Author
Listed:
- Wei Shan
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China
Ministry of Education Observation and Research Station of Permafrost Geo-Environment System in Northeast China (MEORS-PGSNEC), Harbin 150040, China
Collaborative Innovation Centre for Permafrost Environment and Road Construction and Maintenance in Northeast China (CIC-PERCM), Harbin 150040, China
Low-Carbon Road Construction and Maintenance Engineering Technology Research Center in Northeast Permafrost Region of Heilongjiang Province (LCRCMET-HLJ), Harbin 150040, China)
- Guangchao Xu
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China)
- Yan Wang
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China)
- Lisha Qiu
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China)
- Ying Guo
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China
Ministry of Education Observation and Research Station of Permafrost Geo-Environment System in Northeast China (MEORS-PGSNEC), Harbin 150040, China
Collaborative Innovation Centre for Permafrost Environment and Road Construction and Maintenance in Northeast China (CIC-PERCM), Harbin 150040, China
Low-Carbon Road Construction and Maintenance Engineering Technology Research Center in Northeast Permafrost Region of Heilongjiang Province (LCRCMET-HLJ), Harbin 150040, China)
- Chengcheng Zhang
(Institute of Cold Regions Science and Engineering, Northeast Forestry University, Harbin 150040, China
Ministry of Education Observation and Research Station of Permafrost Geo-Environment System in Northeast China (MEORS-PGSNEC), Harbin 150040, China
Collaborative Innovation Centre for Permafrost Environment and Road Construction and Maintenance in Northeast China (CIC-PERCM), Harbin 150040, China
Low-Carbon Road Construction and Maintenance Engineering Technology Research Center in Northeast Permafrost Region of Heilongjiang Province (LCRCMET-HLJ), Harbin 150040, China)
Abstract
In the permafrost zone, the vegetation growth condition is closely related to the permafrost occurrence state. Changbai Mountain is the highest peak in Northeast China and is also a permafrost distribution area, where the vegetation shows an obvious vertical distribution pattern, and the alpine timberline has a clear boundary. The intersecting zone of alpine timberline is an ecologically fragile area that can be used as an external signal amplifier and is an important site for monitoring climate change. In this study, the surface frost number and alpine timberline in the Changbai Mountain area were analyzed through combining ground and remote-sensing data, using the freezing number model and support vector machine method. The results show that the distribution characteristics of alpine timberline and permafrost at elevation are correlated, there is a response mechanism of alpine timberline to the degradation of permafrost, and the upward migration rate of alpine timberline has increased in the last 20 years. The continuous degradation of permafrost will change the environment of vegetation growth, which, in turn, will affect the global carbon cycle process. Focusing on the state of permafrost will help us to understand climate change in depth, and we can respond to a series of impacts caused by ecological changes in cold regions in advance.
Suggested Citation
Wei Shan & Guangchao Xu & Yan Wang & Lisha Qiu & Ying Guo & Chengcheng Zhang, 2023.
"Response of Alpine Timberline to Permafrost Degradation on Changbai Mountain,"
Sustainability, MDPI, vol. 15(24), pages 1-16, December.
Handle:
RePEc:gam:jsusta:v:15:y:2023:i:24:p:16768-:d:1298855
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