Do Extreme Climate Events Cause the Degradation of Malus sieversii Forests in China?

Qianjuan Shan; Hongbo Ling; Hangzheng Zhao; Mengyi Li; Zikang Wang; Guangpeng Zhang

doi:10.3389/fpls.2021.608211

Do Extreme Climate Events Cause the Degradation of Malus sieversii Forests in China?

Front Plant Sci. 2021 Jun 16:12:608211. doi: 10.3389/fpls.2021.608211. eCollection 2021.

Authors

Qianjuan Shan^{1

2}, Hongbo Ling^{1

2

3}, Hangzheng Zhao⁴, Mengyi Li⁵, Zikang Wang^{1

2}, Guangpeng Zhang^{1

2}

Affiliations

¹ State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China.
² University of Chinese Academy of Sciences, Beijing, China.
³ Xinjiang Aksu Oasis Agro-Ecosystem Observation and Experiment Station, Urumqi, China.
⁴ School of Chemical and Environmental Engineering, China University of Mining and Technology, Beijing, China.
⁵ School of Civil Engineering, Tianjin University, Tianjin, China.

Abstract

Frequent extreme climate events have attracted considerable attention around the world. Malus sieversii in Xinjiang is the ancestor of cultivated apple, and it is mainly distributed in the Ili river valley at end of the Tianshan Mountains. Wild fruit forests have been degraded, but the cause remains unclear. In order to identify whether extreme climate events caused this degradation reanalysis data and atmospheric circulation indices were used to determine the trends and the reasons for extreme climate changes. Subsequently, we further investigated the effect of extreme climate events on wild fruit forest using characteristics of extreme climate indices and tree-ring chronology. We found increasing trends in both extreme precipitation and warm indices, and decreasing trends in cool indices. Extreme climate events were mainly associated with the Atlantic Multidecadal Oscillation (AMO). Analysis of data of wind and geopotential height field at 500 hPa showed that strengthening wind, increasing geopotential height, cyclone and anti-cyclone circulation drivers contributed to extreme climate events. In the non-degraded region, there were significant positive correlations between tree-ring chronology and both extreme precipitation and extreme warm indices (except for warm spell duration indicator). The other extreme indices (except for heavy rain days) had a large correlation range with tree-rings in a 4-8-year period. These results indicated that extreme precipitation and extreme warm indices intensified M. sieversii growth of the non-degraded region on multi-time scales. In contrast, the degraded region showed insignificant negative relationship between tree-ring chronology and both extreme precipitation and extreme warm indices [except for warm spell duration index (WSDI)], and significant negative correlations in a 4-8-year period were detected between tree-ring chronology and most of the extreme precipitation indices, including heavy rain days, very wet days, cold spell duration indicator, simple precipitation intensity index (SDII), and annual total precipitation. Under the long disturbance of inappropriate anthropic activities, extreme climate has caused the outbreak of pests and diseases resulting in the degeneration of wild fruit forest. Our study provides scientific guidance for the ecosystem conservation in wild fruit forest in China, and also across the region.

Keywords: anthropogenic impact; atmospheric circulation; dendrochronology of Malus sieversii trees; extreme climate indices; the degraded wild fruit forest.