Spring phenology at different altitudes is becoming more uniform under global warming in Europe

• Published in: Global change biology Vol. 24; no. 9; pp. 3969 - 3975
• Main Authors: Chen, Lei, Huang, Jian‐Guo, Ma, Qianqian, Hänninen, Heikki, Rossi, Sergio, Piao, Shilong, Bergeron, Yves
• Format: Journal Article
• Language: English
• Published: England Blackwell Publishing Ltd 01.09.2018
• Subjects: altitude; Chilling; Climate change; cold treatment; Cooling; Elevation; elevation‐dependent warming; Europe; Global warming; leaf unfolding; Leaves; Phenology; Plant species; Regions; Spring; temperature; Temperature effects; trees; Europe; leaf unfolding; elevation-dependent warming; phenology; climate change
• ISSN: 1354-1013; 1365-2486; 1365-2486
• DOI: 10.1111/gcb.14288

Under current global warming, high‐elevation regions are expected to experience faster warming than low‐elevation regions. However, due to the lack of studies based on long‐term large‐scale data, the relationship between tree spring phenology and the elevation‐dependent warming is unclear. Using 652k records of leaf unfolding of five temperate tree species monitored during 1951–2013 in situ in Europe, we discovered a nonlinear trend in the altitudinal sensitivity (SA, shifted days per 100 m in altitude) in spring phenology. A delayed leaf unfolding (2.7 ± 0.6 days per decade) was observed at high elevations possibly due to decreased spring forcing between 1951 and 1980. The delayed leaf unfolding at high‐elevation regions was companied by a simultaneous advancing of leaf unfolding at low elevations. These divergent trends contributed to a significant increase in the SA (0.36 ± 0.07 days 100/m per decade) during 1951–1980. Since 1980, the SA started to decline with a rate of −0.32 ± 0.07 days 100/m per decade, possibly due to reduced chilling at low elevations and improved efficiency of spring forcing in advancing the leaf unfolding at high elevations, the latter being caused by increased chilling. Our results suggest that due to both different temperature changes at the different altitudes, and the different tree responses to these changes, the tree phenology has shifted at different rates leading to a more uniform phenology at different altitudes during recent decades. A delayed leaf unfolding was observed at high elevations possibly due to decreased spring forcing between 1951 and 1980. The delayed leaf unfolding at high‐elevation regions was companied by a simultaneous advanced leaf unfolding at low elevations. Our results suggest that due to both different temperature changes at the different altitudes, and the different tree responses to these changes, the tree phenology has shifted at different rates leading to a more uniform phenology at different altitudes during recent decades