GSTDTAP  > 气候变化
DOI10.1007/s00382-016-3102-y
Historical and projected changes in the Southern Hemisphere Sub-tropical Jet during winter from the CMIP5 models
Chenoli, Sheeba Nettukandy1; Mazuki, Muhammad Yunus Ahmad1; Turner, John2; Abu Samah, Azizan1
2017
发表期刊CLIMATE DYNAMICS
ISSN0930-7575
EISSN1432-0894
出版年2017
卷号48
文章类型Article
语种英语
国家Malaysia; England
英文摘要

We present projected changes in the speed and meridional location of the Subtropical Jet (STJ) during winter using output of the Coupled Model Intercomparison Project Phase 5 (CMIP5) models. We use the ERA-Interim reanalysis dataset to evaluate the historical simulations of the STJ by 18 of the CMIP5 models for the period 1979-2012. Based on the climatology of the STJ from ERA-Interim, we selected the area of study as 70A degrees E-290A degrees E and 20A degrees S-40A degrees S, which is over the Indian and Southern Pacific Oceans, and 300-100 hPa to reduce altitude-related bias. An assessment of the ability of the CMIP5 models in simulating ENSO effects on the jet stream were carried out using standardized zonal wind anomalies at 300-100 hPa. Results show that 47 % of the CMIP5 models used in this study were able to simulate ENSO impacts realistically. In addition, it is more difficult for the models to reproduce the observed intensity of ENSO impacts than the patterns. The historical simulations of the CMIP5 models show a wide range of trends in meridional movement and jet strength, with a multi-model mean of 0.04A degrees A decade(-1) equatorward and 0.42 ms(-1) decade(-1) respectively. In contrast to the ERA-Interim analysis, 94 % of the CMIP5 models show a strengthening of the jet in the historical runs. Variability of the jet strength is significantly (5 %) linked to the sea surface temperature changes over the eastern tropical Pacific. The CMIP5 model projections with Representative Concentration Pathways (RCPs) 4.5 and 8.5 were used for analysis of changes of the STJ for the period 2011-2099. Based on the RCP 4.5 (RCP 8.5) scenario the multi-model mean trend of the 18 CMIP5 models project a statistically significant (5 % level) increase in jet strength by the end of the century of 0.29 ms(-1) decade(-1) (0.60 ms(-1) decade(-1)). Also, the mean meridional location of the jet is projected to shift poleward by 0.006A degrees A decade(-1) (0.042A degrees A decade(-1)) in 2099 during winter, with the only significant (5 %) trend being with RCP 8.5.


英文关键词Subtropical Jet Stream CMIP5 models El Nino Southern Oscillations Poleward shift Jet core Historical run Future projection Sea surface temperature ERA Interim
领域气候变化
收录类别SCI-E
WOS记录号WOS:000392307300038
WOS关键词ANTARCTIC SEA-ICE ; HADLEY-CELL ; EL-NINO ; SPLIT JET ; VARIABILITY ; STREAM ; ENSO ; TRENDS ; CLIMATOLOGY ; TEMPERATURE
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/35266
专题气候变化
作者单位1.Univ Malaya, Inst Postgrad Studies, Natl Antarct Res Ctr, Kuala Lumpur 50603, Malaysia;
2.British Antarctic Survey, Cambridge, England
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GB/T 7714
Chenoli, Sheeba Nettukandy,Mazuki, Muhammad Yunus Ahmad,Turner, John,et al. Historical and projected changes in the Southern Hemisphere Sub-tropical Jet during winter from the CMIP5 models[J]. CLIMATE DYNAMICS,2017,48.
APA Chenoli, Sheeba Nettukandy,Mazuki, Muhammad Yunus Ahmad,Turner, John,&Abu Samah, Azizan.(2017).Historical and projected changes in the Southern Hemisphere Sub-tropical Jet during winter from the CMIP5 models.CLIMATE DYNAMICS,48.
MLA Chenoli, Sheeba Nettukandy,et al."Historical and projected changes in the Southern Hemisphere Sub-tropical Jet during winter from the CMIP5 models".CLIMATE DYNAMICS 48(2017).
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