An assessment of Indo-Pacific oceanic channel dynamics in the FGOALS-g2 coupled climate system model | |
Xu Tengfei1,2; Yuan Dongliang1![]() ![]() ![]() | |
刊名 | ADVANCES IN ATMOSPHERIC SCIENCES
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2013-07-01 | |
卷号 | 30期号:4页码:997-1016 |
关键词 | Indian Ocean Dipole ENSO oceanic channel FGOALS-g2 Indonesian Throughflow |
ISSN号 | 0256-1530 |
通讯作者 | Yuan, DL |
中文摘要 | Lag correlations of sea surface temperature anomalies (SSTAs), sea surface height anomalies (SSHAs), subsurface temperature anomalies, and surface zonal wind anomalies (SZWAs) produced by the Flexible Global Ocean-Atmosphere-Land System model: Grid-point Version 2 (FGOALS-g2) are analyzed and compared with observations. The insignificant, albeit positive, lag correlations between the SSTAs in the southeastern tropical Indian Ocean (STIO) in fall and the SSTAs in the central-eastern Pacific cold tongue in the following summer through fall are found to be not in agreement with the observational analysis. The model, however, does reproduce the significant lag correlations between the SSHAs in the STIO in fall and those in the cold tongue at the one-year time lag in the observations. These, along with the significant lag correlations between the SSTAs in the STIO in fall and the subsurface temperature anomalies in the equatorial Pacific vertical section in the following year, suggest that the Indonesian Throughflow plays an important role in propagating the Indian Ocean anomalies into the equatorial Pacific Ocean. Analyses of the interannual anomalies of the Indonesian Throughflow transport suggest that the FGOALS-g2 climate system simulates, but underestimates, the oceanic channel dynamics between the Indian and Pacific Oceans. FGOALS-g2 is shown to produce lag correlations between the SZWAs over the western equatorial Pacific in fall and the cold tongue SSTAs at the one-year time lag that are too strong to be realistic in comparison with observations. The analyses suggest that the atmospheric bridge over the Indo-Pacific Ocean is overestimated in the FGOALS-g2 coupled climate model. |
英文摘要 | Lag correlations of sea surface temperature anomalies (SSTAs), sea surface height anomalies (SSHAs), subsurface temperature anomalies, and surface zonal wind anomalies (SZWAs) produced by the Flexible Global Ocean-Atmosphere-Land System model: Grid-point Version 2 (FGOALS-g2) are analyzed and compared with observations. The insignificant, albeit positive, lag correlations between the SSTAs in the southeastern tropical Indian Ocean (STIO) in fall and the SSTAs in the central-eastern Pacific cold tongue in the following summer through fall are found to be not in agreement with the observational analysis. The model, however, does reproduce the significant lag correlations between the SSHAs in the STIO in fall and those in the cold tongue at the one-year time lag in the observations. These, along with the significant lag correlations between the SSTAs in the STIO in fall and the subsurface temperature anomalies in the equatorial Pacific vertical section in the following year, suggest that the Indonesian Throughflow plays an important role in propagating the Indian Ocean anomalies into the equatorial Pacific Ocean. Analyses of the interannual anomalies of the Indonesian Throughflow transport suggest that the FGOALS-g2 climate system simulates, but underestimates, the oceanic channel dynamics between the Indian and Pacific Oceans. FGOALS-g2 is shown to produce lag correlations between the SZWAs over the western equatorial Pacific in fall and the cold tongue SSTAs at the one-year time lag that are too strong to be realistic in comparison with observations. The analyses suggest that the atmospheric bridge over the Indo-Pacific Ocean is overestimated in the FGOALS-g2 coupled climate model. |
学科主题 | Meteorology & Atmospheric Sciences |
WOS标题词 | Science & Technology ; Physical Sciences |
类目[WOS] | Meteorology & Atmospheric Sciences |
研究领域[WOS] | Meteorology & Atmospheric Sciences |
关键词[WOS] | SEA-SURFACE TEMPERATURE ; TROPICAL INDIAN-OCEAN ; COMMUNITY LAND MODEL ; ATMOSPHERIC BRIDGE ; VERSION 2 ; ENSO ; VARIABILITY ; DIPOLE ; DESIGN ; WAVE |
收录类别 | SCI |
原文出处 | 10.1007/s00376-013-2131-2 |
语种 | 英语 |
WOS记录号 | WOS:000320561800004 |
公开日期 | 2014-07-17 |
内容类型 | 期刊论文 |
源URL | [http://ir.qdio.ac.cn/handle/337002/16391] ![]() |
专题 | 海洋研究所_海洋环流与波动重点实验室 海洋研究所_海洋地质与环境重点实验室 |
通讯作者 | Yuan, DL |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Xu Tengfei,Yuan Dongliang,Yu Yongqiang,et al. An assessment of Indo-Pacific oceanic channel dynamics in the FGOALS-g2 coupled climate system model[J]. ADVANCES IN ATMOSPHERIC SCIENCES,2013,30(4):997-1016. |
APA | Xu Tengfei,Yuan Dongliang,Yu Yongqiang,Zhao Xia,&Yuan, DL.(2013).An assessment of Indo-Pacific oceanic channel dynamics in the FGOALS-g2 coupled climate system model.ADVANCES IN ATMOSPHERIC SCIENCES,30(4),997-1016. |
MLA | Xu Tengfei,et al."An assessment of Indo-Pacific oceanic channel dynamics in the FGOALS-g2 coupled climate system model".ADVANCES IN ATMOSPHERIC SCIENCES 30.4(2013):997-1016. |
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