The Climate Change Crisis: History
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Albert J. Gabric

Anthropogenic climate change (ACC) has evolved into a set of crises due to society’s deep economic dependency on fossil fuels. These multiple crises have been well documented and span diverse ecological, human health and economic settings. Given the scale and breadth of CC impacts, expert labeling of the issues has gradually changed from the somewhat benign sounding “global warming” to the more frightening description of a “climate emergency”. Notwithstanding calls for transformative societal change, serious attempts to confront ACC have been hampered by decades of government policy inaction, various scientific debates, political conservatism and denial and public ignorance or apathy. 

  • climate change
  • fossil fuels
  • mitigation

1. Introduction

The multiple threats due to impacts of ACC are now thought to constitute a global emergency [1], with potentially catastrophic consequences for humanity [2]. Notwithstanding decades of international research, political debate and increasingly ominous scientific warnings since the first IPCC assessment in 1990, the failure of mitigation through carbon emissions reduction is depressingly clear. In fact, the global increase in CO2 emissions has been relentless, with emissions now 60% higher than they were in 1990 [3]. Monthly mean carbon dioxide measured at the Mauna Loa Observatory, Hawaii, constitutes the longest record of direct measurements of CO2 in the atmosphere (see Figure 1). This monitoring program was started by C. David Keeling of the Scripps Institution of Oceanography in March 1958 at a facility of the National Oceanic and Atmospheric Administration [4]. Current CO2 concentration (April 2023) at Mauna Loa is 423 ppm, which is an increase of about 108 ppm (or 35%) since the start of the monitoring program. The current emissions trajectory puts the world on track for a temperature rise of between 2.1 °C and 3.9 °C by the end of this century [5], with even the lower temperature bound implying severe disruption to many of the Earth’s systems.
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Figure 1. The so-called “Keeling curve”. Data retrieved from NOAA Global Monitoring website https://gml.noaa.gov/ccgg/trends/, accessed on 5 June 2023.
As an attempt to reduce our collective dependence on fossil fuels, various alternative energy sources such as renewables have been promoted and developed in recent decades. However, fossil fuels still accounted for 82% of primary energy in 2021, down from 83% in 2019 and 85% five years ago [6]. Notwithstanding photovoltaic, nuclear and hydroelectric sources, fossil fuels (primarily coal and gas) still dominate global electricity production, generating over 60% of today’s global electricity supply (https://ourworldindata.org/fossil-fuels, accessed on 30 May 2023).
Against this background of climate policy inaction, multiple biophysical and human health impacts are already evident or predicted to increase in the near future. These impacts include: changes in the growth and distribution of plants [7], animals and insects [8]; ocean acidification [9] and poleward shifts in the distribution of marine species [10] with effects on global fisheries; and increases in marine heatwaves and coral bleaching [11].
It is likely that ACC has increased the frequency and intensity of daily temperature extremes [12] and has also contributed to a widespread intensification of daily precipitation extremes [13]. These extreme weather events have increased human morbidity and mortality [14][15] and contributed to forced human migration [16], especially in the world’s poorer regions. There is also some evidence of a temporal increase in economic damages from extreme weather events, particularly in temperate climate zones [17].
Although consistent with the warming of the troposphere, it is still uncertain whether specific extreme weather events—such as floods, droughts and heat waves—are partially or totally the result of anthropogenic climate change. A closely related question is how ACC affects the statistical probability of a particular extreme weather event occurring. Resolving this attribution question is not straightforward and involves the analysis of often-limited observational data and the use of climate model(s), thus often taking some time to resolve. Given the increasing number of extreme weather events (https://www.undrr.org/quick/50922, accessed on 30 May 2023), the field of “event attribution” science has grown during the last decade but is still an evolving field of research [18][19]. For a good overview of event attribution, the reader is referred to van Oldenborgh et al. [20].

2. Mitigation Failure

Global carbon emissions increased rapidly from the mid-20th century (see Figure 2a), coinciding with a sharp upturn in a multitude of global socio-economic indicators at that time (See Figure 2b), a phenomenon termed the ‘Great Acceleration’ [21]. It is important to note that per capita GDP has increased faster than global population, with the “average person” in the world now being 4.4 times richer than in 1950, during which time the world population has increased 3-fold, from around 2.5 billion to almost 7.5 billion today [22]. It is pertinent to reflect on what the number of impoverished people would have been without this increase in GDP, largely enabled by the combustion of fossil fuels. This highlights the ethical and social justice dimensions of attempts at emissions reduction, where the remaining carbon budget (to avoid catastrophic CC) needs to be allocated amongst countries in a fashion that is deemed fair to all parties (see Zhou and Wang [23] and Williges et al. [24] for reviews of this contentious field).
Atmosphere 14 01081 g002a 550Atmosphere 14 01081 g002b 550
Figure 2. (a) Global CO2-equivalent emissions data retrieved from Ritchie et al. [25], source data from Jones et al [26] (b) GDP per capita in selected regions, data retrieved from https://ourworldindata.org/economic-growth#gdp-growth-since-1950, accessed on 2 May 2023 based on Bolt and Van Zanden [27].
Various multi-faceted reasons for our collective failure to bend the global emissions curve have been identified [3]. These include, inter alia, economic, geo-political, psychological and sociological factors, all combining to create an almost immutable status quo. In addition, the last three decades have seen a concerted effort to either deny the reality of CC [28][29] or, through the use of more nuanced arguments, to seek to delay climate action [30]. These denialist strategies have been successful, as shown by recent analyses of public opinion in the USA, where public understanding of global warming is improving but remains low and perceived personal risk is still very low [31]. In the highly polarized and politicized USA population, the expression of skeptical opinions appears to have more influence on public perceptions than factual science [32]. Likewise, studies of public opinion in Europe suggest that climate change experiences (e.g., extreme weather events) can increase support for climate action, but only under favorable economic conditions [33]. A similar relationship was found in Australia, where climate change skepticism was shown to be negatively associated with the annual global temperatures the previous year [34].
Some authors point to a breakdown of the science–society contract, referring to the tragedy of climate change science—namely, that despite compelling evidence and fresh warnings issued ever more frequently, greenhouse gas (GHG) emissions and other indicators of adverse climate impacts have risen steadily. This lack of societal action has led some to suggest a moratorium on further CC research [35]. The only momentary slowing of emissions occurred during the 2008–09 GFC, with a rapid rebound in subsequent years [36], underscoring the tight coupling of global economic growth and fossil fuel usage. This multi-faceted complexity emphasizes the “wicked” nature of the CC problem which underpins the difficulty in addressing the climate change threat through efforts at societal decarbonization. As first discussed by Rittel and Webber [37], wicked problems always occur in a social context—the wickedness of the problem reflects the diversity among the stakeholders affected by the problem. In the context of climate change, all of us are arguably stakeholders, which underscores both the complexity of the problem and the difficulty of reaching international consensus on ways forward.
Carbon capture and storage (CCS), once thought to be a central technology to offset present and future GHG emissions while continuing societal use of fossil fuels, has proved to be expensive and difficult to deploy at the required rate due to the limited availability of storage sites [38][39]. At current rates of deployment, CO2 storage capacity by 2050 is projected to be around 700 million tons per year, just 10% of what is required [40]. Oreskes [41] describes CCS as a technology that does not yet exist—in other words, despite many attempts, it has not been shown to be a way to store carbon in the ground safely, permanently and affordably.

3. Calls for Transformative Change

It is evident that the rate of mitigation needs to increase and that the international community must urgently reduce GHG emissions. What is also clear is that this implies nothing less than wholesale societal changes, without which CC impacts will continue and likely accelerate. This will only happen through deep changes to our energy, industry, transport, food and financial systems. In the context of widespread global environmental degradation (of which CC is only one, albeit important, part), Diaz et al. [42] urge transformative change that tackles the root causes: the interconnected economic, sociocultural, demographic, political, institutional and technological indirect drivers behind the direct drivers. A call for just such a societal transformation was made in the papal encyclical “Laudato Si” by Pope Francis [43]. More recently, faith leaders representing the world’s major religions joined scientists at the Vatican to call on the international community to raise their ambition and step up their climate action ahead of the UN Climate Change Conference COP26 in November 2021 in Glasgow. The faith leaders’ appeal stated: “We must address these challenges using the knowledge of science and the wisdom of religion. We must think long-term for the sake of the whole of humanity. Now is the time to take transformative action as a common response”.

4. Nonlinearity in the Climate System

The nonlinearity of the climate has been recognized for quite some time [44] and may lead to abrupt and dangerous perturbations to the climate [45]. Nonlinear dynamical systems are characterized by several important differences from linear systems. These differences include:
-
The possibility of the system undergoing sharp transitions, even in the presence of steady forcing;
-
A small change in some parameters can cause great qualitative differences in the resulting behavior (e.g., chaos);
-
The response of a nonlinear system to oscillatory external forcing usually exhibits frequencies not present in the external forcing.
Nonlinear dynamical systems are challenging to model and can harbor surprises or manifest periods of abrupt change (or even persistent catastrophic shifts), notwithstanding only gradual change in external forcings, e.g., increasing GHG emissions [46]. Abrupt change in the climate system has been identified in the paleoclimatic ice core record even during the otherwise relatively stable Holocene epoch [47][48]. Indeed, various potential “climate tipping points” have been identified in the Earth’s climate system [49]. Examples of these tipping points include, inter alia, triggering polar ice sheet collapses, polar permafrost thawing, monsoon disruptions and forest and coral reef diebacks. If triggered, these could cause rapid, and perhaps irreversible, planetary change [50]. Although the timing of such possible changes is uncertain, their occurrence will likely be a function of the degree of warming [51]. Armstrong Mackay et al. [52] note that even a global warming of 1 °C, a threshold that we already have passed, puts us at risk by triggering some tipping points. Limiting global warming to 1.5–2 °C—as agreed upon in the Paris Accord—could still mean exceeding the best estimates for several tipping points, causing the loss of mountain glaciers and the disruption of key ocean currents. This finding underscores the urgency of limiting additional warming as much as possible.

5. Enhancing Natural Carbon Sinks

Agricultural land use practices have historically been a major contributor to GHG emissions and are still responsible for up to a third of total anthropogenic GHG emissions [53]. Poor land management has caused between 1 and 6 billion hectares of global soils to be considered degraded to varying degrees [54], having lost much of their soil organic carbon (SOC) through the historical expansion of agriculture [55]. The main land-based mechanisms to enhance emissions sinks (so-called ‘negative emissions technologies’) are through improving the SOC of degraded agricultural lands and through afforestation or reforestation. For context, it is useful to note that, during the last decade (2011–2020), the net global increase in anthropogenic CO2 emissions, after accounting for ocean and land sinks, was 4.9 GtC yr−1 [56]. If land management practices are improved, it is estimated that sequestering organic carbon in soil could potentially remove up to 1.54 GtC yr−1 from the atmosphere, while afforestation and reforestation could remove up to 0.98 GtC yr−1 [57]. These approaches would provide significant environmental co-benefits, such as improving soil health and food security, apart from addressing ACC [58]. However, as noted above, the period left to implement change at the scale required is short, and improved land management practices need to be rapidly scaled up and implemented to contribute effectively to climate change mitigation [59][60]. Unfortunately, accurate estimates of land use emissions are still being assessed, and uncertainties in land use emissions are very high [61].

This entry is adapted from the peer-reviewed paper 10.3390/atmos14071081

References

  1. Ripple, W.J.; Wolf, C.; Gregg, J.W.; Levin, K.; Rockström, J.; Newsome, T.M.; Betts, M.G.; Huq, S.; Law, B.E.; Kemp, L.; et al. World Scientists’ Warning of a Climate Emergency 2022. BioScience 2022, 72, 1149–1155.
  2. Kemp, L.; Xu, C.; Depledge, J.; Ebi, K.L.; Gibbins, G.; Kohler, T.A.; Rockström, J.; Scheffer, M.; Schellnhuber, H.J.; Steffen, W.; et al. Climate Endgame: Exploring catastrophic climate change scenarios. Proc. Natl. Acad. Sci. USA 2022, 119, e2108146119.
  3. Stoddard, I.; Anderson, K.; Capstick, S.; Carton, W.; Depledge, J.; Facer, K.; Gough, C.; Hache, F.; Hoolohan, C.; Hultman, M. Three decades of climate mitigation: Why haven’t we bent the global emissions curve? Annu. Rev. Environ. Resour. 2021, 46, 653–689.
  4. Keeling, C.D.; Bacastow, R.B.; Bainbridge, A.E.; Ekdahl, C.A., Jr.; Guenther, P.R.; Waterman, L.S.; Chin, J.F.S. Atmospheric carbon dioxide variations at Mauna Loa Observatory, Hawaii. Tellus 1976, 28, 538–551.
  5. Liu, P.R.; Raftery, A.E. Country-based rate of emissions reductions should increase by 80% beyond nationally determined contributions to meet the 2 C target. Commun. Earth Environ. 2021, 2, 29.
  6. BP. The Energy Institute Statistical Review of World Energy. Available online: https://www.bp.com/en/global/corporate/energy-economics/statistical-review-of-world-energy.html (accessed on 22 May 2023).
  7. Parmesan, C.; Hanley, M.E. Plants and climate change: Complexities and surprises. Ann. Bot. 2015, 116, 849–864.
  8. Halsch, C.A.; Shapiro, A.M.; Fordyce, J.A.; Nice, C.C.; Thorne, J.H.; Waetjen, D.P.; Forister, M.L. Insects and recent climate change. Proc. Natl. Acad. Sci. USA 2021, 118, e2002543117.
  9. Doney, S.C.; Busch, D.S.; Cooley, S.R.; Kroeker, K.J. The Impacts of Ocean Acidification on Marine Ecosystems and Reliant Human Communities. Annu. Rev. Environ. Resour. 2020, 45, 83–112.
  10. Poloczanska, E.S.; Brown, C.J.; Sydeman, W.J.; Kiessling, W.; Schoeman, D.S.; Moore, P.J.; Brander, K.; Bruno, J.F.; Buckley, L.B.; Burrows, M.T.; et al. Global imprint of climate change on marine life. Nat. Clim. Chang. 2013, 3, 919–925.
  11. Hughes, T.P.; Baird, A.H.; Bellwood, D.R.; Card, M.; Connolly, S.R.; Folke, C.; Grosberg, R.; Hoegh-Guldberg, O.; Jackson, J.B.C.; Kleypas, J.; et al. Climate Change, Human Impacts, and the Resilience of Coral Reefs. Science 2003, 301, 929–933.
  12. Dahl, K.; Licker, R.; Abatzoglou, J.T.; Declet-Barreto, J. Increased frequency of and population exposure to extreme heat index days in the United States during the 21st century. Environ. Res. Commun. 2019, 1, 075002.
  13. Fowler, H.J.; Lenderink, G.; Prein, A.F.; Westra, S.; Allan, R.P.; Ban, N.; Barbero, R.; Berg, P.; Blenkinsop, S.; Do, H.X.; et al. Anthropogenic intensification of short-duration rainfall extremes. Nat. Rev. Earth Environ. 2021, 2, 107–122.
  14. Vicedo-Cabrera, A.M.; Scovronick, N.; Sera, F.; Royé, D.; Schneider, R.; Tobias, A.; Astrom, C.; Guo, Y.; Honda, Y.; Hondula, D.M.; et al. The burden of heat-related mortality attributable to recent human-induced climate change. Nat. Clim. Chang. 2021, 11, 492–500.
  15. Patz, J.A.; Campbell-Lendrum, D.; Holloway, T.; Foley, J.A. Impact of regional climate change on human health. Nature 2005, 438, 310–317.
  16. Berchin, I.I.; Valduga, I.B.; Garcia, J.; de Andrade Guerra, J.B.S.O. Climate change and forced migrations: An effort towards recognizing climate refugees. Geoforum 2017, 84, 147–150.
  17. Coronese, M.; Lamperti, F.; Keller, K.; Chiaromonte, F.; Roventini, A. Evidence for sharp increase in the economic damages of extreme natural disasters. Proc. Natl. Acad. Sci. USA 2019, 116, 21450–21455.
  18. National Academies of Sciences, Engineering and Medicine. Attribution of Extreme Weather Events in the Context of Climate Change; National Academies Press: Washington, DC, USA, 2016.
  19. Stott, P. How climate change affects extreme weather events. Science 2016, 352, 1517–1518.
  20. van Oldenborgh, G.J.; van der Wiel, K.; Kew, S.; Philip, S.; Otto, F.; Vautard, R.; King, A.; Lott, F.; Arrighi, J.; Singh, R.; et al. Pathways and pitfalls in extreme event attribution. Clim. Chang. 2021, 166, 13.
  21. Head, M.J.; Steffen, W.; Fagerlind, D.; Waters, C.N.; Poirier, C.; Syvitski, J.; Zalasiewicz, J.A.; Barnosky, A.D.; Cearreta, A.; Jeandel, C.; et al. The Great Acceleration is real and provides a quantitative basis for the proposed Anthropocene Series/Epoch. Int. Union Geol. Sci. 2022, 45, 359–376.
  22. UN. World Population Prospects 2022. Available online: https://population.un.org/wpp/Download/Standard/Population/ (accessed on 11 May 2023).
  23. Zhou, P.; Wang, M. Carbon dioxide emissions allocation: A review. Ecol. Econ. 2016, 125, 47–59.
  24. Williges, K.; Meyer, L.H.; Steininger, K.W.; Kirchengast, G. Fairness critically conditions the carbon budget allocation across countries. Glob. Environ. Chang. 2022, 74, 102481.
  25. Ritchie, H.; Roser, M.; Rosado, P. CO2 and Greenhouse Gas Emissions . Available online: https://ourworldindata.org/co2-and-greenhouse-gas-emissions (accessed on 2 May 2023).
  26. Jones, M.W.; Peters, G.P.; Gasser, T.; Andrew, R.M.; Schwingshackl, C.; Gütschow, J.; Houghton, R.A.; Friedlingstein, P.; Pongratz, J.; Le Quéré, C. National contributions to climate change due to historical emissions of carbon dioxide, methane, and nitrous oxide since 1850. Sci. Data 2023, 10, 155.
  27. Bolt, J.; Van Zanden, J.L. Maddison style estimates of the evolution of the world economy. A new 2020 update. In Maddison-Project Working Paper WP-15; University of Groningen: Groningen, The Netherlands, 2020.
  28. Oreskes, N. The scientific consensus on climate change. Science 2004, 306, 1686.
  29. Lewandowsky, S.; Oreskes, N.; Risbey, J.S.; Newell, B.R.; Smithson, M. Seepage: Climate change denial and its effect on the scientific community. Glob. Environ. Chang. 2015, 33, 1–13.
  30. Lamb, W.F.; Mattioli, G.; Levi, S.; Roberts, J.T.; Capstick, S.; Creutzig, F.; Minx, J.C.; Müller-Hansen, F.; Culhane, T.; Steinberger, J.K. Discourses of climate delay. Glob. Sustain. 2020, 3, e17.
  31. Ballew, M.T.; Leiserowitz, A.; Roser-Renouf, C.; Rosenthal, S.A.; Kotcher, J.E.; Marlon, J.R.; Lyon, E.; Goldberg, M.H.; Maibach, E.W. Climate Change in the American Mind: Data, Tools, and Trends. Environ. Sci. Policy Sustain. Dev. 2019, 61, 4–18.
  32. Nyhan, B.; Porter, E.; Wood, T.J. Time and skeptical opinion content erode the effects of science coverage on climate beliefs and attitudes. Proc. Natl. Acad. Sci. USA 2022, 119, e2122069119.
  33. Hoffmann, R.; Muttarak, R.; Peisker, J.; Stanig, P. Climate change experiences raise environmental concerns and promote Green voting. Nat. Clim. Chang. 2022, 12, 148–155.
  34. Hornsey, M.J.; Chapman, C.M.; Humphrey, J.E. Climate skepticism decreases when the planet gets hotter and conservative support wanes. Glob. Environ. Chang. 2022, 74, 102492.
  35. Glavovic, B.C.; Smith, T.F.; White, I. The tragedy of climate change science. Clim. Dev. 2022, 14, 829–833.
  36. Peters, G.P.; Marland, G.; Le Quéré, C.; Boden, T.; Canadell, J.G.; Raupach, M.R. Rapid growth in CO2 emissions after the 2008–2009 global financial crisis. Nat. Clim. Chang. 2012, 2, 2–4.
  37. Rittel, H.W.; Webber, M.M. Wicked problems. Man-Made Futur. 1974, 26, 272–280.
  38. Scott, V.; Gilfillan, S.; Markusson, N.; Chalmers, H.; RS, H. Last chance for carbon capture and storage. Nat. Clim. Chang. 2013, 3, 105–111.
  39. Lu, Y.; Cohen, F.; Smith, S.M.; Pfeiffer, A. Plant conversions and abatement technologies cannot prevent stranding of power plant assets in 2 °C scenarios. Nat. Commun. 2022, 13, 806.
  40. Martin-Roberts, E.; Scott, V.; Flude, S.; Johnson, G.; Haszeldine, R.S.; Gilfillan, S. Carbon capture and storage at the end of a lost decade. One Earth 2021, 4, 1569–1584.
  41. Oreskes, N. Carbon-reduction plans rely on tech that doesn’t exist. Sci. Am. 2022, 327, 90.
  42. Díaz, S.; Settele, J.; Brondízio, E.S.; Ngo, H.T.; Agard, J.; Arneth, A.; Balvanera, P.; Brauman, K.A.; Butchart, S.H.M.; Chan, K.M.A.; et al. Pervasive human-driven decline of life on Earth points to the need for transformative change. Science 2019, 366, eaax3100.
  43. Francis, P. Praise Be to You: Laudato Si’: On Care for Our Common Home; Ignatius Press: San Francisco, CA, USA, 2015.
  44. Rial, J.A.; Pielke, R.A.; Beniston, M.; Claussen, M.; Canadell, J.; Cox, P.; Held, H.; de Noblet-Ducoudré, N.; Prinn, R.; Reynolds, J.F. Nonlinearities, feedbacks and critical thresholds within the Earth’s climate system. Clim. Chang. 2004, 65, 11–38.
  45. Rial, J.A. Abrupt climate change: Chaos and order at orbital and millennial scales. Glob. Planet. Chang. 2004, 41, 95–109.
  46. Krishnamurthy, V. Predictability of Weather and Climate. Earth Space Sci. 2019, 6, 1043–1056.
  47. Dansgaard, W.; Johnsen, S.J.; Clausen, H.B.; Dahl-Jensen, D.; Gundestrup, N.S.; Hammer, C.U.; Hvidberg, C.S.; Steffensen, J.P.; Sveinbjörnsdottir, A.E.; Jouzel, J.; et al. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature 1993, 364, 218–220.
  48. Alley, R.B.; Ágústsdóttir, A.M. The 8k event: Cause and consequences of a major Holocene abrupt climate change. Quat. Sci. Rev. 2005, 24, 1123–1149.
  49. Lenton, T.M.; Held, H.; Kriegler, E.; Hall, J.W.; Lucht, W.; Rahmstorf, S.; Schellnhuber, H.J. Tipping elements in the Earth’s climate system. Proc. Natl. Acad. Sci. USA 2008, 105, 1786–1793.
  50. Lenton, T.M.; Rockström, J.; Gaffney, O.; Rahmstorf, S.; Richardson, K.; Steffen, W.; Schellnhuber, H.J. Climate tipping points—Too risky to bet against. Nature 2019, 575, 592–595.
  51. Kriegler, E.; Hall, J.W.; Held, H.; Dawson, R.; Schellnhuber, H.J. Imprecise probability assessment of tipping points in the climate system. Proc. Natl. Acad. Sci. USA 2009, 106, 5041–5046.
  52. Armstrong McKay, D.I.; Staal, A.; Abrams, J.F.; Winkelmann, R.; Sakschewski, B.; Loriani, S.; Fetzer, I.; Cornell, S.E.; Rockström, J.; Lenton, T.M. Exceeding 1.5C global warming could trigger multiple climate tipping points. Science 2022, 377, eabn7950.
  53. Vermeulen, S.J.; Campbell, B.M.; Ingram, J.S. Climate change and food systems. Annu. Rev. Environ. Resour. 2012, 37, 195–222.
  54. Gibbs, H.K.; Salmon, J.M. Mapping the world’s degraded lands. Appl. Geogr. 2015, 57, 12–21.
  55. Sanderman, J.; Hengl, T.; Fiske, G.J. Soil carbon debt of 12,000 years of human land use. Proc. Natl. Acad. Sci. USA 2017, 114, 9575–9580.
  56. Friedlingstein, P.; Jones, M.W.; O’Sullivan, M.; Andrew, R.M.; Bakker, D.C.; Hauck, J.; Le Quéré, C.; Peters, G.P.; Peters, W.; Pongratz, J. Global carbon budget 2021. Earth Syst. Sci. Data 2022, 14, 1917–2005.
  57. Fuss, S.; Lamb, W.F.; Callaghan, M.W.; Hilaire, J.; Creutzig, F.; Amann, T.; Beringer, T.; de Oliveira Garcia, W.; Hartmann, J.; Khanna, T.; et al. Negative emissions—Part 2: Costs, potentials and side effects. Environ. Res. Lett. 2018, 13, 063002.
  58. Griscom, B.W.; Adams, J.; Ellis, P.W.; Houghton, R.A.; Lomax, G.; Miteva, D.A.; Schlesinger, W.H.; Shoch, D.; Siikamäki, J.V.; Smith, P.; et al. Natural climate solutions. Proc. Natl. Acad. Sci. USA 2017, 114, 11645–11650.
  59. Amelung, W.; Bossio, D.; de Vries, W.; Kögel-Knabner, I.; Lehmann, J.; Amundson, R.; Bol, R.; Collins, C.; Lal, R.; Leifeld, J.; et al. Towards a global-scale soil climate mitigation strategy. Nat. Commun. 2020, 11, 5427.
  60. Lal, R.; Bouma, J.; Brevik, E.; Dawson, L.; Field, D.J.; Glaser, B.; Hatano, R.; Hartemink, A.E.; Kosaki, T.; Lascelles, B.; et al. Soils and sustainable development goals of the United Nations: An International Union of Soil Sciences perspective. Geoderma Reg. 2021, 25, e00398.
  61. Fyson, C.L.; Jeffery, M.L. Ambiguity in the Land Use Component of Mitigation Contributions Toward the Paris Agreement Goals. Earth’s Future 2019, 7, 873–891.
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