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DOI | 10.3189/172756405781813294 |
An ice-core proxy for Antarctic circumpolar zonal wind intensity | |
Yan, Yuping; Mayewski, Paul A.; Kang, Shichang; Meyerson, Eric | |
发表日期 | 2005 |
ISSN | 0260-3055 |
起始页码 | 121 |
结束页码 | 130 |
卷号 | 41 |
英文摘要 | Using US National Centers for Environmental Prediction/US National Center for Atmospheric Research re-analysis data, we investigate the relationships between crustal ion (nssCa(2+)) concentrations from three West Antarctic ice cores, namely, Siple Dome (SD), ITASE00-1 (IT001) and ITASE01-5 (IT015), and primary components of the climate system, namely, air pressure/geopotential height, zonal (u) and meridional (v) wind strength. Linear correlation analyses between nssCa(2+) concentrations and both air-pressure and wind fields for the period of overlap between records indicate that the SD nssCa(2+) variation is positively correlated with spring circumpolar zonal wind, while IT001 nssCa(2+) has a positive correlation with circumpolar zonal wind throughout the year (r > 0.3, p < 0.01). Intensified Southern Westerlies circulation is conducive to transport of more crustal aerosols to both sites. Further correlation analyses between nssCa(2+) concentrations from SD and IT001 and atmospheric circulation suggest that the high inland plateau (represented by core IT001) is largely influenced by transport from the upper troposphere. IT015 nssCa(2+) is negatively correlated with westerly wind in October and November, suggesting that stronger westerly circulation may weaken the transport of crustal species to IT015. Correlations of nssCa(2+) from the three ice cores with the Antarctic Oscillation index are consistent with results developed from the wind-field investigation. In addition, calibration between nssCa(2+) concentration and the multivariate El Nino-Southern Oscillation (ENSO) index shows that crustal species transport to IT001 is enhanced during strong ENSO events. |
关键词 | HEMISPHERE ATMOSPHERIC CIRCULATIONOPERATIONAL NUMERICAL-ANALYSESSOUTHERN-HEMISPHEREEL-NINONORTHERN-HEMISPHERESPATIAL VARIABILITYEAST ANTARCTICASURFACE SNOWCLIMATEGREENLAND |
学科领域 | Geology |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000238029800018 |
来源期刊 | ANNALS OF GLACIOLOGY, VOL 41, 2005
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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/111446 |
推荐引用方式 GB/T 7714 | Yan, Yuping,Mayewski, Paul A.,Kang, Shichang,et al. An ice-core proxy for Antarctic circumpolar zonal wind intensity[J]. 中国科学院青藏高原研究所,2005,41. |
APA | Yan, Yuping,Mayewski, Paul A.,Kang, Shichang,&Meyerson, Eric.(2005).An ice-core proxy for Antarctic circumpolar zonal wind intensity.ANNALS OF GLACIOLOGY, VOL 41, 2005,41. |
MLA | Yan, Yuping,et al."An ice-core proxy for Antarctic circumpolar zonal wind intensity".ANNALS OF GLACIOLOGY, VOL 41, 2005 41(2005). |
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