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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. | ||
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^ Author | ^ Author | ||
+ | | Suzanne E. Cotillon | West Africa land use and land cover time series: U.S. Geological Survey Fact Sheet 2017–3004 | | ||
+ | | 2017 | The data shows snapshots of 1975, 2000 and 2013 at typically 2km resolution, is based on Landsat imagery and validated with aerial photography, | ||
+ | | | https:// | ||
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| Livia C.P. Dias | Patterns of land use, extensification, | | Livia C.P. Dias | Patterns of land use, extensification, | ||
| 2016 | Periods 1940-2000 and 2000-2012: Based on Hansen' | | 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 | | ||
- | | 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. Differences in budget estimates are substantial for East Asia and South America. There is uncertainty in several regions as to whether these represent a carbon sink or source. Given these findings, caution should be taken when interpreting regional CO2 budgets.Those uncertainties continue to limit our ability to project the mitigation potential by the terrestrial biosphere. | | ||
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- | | Andreas Krause | Legacy Effects from Historical Environmental Changes Dominate Future Terrestrial Carbon Uptake | | ||
- | | 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. | | ||
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- | | Andreas Krause | Large uncertainty in carbon uptake potential of land-based climate-change mitigation efforts | | ||
- | | 2018 | {{ : | ||
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| 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 | | |