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Global patterns of drought recovery.
Christopher R Schwalm1,2, William R L Anderegg3, Anna M Michalak4
1Woods Hole Research Center, Falmouth, Massachusetts 02540, USA.
Nature
|August 11, 2017
Summary
Drought recovery time, crucial for ecosystem health, depends mainly on climate and carbon cycle dynamics. Recovery is slowest in the tropics and high northern latitudes, with increasing drought impacts observed over the last century.
Area of Science:
- Ecology
- Climate Science
- Carbon Cycle Research
Background:
- Droughts are a major climatic extreme impacting global ecosystems and the land carbon sink.
- Understanding ecosystem recovery time after drought is critical for predicting future land carbon dynamics.
- Global trends in drought regimes are uncertain, but increased frequency and severity are projected for the 21st century.
Observation:
- Analysis of three independent gross primary productivity datasets reveals key factors influencing drought recovery.
- Drought recovery time is strongly linked to climate variables and carbon cycle processes.
- Biodiversity and carbon dioxide (CO2) fertilization play secondary roles in ecosystem drought recovery.
Findings:
- Drought recovery is longest in tropical and high northern latitude ecosystems, areas particularly vulnerable to climate change.
- Ecosystem drought impacts, measured by recovery area and time, have demonstrably increased throughout the 20th century.
- Global spatiotemporal patterns of drought recovery are strongly associated with climate and carbon cycle dynamics.
Implications:
- Projected increases in drought frequency may shorten the intervals between drought events, potentially exceeding ecosystem recovery times.
- This could lead to irreversible ecosystem damage and significant degradation of the vital land carbon sink.
- Urgent research and mitigation strategies are needed to address the growing threat of prolonged drought impacts on global ecosystems.
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