Welcome to Chinese Journal of Applied Ecology! Today is Share:

Chinese Journal of Applied Ecology ›› 2020, Vol. 31 ›› Issue (2): 381-387.doi: 10.13287/j.1001-9332.202002.026

Previous Articles     Next Articles

Reconstruction of the March-April average maximum air temperature over 165 years based on Pinus tabuliformis tree-rings of Zhen’an County, Shaanxi Province, China

HUA Ya-wei, ZHANG Hong-juan, LIU Kang*   

  1. College of Urban and Environmental Science, Northwest Univer-sity/Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Xi’an 710127, China
  • Received:2019-10-08 Online:2020-02-15 Published:2020-02-15
  • Contact: * E-mail: liuk63@126.com
  • Supported by:
    This work was supported by the Special Project for Scientific Research of the National Forestry Public Welfare Industry (201304309).

Abstract: We used tree rings of Pinus tabuliformis sampled in the Muwang National Forest Park to establish a standardized chronology (STD) and calculated the correlation coefficients between the standardized chronology and climatic factors of Zhen’an meteorological station. With linear regression analysis, we reconstructed the March-April mean maximum temperature of Zhen’an over 165 years from 1853 to 2017. The highest correlation coefficient was observed between the standardized chronology and the March-April mean maximum temperature (r=0.596, n=60, P<0.01). The variance interpretation of the March-April mean maximum temperature reconstruction function was 33.2%, and the reconstruction function and results were credible and reliable. Warm years occurred 25 times and cold years occurred 29 times in the reconstruction sequence. The warm years were more accompanied by flood events, while the cold years were accompanied by more drought events. Temperature fluctuated obviously in the reconstruction sequence, with two cold periods (1902-1917 and 1953-2000) and four warm periods (1868-1892, 1917-1937, 1941-1953 and 2001-2012). The obvious periodic variations of 2-7, 8-15, 18-28, 75-96, and 100-125 years were found in the reconstruction sequence, in which the quasi-113, 88 and 22 years were the first, second and third main periods, respectively. These variations might potentially be the fingerprints of some climate change forces such as solar activity, monsoon and EI Niño-Southern Oscillation (ENSO) activity.