Differentiating drought legacy effects on vegetation growth over the temperate Northern Hemisphere
Language English Country Great Britain, England Media print-electronic
Document type Journal Article, Research Support, Non-U.S. Gov't
PubMed
28973825
DOI
10.1111/gcb.13920
Knihovny.cz E-resources
- Keywords
- drought legacy effect *, drought resilience *, ecohydrological responses *, extreme drought *, plant functional groups *, rooting system *, stomatal conductance *, vegetation growth *,
- MeSH
- Hydrology MeSH
- Climate Change * MeSH
- Forests * MeSH
- Droughts * MeSH
- Trees growth & development MeSH
- Water physiology MeSH
- Publication type
- Journal Article MeSH
- Research Support, Non-U.S. Gov't MeSH
- Names of Substances
- Water MeSH
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.
CEA CNRS UVSQ UMR8212 Laboratoire des Sciences du Climat et de l'Environnement Gif Sur Yvette France
College of Global Change and Earth System Science Beijing Normal University Beijing China
College of Urban and Environmental Science Peking University Beijing China
CzechGlobe Global Change Research Institute CAS Brno Czech Republic
Dendro Sciences Swiss Federal Research Institute WSL Birmensdorf Switzerland
Faculty of Geographical Science Beijing Normal University Beijing China
W Szafer Institute of Botany Polish Academy of Sciences Krakow Poland
References provided by Crossref.org
Responses of stem growth and canopy greenness of temperate conifers to dry spells