Reconstruction of the springtime East Asian Subtropical Jet and Western Pacific pattern from a millennial-length Taiwanese tree-ring chronology

被引:9
|
作者
Wright, W. E. [1 ]
Guan, B. T. [2 ]
Tseng, Y. -H. [3 ]
Cook, E. R. [4 ]
Wei, K. -Y. [5 ]
Chang, S. -T. [2 ]
机构
[1] Univ Arizona, Tree Ring Res Lab, Tucson, AZ 85721 USA
[2] Natl Taiwan Univ, Sch Forestry & Resource Conservat, Taipei 10764, Taiwan
[3] Natl Ctr Atmospher Res, Earth Syst Lab, Boulder, CO 80307 USA
[4] Lamont Doherty Earth Observ, Biol & Paleoenvironm, Palisades, NY USA
[5] Natl Taiwan Univ, Dept Geosci, Taipei 10764, Taiwan
关键词
Tree-ring; Cloud forest; East Asian Subtropical jet; Western Pacific pattern; North Pacific storm track; Temperature; ATMOSPHERIC CIRCULATION; CLOUD FOREST; CLIMATE; VARIABILITY; MONSOON; REANALYSIS; TEMPERATURES; OSCILLATION; MECHANISMS; SIGNALS;
D O I
10.1007/s00382-014-2402-3
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The East Asian subtropical jet (EAJ) and the closely related Western Pacific pattern (WP) are among the most important features in global atmospheric dynamics, but little is known about their long-term variability. This study presents reconstructions of the Spring EAJ index (EAJI) and the Spring WP index (WPI) based on significant relationships identified between mean values for these features and a millennial length tree-ring width chronology of Chamaecyparis obtusa var. formosana, a high-mountain cloud forest species from northeastern Taiwan. Tree-ring based reconstructions of high pass filtered versions of the EAJI and WPI (EAJI 5YR and WPI 5YR) presented herein explain 42 and 31 % of the WPI 5YR and EAJI 5YR, respectively, and display acceptable reliability back to A.D. 1237. A significant trend present in the long-term variance of the reconstructed EAJI and WPI after A.D. 1860 suggests long-term increasing variability in the spring mean latitudinal placement and/or the strength/breadth of the EAJ core region near Taiwan and Japan and in the trajectory of the EAJ over the North Pacific. Related features affected by changes in the EAJ include the North Pacific storm track and Asian Dust transport.
引用
收藏
页码:1645 / 1659
页数:15
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