CzechGlobe-Global Change Research Institute, Academy of Sciences of the Czech Republic, Belidla 4a, 603 00 Brno, Czech Republic; MendelGlobe-Global Change and Managed Ecosystems, Faculty of Forestry Mendel University, Zemědělská 1, 613 00 Brno, Czech Republic.
Geography and Environment, University of Southampton, Southampton SO17 1BJ, UK.
Sci Total Environ. 2016 Sep 1;563-564:486-95. doi: 10.1016/j.scitotenv.2016.04.124. Epub 2016 May 3.
Recent climate warming has shifted the timing of spring and autumn vegetation phenological events in the temperate and boreal forest ecosystems of Europe. In many areas spring phenological events start earlier and autumn events switch between earlier and later onset. Consequently, the length of growing season in mid and high latitudes of European forest is extended. However, the lagged effects (i.e. the impact of a warm spring or autumn on the subsequent phenological events) on vegetation phenology and productivity are less explored. In this study, we have (1) characterised extreme warm spring and extreme warm autumn events in Europe during 2003-2011, and (2) investigated if direct impact on forest phenology and productivity due to a specific warm event translated to a lagged effect in subsequent phenological events. We found that warmer events in spring occurred extensively in high latitude Europe producing a significant earlier onset of greening (OG) in broadleaf deciduous forest (BLDF) and mixed forest (MF). However, this earlier OG did not show any significant lagged effects on autumnal senescence. Needleleaf evergreen forest (NLEF), BLDF and MF showed a significantly delayed end of senescence (EOS) as a result of extreme warm autumn events; and in the following year's spring phenological events, OG started significantly earlier. Extreme warm spring events directly led to significant (p=0.0189) increases in the productivity of BLDF. In order to have a complete understanding of ecosystems response to warm temperature during key phenological events, particularly autumn events, the lagged effect on the next growing season should be considered.
最近的气候变暖已经改变了欧洲温带和北方森林生态系统中春季和秋季植被物候事件的时间。在许多地区,春季物候事件开始得更早,秋季事件在更早和更晚之间转换。因此,中高纬度欧洲森林的生长季节延长了。然而,对植被物候和生产力的滞后效应(即温暖的春季或秋季对随后的物候事件的影响)研究较少。在这项研究中,我们(1)描述了 2003-2011 年期间欧洲极端温暖的春季和秋季事件,以及(2)调查了由于特定温暖事件对森林物候和生产力的直接影响是否转化为随后物候事件的滞后效应。我们发现,高纬度欧洲广泛发生了更温暖的春季事件,导致阔叶林(BLDF)和混合林(MF)的绿化(OG)显著提前开始。然而,OG 提前并没有对秋季衰老产生任何显著的滞后效应。由于极端温暖的秋季事件,针叶常绿林(NLEF)、BLDF 和 MF 的衰老结束(EOS)明显延迟;并且在下一年的春季物候事件中,OG 开始得更早。极端温暖的春季事件直接导致 BLDF 生产力显著增加(p=0.0189)。为了全面了解生态系统在关键物候事件(特别是秋季事件)期间对暖温的反应,应该考虑下一个生长季节的滞后效应。