Articles | Volume 17, issue 15
https://doi.org/10.5194/bg-17-4007-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-4007-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
10 Aug 2020
Research article | Highlight paper |
| 10 Aug 2020
| 10 Aug 2020
Rainfall intensification increases the contribution of rewetting pulses to soil heterotrophic respiration
Stefano Manzoni
CORRESPONDING AUTHOR
Department of Physical Geography, Stockholm University, 10691
Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Arjun Chakrawal
Department of Physical Geography, Stockholm University, 10691
Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Thomas Fischer
Central Analytical Laboratory, Brandenburg University of Technology,
Cottbus, Germany
Joshua P. Schimel
Department of Ecology, Evolution, and Marine Biology, University of
California, Santa Barbara, USA
Amilcare Porporato
Department of Civil and environmental Engineering, Princeton
University, Princeton, USA
Giulia Vico
Department of Crop Production Ecology, Swedish University of
Agricultural Sciences, Uppsala, Sweden
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25 citations as recorded by crossref.
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- Soil Carbonyl Sulfide (OCS) Fluxes in Terrestrial Ecosystems: An Empirical Model M. Whelan et al. 10.1029/2022JG006858
- Variability of ecosystem carbon source from microbial respiration is controlled by rainfall dynamics H. Huang et al. 10.1073/pnas.2115283118
- A Microbial‐Explicit Soil Organic Carbon Decomposition Model (MESDM): Development and Testing at a Semiarid Grassland Site X. Zhang et al. 10.1029/2021MS002485
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- Dryland productivity under a changing climate L. Wang et al. 10.1038/s41558-022-01499-y
- Microscale heterogeneity controls macroscopic soil heterotrophic respiration by regulating resource availability and environmental stress Z. Yan et al. 10.1007/s10533-023-01044-9
- Soil texture and environmental conditions influence the biogeochemical responses of soils to drought and flooding K. Patel et al. 10.1038/s43247-021-00198-4
- The Response of Daily Carbon Dioxide and Water Vapor Fluxes to Temperature and Precipitation Extremes in Temperate and Boreal Forests D. Gushchina et al. 10.3390/cli11100206
- Repeated drying and rewetting cycles accelerate bacterial growth recovery after rewetting A. Leizeaga et al. 10.1007/s00374-022-01623-2
- Different responses of soil respiration to reduced throughfall in spring and winter under contrasting hydrological conditions in a temperate forest J. Wang et al. 10.1016/j.catena.2024.108260
- Soil respiration responses of moss and lichen biocoenoses to moderate and severe rain events after summer drought in a temperate early‐successional ecosystem T. Fischer et al. 10.1002/eco.2578
- EFFECTS OF TEMPERATURE AND PRECIPITATION ANOMALIES ON CARBON DIOXIDE FLUXES IN THE EXTRATROPICAL FORESTS OF THE NORTHERN HEMISPHERE E. SATOSINA et al. 10.55959/MSU0579-9414.5.79.2.2
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Latest update: 13 Dec 2024
Short summary
Carbon dioxide is produced by soil microbes through respiration, which is particularly fast when soils are moistened by rain. Will respiration increase with future more intense rains and longer dry spells? With a mathematical model, we show that wetter conditions increase respiration. In contrast, if rainfall totals stay the same, but rain comes all at once after long dry spells, the average respiration will not change, but the contribution of the respiration bursts after rain will increase.
Carbon dioxide is produced by soil microbes through respiration, which is particularly fast when...
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