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- | == Table of Literature potentially useful to our work... == | + | == Tables |
+ | Feel free to create more sub-pages as you see fit. | ||
Please insert any additions alphabetically by sir name of the first author. | Please insert any additions alphabetically by sir name of the first author. | ||
- | ^ Author | + | [[.collection_of_publications:carbon_cycle |
- | | Livia C.P. Dias | Patterns of land use, extensification, | + | |
- | | 2016 | Periods 1940-2000 and 2000-2012: Based on Hansen' | + | |
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- | | | {{ : | + | |
- | | Masayuki Kondo | State of the science in reconciling top-down and bottom-up approaches for terrestrial CO2 budget | | + | [[.collection_of_publications: |
- | | 2019 | Their set of atmospheric inversions and bio-sphere models, showed a high level of agreement for global and hemispheric CO2 budgets in the 2000s as well as for the regions of North America and South-east Asia. | + | |
- | | | https:// | + | [[.collection_of_publications: |
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- | | Andreas Krause | Legacy Effects from Historical Environmental Changes Dominate Future Terrestrial Carbon Uptake | | + | [[.collection_of_publications:lai_publications |
- | | 2020 | They use LPJ‐GUESS to quantify legacy effects for the 21st century. LUH2 (historic) and bias-corrected IPSL‐CM5A‐LR climate mode (future) are employed to provide land use forcing. The combined legacy effects of historical (1850–2015) environmental changes result in a land carbon uptake of +126 Gt C over the future (2015–2099) period. This by far exceeds the impacts of future environmental changes (range −53 Gt C to +16 Gt C for three scenarios) and is comparable in magnitude to historical carbon losses (−154 Gt C). The response of the biosphere to historical environmental changes dominates future terrestrial carbon cycling at least until mid-century. | | + | |
- | | | https:// | + | [[.collection_of_publications:lulcc_publications |
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- | | Andreas Krause | Large uncertainty in carbon uptake potential of land-based climate-change mitigation efforts | | + | ^ Author |
- | | 2018 | {{ : | + | |
- | | | https:// | + | |
| Pete Smith | Which practices co-deliver food security, climate change mitigation and adaptation, and combat land degradation and desertification? | | Pete Smith | Which practices co-deliver food security, climate change mitigation and adaptation, and combat land degradation and desertification? | ||
| 2019 | | | | 2019 | | | ||
| | https:// | | | https:// | ||
| | {{ : | | | {{ : | ||
- | | Philip Vergragt et al | Comparison of forest above-ground biomass from dynamic global vegetation models with spatially explicit remotely sensed observation-based estimates | | ||
- | | 2011 | This paper investigates if and how carbon capture and storage (CCS) could help to avoid reinforcing fossil fuel lock-in. The outcome is that a large-scale BECCS development could be feasible under certain conditions, thus largely avoiding the risk of reinforced fossil fuel lock-in. //Keywords: Carbon capture and storage, Biomass, Fossil fuel// | | ||
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- | | Hui Yang | Comparison of forest above-ground biomass from dynamic global vegetation models with spatially explicit remotely sensed observation-based estimates | | ||
- | | 2020 | Uses the GlobBiomass data set of forest above-ground biomass (AGB) density for the year 2010, obtained from multiple remote sensing and in situ observations at 100 m spatial resolution to evaluate AGB estimated by nine dynamic global vegetation models (DGVMs).Model estimates are 365 ± 66 Pg C compared to 275 (±13.5%) Pg C from GlobBiomass. The results suggest that TRENDY v6 DGVMs tend to underestimate biomass loss from anthropogenic disturbances.| | ||
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