The Potential of Using Tree-Ring Data from Jeju Island to Reconstruct Climate in Subtropical Korea and the Western North Pacific

被引:7
|
作者
Zhang, Peng [1 ]
Jeong, Jee-Hoon [1 ]
Linderholm, Hans W. [2 ]
Jeong, Ji-Yoon [1 ]
Salo, Riikka [2 ]
Kim, Baek-Min [3 ]
Kim, Min-Seok [1 ]
机构
[1] Chonnam Natl Univ, Dept Oceanog, Gwangju, South Korea
[2] Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden
[3] Pukyong Natl Univ, Dept Environm Atmospher Sci, Busan, South Korea
基金
新加坡国家研究基金会; 瑞典研究理事会;
关键词
Dendroclimatology; Jeju Island; Korean fir; Korean red pine; Western North Pacific; SEA-SURFACE TEMPERATURE; PINUS-DENSIFLORA; VARIABILITY; UPGRADES; KUROSHIO; GROWTH; CHINA; PART;
D O I
10.1007/s13143-018-0089-9
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Annual rings from trees have been used to infer past climate variability beyond the observational records. Here, we assess if two conifer species from the humid subtropical island of Jeju, South Korea, can be used as proxies for past regional climate variability and large-scale ocean current variability, such as the Kuroshio Current, over the Western North Pacific. Korean red pine (Pinus densiflora) and Korean fir (Abies koreana) were sampled close to their altitudinal limits of distribution on the southern slopes of the volcano Mt. Halla at 1320m and 1640ma.s.l., respectively. Comparison with climate variables from nearby meteorological stations indicated a significant positive association between temperature in January/April and Korean red pine growth, which suggests that the red pine can be used to reconstruct mid-winter/spring temperatures back in time. Positive correlations were also found between the tree-ring growth and October (for Korean fir) and January (for Korean red pine) precipitation. Moreover, pine tree growth showed significant multi-month associations with sea surface temperatures over the Western North Pacific and variability of the Kuroshio Extension. The results suggest that subtropical trees from South Korea can be used as indicators of past climate variability on local to regional scales, and possibly also to infer the past variability of the Kuroshio Current in the Western North Pacific.
引用
收藏
页码:293 / 301
页数:9
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