Title The Shift from Energy to Water Limitation in Local Canopy Height from Temperate to Tropical Forests in China
Authors Wang, Bojian
Fang, Shuai
Wang, Yunyun
Guo, Qinghua
Hu, Tianyu
Mi, Xiangcheng
Lin, Luxiang
Jin, Guangze
Coomes, David Anthony
Yuan, Zuoqiang
Ye, Ji
Wang, Xugao
Lin, Fei
Hao, Zhanqing
Affiliation Chinese Acad Sci, Inst Appl Ecol, CAS Key Lab Forest Ecol & Management, Shenyang 110016, Peoples R China
Univ Chinese Acad Sci, Beijing 100049, Peoples R China
Cent South Univ Forestry & Technol, Fac Life Sci & Technol, Changsha 410004, Peoples R China
Peking Univ, Coll Urban & Environm Sci, Inst Ecol, Beijing 100871, Peoples R China
Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China
Chinese Acad Sci, Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Kunming 650201, Yunnan, Peoples R China
Northeast Forestry Univ, Ctr Ecol Res, Harbin 150040, Peoples R China
Northeast Forestry Univ, Key Lab Sustainable Forest Ecosyst Management, Minist Educ, Harbin 150040, Peoples R China
Univ Cambridge, Conservat Res Inst, Dept Plant Sci, Cambridge CB2 3QZ, England
Northwestern Polytech Univ, Res Ctr Ecol & Environm Sci, Xian 710072, Peoples R China
Keywords TOPOGRAPHIC WETNESS INDEX
GLOBAL PATTERNS
TREE HEIGHT
HABITAT ASSOCIATIONS
SOLAR-RADIATION
DETERMINANTS
LIMITS
CLIMATE
BIOMASS
ASCENT
Issue Date May-2022
Publisher FORESTS
Abstract Canopy height greatly affects the biomass stock, carbon dynamics, and maintenance of biodiversity in forests. Previous research reported that the maximum forest canopy height (Hmax) at global and regional scales could be explained by variations in water or energy availability, that is, the water- or energy-related hypothesis. However, fundamental gaps remain in our understanding of how different drivers (i.e., water and energy) contribute to the Hmax at the local scale. In this study, we selected eight dynamic forest plots (20-30 ha) across a latitudinal gradient (from 21.6 degrees N to 48.1 degrees N) in China and measured the canopy structure using airborne light detection and ranging (LiDAR) data. Based on the LiDAR point cloud data, we extracted the maximum tree height (Hmax) in a 20 x 20 m quadrat as a proxy for canopy height, and the topographic wetness index (TWI) and digital terrain model-derived insolation (DTMI) were calculated as proxies for water and energy conditions. We used a linear mixed model and spatial simultaneous autoregressive error model to quantify how TWI and DTMI contributed to variations in Hmax at the local scale. We found that the positive effect of TWI was stronger in subtropical and tropical forests, highlighting that water was the main factor that drives the canopy height pattern in these regions. In contrast, although the effects of DTMI can be both positive and negative, its relative contribution was higher in temperate forest plots than in other forest types, supporting the idea that energy input is more critical for Hmax in temperate forests. Overall, our study revealed the directional change from energy to water limitation from temperate to subtropical and tropical forests. Our findings can offer important insights into forest management, especially under global climate change in the Anthropocene.
URI http://hdl.handle.net/20.500.11897/647167
DOI 10.3390/f13050639
Indexed SCI(E)
Appears in Collections: 城市与环境学院

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