Early Summer Temperature Variation Recorded by Earlywood Width in the Northern Boundary of Pinus taiwanensis Hayata in Central China and Its Linkages to the Indian and Pacific Oceans

Meng Peng; Xuan Li; Jianfeng Peng; Jiayue Cui; Jingru Li; Yafei Wei; Xiaoxu Wei; Jinkuan Li

doi:10.3390/biology11071077

Early Summer Temperature Variation Recorded by Earlywood Width in the Northern Boundary of Pinus taiwanensis Hayata in Central China and Its Linkages to the Indian and Pacific Oceans

Biology (Basel). 2022 Jul 19;11(7):1077. doi: 10.3390/biology11071077.

Authors

Meng Peng¹, Xuan Li¹, Jianfeng Peng^{1

2

3}, Jiayue Cui¹, Jingru Li¹, Yafei Wei^{1

2}, Xiaoxu Wei¹, Jinkuan Li¹

Affiliations

¹ College of Geography and Environmental Science, Henan University, Kaifeng 475004, China.
² The Key Laboratory of Earth System Observation and Simulation of Henan Province, Kaifeng 475004, China.
³ National Demonstration Center for Environment and Planning, Henan University, Kaifeng 475004, China.

Abstract

The Tongbai Mountains are an ecologically sensitive region to climate change, where there lies a climatic transitional zone from a subtropical to a warm−temperate monsoon climate. The northern boundary of Pinus taiwanensis Hayata is here; thus, climate information is well recorded in its tree rings. Based on developed earlywood width (EWW), latewood width (LWW) and total ring width (RW) chronologies (time period: 1887−2014 year) of Pinus taiwanensis Hayata in the Tongbai Mountains in central China, this paper analyzed characteristics of these chronologies and correlations between these chronologies and climate factors. The correlation results showed that earlywood width chronology contains more climate information than latewood width chronology and total ring width chronology, and mean temperature and mean maximum temperature in May−June were the main limiting factors for radial growth of Pinus taiwanensis Hayata. The highest significant value in all correlation analyses is −0.669 (p < 0.05) between earlywood width chronology and May−June mean temperature (TMJ) in the pre-mutation period (1958−2005) based on mutating in 2006. Thus, this paper reconstructed May−June mean temperature using earlywood width chronology from 1901 to 2005 (reliable period of earlywood width chronology is 1901−2014). The reconstructed May−June mean temperature experienced eight warmer periods and eight colder periods and also showed 2−3a cycle change over the past 105 years. The spatial correlation showed that the reconstructed series was representative of the May−June mean temperature variation in central and eastern China and significant positive/negative correlation with the sea surface temperature (SST) of the subtropical Pacific Ocean and the tropical Western Pacific Ocean and Indian Ocean from the previous October to the current June. This also indicated that May−June mean temperature periodic fluctuations might be related to the quasi-biennial oscillation (QBO) in the tropical Western Pacific Ocean and Indian Ocean. The results of this study have extended and supplemented the meteorological records of the Tongbai Mountains and have a guiding significance for forest tending and management in this area.

Keywords: Pinus taiwanensis Hayata; SST; Tongbai Mountains; temperature variation; tree-ring width.

Abstract

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