds over the subtropical WNP, generating an anomalous low-level anticyclone and hence improving simulations of the low-level westerlies and WPSH. With lower SSTs, ROM produces less evaporation over the ocean, inducing a drier lower troposphere. As a result, the precipitation simulated by ROM is improved over the East Asian continent but with dry biases over the WNP. (3) Both models perform fairly well for the upper level circulation. In general, compared with the standalone REMO model, ROM improves simulations of the circulation associated with the moisture transport in the lower- to mid-troposphere and reproduces the observed EASM characteristics, demonstrating the advantages of the regionally coupled model ROM in regions where air-sea interactions are highly relevant for the East Asian climate. |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China ; Germany ; Russia |
开放获取类型 | Green Published |
收录类别 | SCI-E |
WOS记录号 | WOS:000521505600027 |
WOS关键词 | INTERANNUAL VARIABILITY ; GLOBAL PRECIPITATION ; TIBETAN PLATEAU ; CLIMATE-CHANGE ; WATER-BUDGET ; REMO ; SIMULATION ; CHINA ; SEA ; PERFORMANCE |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | 南京信息工程大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/315663 |
作者单位 | 1.Nanjing Univ Informat Sci & Technol, Minist Educ, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Key Lab Meteorol Disasters, Nanjing 210044, Peoples R China; 2.Helmholtz Ctr Mat & Coastal Res, Climate Serv Ctr Germany, D-20095 Hamburg, Germany; 3.Max Planck Inst Meteorol, D-20146 Hamburg, Germany; 4.Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, D-27570 Bremerhaven, Germany; 5.Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia; 6.Univ Hamburg, Meteorol Inst, D-20146 Hamburg, Germany; 7.Chengdu Univ Informat Technol, Sch Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610225, Peoples R China |
推荐引用方式 GB/T 7714 | Zhu, Shoupeng,Remedio, Armelle Reca C.,Sein, Dmitry V.,et al. Added value of the regionally coupled model ROM in the East Asian summer monsoon modeling[J]. 南京信息工程大学,2020,140(1-2):375-387. |
APA | Zhu, Shoupeng.,Remedio, Armelle Reca C..,Sein, Dmitry V..,Sielmann, Frank.,Ge, Fei.,...&Zhi, Xiefei.(2020).Added value of the regionally coupled model ROM in the East Asian summer monsoon modeling.THEORETICAL AND APPLIED CLIMATOLOGY,140(1-2),375-387. |
MLA | Zhu, Shoupeng,et al."Added value of the regionally coupled model ROM in the East Asian summer monsoon modeling".THEORETICAL AND APPLIED CLIMATOLOGY 140.1-2(2020):375-387. |
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