Details
| Original language | English |
|---|---|
| Article number | e780 |
| Journal | Wiley Interdisciplinary Reviews: Climate Change |
| Volume | 13 |
| Issue number | 4 |
| Publication status | Published - 14 Jun 2022 |
Abstract
Soil organic carbon (SOC) holds the largest terrestrial carbon stock because of soil conditions and processes that favor soil carbon persistence. Vulnerable to climate change, SOC may cross a tipping point toward liberating carbon-based greenhouse gases, implying massive self-amplifying SOC- climate interactions. Estimates of SOC persistence are challenging as we still lack broad mechanistic insights. Upscaling mechanistic details from small to larger scales is challenging because the driving factors are not available at the needed resolution. Downscaling is problematic as many modeling studies point to the highest uncertainties deriving from the SOC response to climate change, while models themselves have difficulties in replicating contemporary soil properties and dynamics. To bridge the problems of scaling, strict process orientation seems adequate. Holdridge Life Zones (HLZ) classification, as one example, is a climate classification framework at a mesoscale that provides a descriptive approach to facilitate the identification of potential hotspots and coldspots of SOC-climate interaction. Establishing coordinated experiments across all HLZ, but also including multiple global change drivers, has the potential to advance our understanding of general principles regulating SOC-climate interaction and SOC persistence. Therefore, regionally tailored solutions for both experiments and modeling are urgently needed and can lead to better management of soil and the ecosystem services provided. Improving “translations” from the scales relevant for process understanding to the scales of decision-making is key to good management and to predict the fate of our largest terrestrial carbon stock. This article is categorized under: Integrated Assessment of Climate Change > Integrated Scenario Development.
Keywords
- critical mesoscale, ESM, regional perspectives, soil carbon persistence
ASJC Scopus subject areas
- Social Sciences(all)
- Geography, Planning and Development
- Environmental Science(all)
- Global and Planetary Change
- Earth and Planetary Sciences(all)
- Atmospheric Science
Sustainable Development Goals
Cite this
- Standard
- Harvard
- Apa
- Vancouver
- BibTeX
- RIS
In: Wiley Interdisciplinary Reviews: Climate Change, Vol. 13, No. 4, e780, 14.06.2022.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Global soil organic carbon–climate interactions: Why scales matter
AU - Jungkunst, Hermann F.
AU - Göpel, Jan
AU - Horvath, Thomas
AU - Ott, Simone
AU - Brunn, Melanie
N1 - Funding Information: We thank our home institutes for providing the overhead support for this collaborative work. We also acknowledge the contributions of the broadest scientific community for continuously improving both experimental and modeling approaches to better understanding the role of soils under climate change, and the interest of society in using science to inform decisions that affect humanity as a whole. Open access funding enabled and organized by Projekt DEAL.
PY - 2022/6/14
Y1 - 2022/6/14
N2 - Soil organic carbon (SOC) holds the largest terrestrial carbon stock because of soil conditions and processes that favor soil carbon persistence. Vulnerable to climate change, SOC may cross a tipping point toward liberating carbon-based greenhouse gases, implying massive self-amplifying SOC- climate interactions. Estimates of SOC persistence are challenging as we still lack broad mechanistic insights. Upscaling mechanistic details from small to larger scales is challenging because the driving factors are not available at the needed resolution. Downscaling is problematic as many modeling studies point to the highest uncertainties deriving from the SOC response to climate change, while models themselves have difficulties in replicating contemporary soil properties and dynamics. To bridge the problems of scaling, strict process orientation seems adequate. Holdridge Life Zones (HLZ) classification, as one example, is a climate classification framework at a mesoscale that provides a descriptive approach to facilitate the identification of potential hotspots and coldspots of SOC-climate interaction. Establishing coordinated experiments across all HLZ, but also including multiple global change drivers, has the potential to advance our understanding of general principles regulating SOC-climate interaction and SOC persistence. Therefore, regionally tailored solutions for both experiments and modeling are urgently needed and can lead to better management of soil and the ecosystem services provided. Improving “translations” from the scales relevant for process understanding to the scales of decision-making is key to good management and to predict the fate of our largest terrestrial carbon stock. This article is categorized under: Integrated Assessment of Climate Change > Integrated Scenario Development.
AB - Soil organic carbon (SOC) holds the largest terrestrial carbon stock because of soil conditions and processes that favor soil carbon persistence. Vulnerable to climate change, SOC may cross a tipping point toward liberating carbon-based greenhouse gases, implying massive self-amplifying SOC- climate interactions. Estimates of SOC persistence are challenging as we still lack broad mechanistic insights. Upscaling mechanistic details from small to larger scales is challenging because the driving factors are not available at the needed resolution. Downscaling is problematic as many modeling studies point to the highest uncertainties deriving from the SOC response to climate change, while models themselves have difficulties in replicating contemporary soil properties and dynamics. To bridge the problems of scaling, strict process orientation seems adequate. Holdridge Life Zones (HLZ) classification, as one example, is a climate classification framework at a mesoscale that provides a descriptive approach to facilitate the identification of potential hotspots and coldspots of SOC-climate interaction. Establishing coordinated experiments across all HLZ, but also including multiple global change drivers, has the potential to advance our understanding of general principles regulating SOC-climate interaction and SOC persistence. Therefore, regionally tailored solutions for both experiments and modeling are urgently needed and can lead to better management of soil and the ecosystem services provided. Improving “translations” from the scales relevant for process understanding to the scales of decision-making is key to good management and to predict the fate of our largest terrestrial carbon stock. This article is categorized under: Integrated Assessment of Climate Change > Integrated Scenario Development.
KW - critical mesoscale
KW - ESM
KW - regional perspectives
KW - soil carbon persistence
UR - http://www.scopus.com/inward/record.url?scp=85131415012&partnerID=8YFLogxK
U2 - 10.1002/wcc.780
DO - 10.1002/wcc.780
M3 - Article
VL - 13
JO - Wiley Interdisciplinary Reviews: Climate Change
JF - Wiley Interdisciplinary Reviews: Climate Change
SN - 1757-7780
IS - 4
M1 - e780
ER -