Climate Change Data Portal
DOI | 10.1002/wcc.780 |
Global soil organic carbon-climate interactions: Why scales matter | |
Jungkunst, Hermann F.; Goepel, Jan; Horvath, Thomas; Ott, Simone; Brunn, Melanie | |
发表日期 | 2022 |
ISSN | 1757-7780 |
EISSN | 1757-7799 |
卷号 | 13期号:4页码:17 |
英文摘要 | 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 |
英文关键词 | critical mesoscale; ESM; regional perspectives; soil carbon persistence |
学科领域 | Environmental Studies; Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000804586300001 |
来源期刊 | WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/272956 |
作者单位 | University of Koblenz & Landau; California State University System; California State University Monterey Bay; Leibniz University Hannover |
推荐引用方式 GB/T 7714 | Jungkunst, Hermann F.,Goepel, Jan,Horvath, Thomas,et al. Global soil organic carbon-climate interactions: Why scales matter[J],2022,13(4):17. |
APA | Jungkunst, Hermann F.,Goepel, Jan,Horvath, Thomas,Ott, Simone,&Brunn, Melanie.(2022).Global soil organic carbon-climate interactions: Why scales matter.WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE,13(4),17. |
MLA | Jungkunst, Hermann F.,et al."Global soil organic carbon-climate interactions: Why scales matter".WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE 13.4(2022):17. |
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