4.8 Article

Differentiating drought legacy effects on vegetation growth over the temperate Northern Hemisphere

期刊

GLOBAL CHANGE BIOLOGY
卷 24, 期 1, 页码 504-516

出版社

WILEY
DOI: 10.1111/gcb.13920

关键词

drought legacy effect; drought resilience; ecohydrological responses; extreme drought; plant functional groups; rooting system; stomatal conductance; vegetation growth

资金

  1. Schweizerischer Nationalfonds zur Forderung der Wissenschaftlichen Forschung [P300P2_154543]
  2. National Natural Science Foundation of China [41390462, 41530747, 41571038]
  3. State Key Laboratory of Earth Surface Processes and Resource Ecology [2017-ZY-06]
  4. EU [640176]

向作者/读者索取更多资源

In view of future changes in climate, it is important to better understand how different plant functional groups (PFGs) respond to warmer and drier conditions, particularly in temperate regions where an increase in both the frequency and severity of drought is expected. The patterns and mechanisms of immediate and delayed impacts of extreme drought on vegetation growth remain poorly quantified. Using satellite measurements of vegetation greenness, in-situ tree-ring records, eddy-covariance CO2 and water flux measurements, and meta-analyses of source water of plant use among PFGs, we show that drought legacy effects on vegetation growth differ markedly between forests, shrubs and grass across diverse bioclimatic conditions over the temperate Northern Hemisphere. Deep-rooted forests exhibit a drought legacy response with reduced growth during up to 4 years after an extreme drought, whereas shrubs and grass have drought legacy effects of approximately 2 years and 1 year, respectively. Statistical analyses partly attribute the differences in drought legacy effects among PFGs to plant eco-hydrological properties (related to traits), including plant water use and hydraulic responses. These results can be used to improve the representation of drought response of different PFGs in land surface models, and assess their biogeochemical and biophysical feedbacks in response to a warmer and drier climate.

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