This chapter contains high-level background on the importance of the global carbon cycle, the major pools and fluxes of carbon, what’s changed over time, and perturbations of the carbon cycle. It also has a section that pertains specifically to the North American carbon cycle. The chapter represents a considerable effort on the part of the authors to distill the literature and key points. While it does a good job giving a high-level overview, it could be improved by the harmonization of the data in the text with the figures and other chapters in the draft report as well as by adding new conceptual figure(s) and a table. Some other general suggestions include:
The chapter is not balanced between CO2 and CH4. There needs to be a key finding about CH4. The term “carbon” often refers only to CO2, and not methane (e.g. Section 1.3.2).
For methane, it is important to mention recent studies that have used “top down” observations to derive emission estimates that are higher than the “bottom up” EPA inventory estimates (e.g., Kort et al., 2014; Miller et al., 2013; Turner et al., 2016). Studies that have fused large collections of airborne, ground-based, and satellite data should be given particular attention.
Further editing to clarify and shorten the key findings as well as some of the text would also improve the chapter.
There was not always a consistent mention of cement production and inland waters as important sources of carbon emissions to the atmosphere. And there is some problem with consistency for fluxes within this chapter and Figure 1.1, as well as across other chapters.
Some sections are not well organized or clearly written. For example, Section 1.1 should have, at a minimum, a much stronger introductory sentence that illustrates the fundamental importance of the carbon cycle. See, for example Cole, 2013.
Some of the headers are ambiguous and, in some cases, do not describe well the content of the paragraphs that follow. For example: Section 1.1 (The Role of Carbon)—where, and for what? Section 1.2 (The Natural Carbon Cycle)—the 2nd paragraph talks about human influence on the carbon cycle.
The Chapter is missing a conceptual figure to illustrate feedbacks. The nature and magnitude of feedbacks are likely to be crucially important, which is identified in the text
One of the major new pieces of information for SOCCR2 is the emissions contribution from inland waters. This was not highlighted in the key findings, but should be. The authors should be careful to explain that this flux includes the background flux, not just fluxes in response to anthropogenic emissions. Also the discussion of methane is very slim and should be enhanced.
The suggestion that “global emissions became slightly more uncoupled from economic growth”…requires a synthesis figure and/or references to support this finding.
Often time frames are missing (see above and line comments)
It would be helpful to add:
They were not explicitly part of this chapter.
Yes, with the exception of Key Finding 3, about which it is not possible to tell.
Some improvements are necessary, see above.
In addition to figure and table suggestions noted above, it would be good to add an explanatory sentence or two about radiative anthropogenic forcing on page 5, should the authors decide to keep radiative forcing in this report.
In general, we find the key findings are unnecessarily long, and a few are not as clear as they could be. Specific suggestions include the following:
Key Finding 1.
Key Finding 2.
Key Finding 3.
Key Finding 4.
Key Finding 5.
P49, Line 14-20
Please reference years or range of years in Key Finding 1 as is done for Key Finding 2.
P49, Line 35
Change “slowed” to “decreased”, since there is a negative value for percentage change.
P49, Line 36
Flat growth is an oxymoron, it seems.
P50, Line 8-9
Please clarify, e.g., mitigation activities, such as…
P50, Line 13-15
This wording is awkward, rewording is suggested.
P49, Line 13 – P50, Line23
Missing from the findings are a direct reference to (1) new global emissions estimates from inland waters and (2) the proportion of cement production emissions contributing to global CO2. The data for (1) are in Fig 1.1
P50, Line 24
This chapter should start with some introductory text.
P50, Line 24 – P51, Line 15
This section should be edited for content and clarity. (Role of Carbon—where, for what?)
P50, Line 25-27
The first couple of sentences are vague. See Cole, 2013.
P51, Line 16-21
Some background discussion about the Earth system would be helpful here: for instance, give % marine, %land, % terrestrial, % freshwater, % ice.
P51, Line 16-21
Missing from the system discussion and from Figure 1.1 are feedbacks; this should be included.
P51, Line 38-40
Add temporal reference for slow carbon cycles and geologic reservoirs.
P52, Line 4-11
Mention spatial extent of carbon stored in soils, permafrost, etc.
Page 52, Line 29
The Southern Ocean is the largest region of carbon sink (e.g. Gruber et al., 2009). It is more diffuse than the North Atlantic, but acts over a much larger area. It should be mentioned here for
completeness. Also, “top-down” estimates of the North American CO2 sink are tied to the highly uncertain magnitude of the Southern Ocean sink.
Page 52, Line 31
While small interannual variability of the ocean is what Wanninkhof et al., 2013 suggests, newer information suggests that the variability is likely substantially larger than previously thought (Landschützer et al., 2015).
P52, Line 37-38
This reads as if El Nino of 2016 is the only driver.
P53, Line 4
Add time frame
P53, Line 7
Why “note?”
P53, Line 36
Many of these natural processes are anthropogenically influenced or are a results of feedbacks.
P54, Line 6
Since 1870? From when to 1870? Is the time frame 1870-2014?
P54, Line 7-11
Need references and or a synthesis figure to support this assertion.
P54, Line 27-28
It seems odd to include the reference on how to avoid emissions here.
P54, Line 29-32
Name major sources of OH, to provide more context for this sentence.
P54, Line 22-32
This paragraph mixes emissions and reduction of emissions strategies and processes.
P55, Line 20
What time frame is used for the cumulative emissions discussion?
P55, Line 33-39
The accounting is not clear as written. North American emissions (from fossil fuel burning and cement production only—not inland waters?) are being compared to the terrestrial sink in North America?
P56, Line 3-4
Where is the boundary vis-à-vis ocean uptake? Is any part of that considered a North American sink? This is unclear.
P56, Line 16
The text would benefit from a figure showing feedbacks and how they may interact to influence the future carbon cycle.
P56, Line 25-27
As is pointed out elsewhere in the document, the situation is not quite as direct as CO2 causing a direct fertilization effect.
P56, Line 32-35
This paragraph is rather superficial. In particular, deeper discussion of the likely future response of the ocean sink is needed, as it is not as simple as suggested here. There is substantial uncertainty in future uptake, as a function of ocean circulation, warming, chemical changes (Lovenduski et al., 2016; Randerson et al., 2015). The sensitivity of the ocean sink to emission pathways needs more study. The idea of a continually growing sink in the ocean only applies under a high emission trajectory. If a low emission trajectory is taken, the ocean should outgas carbon, particularly in the subtropics where waters with high anthropogenic carbon content are circulating in the upper ocean (DeVries et al., 2017).
P56, Line 4
The title for this subsection is mismatched with content.
P57, Line 26
Safe for what?
P59, Line 4-5
There are too many “furthermores” used here.
P60, Line 14
This should be estimates of cumulative carbon emissions, correct?
P61, Line 22-26
It would be helpful to see a summary figure showing the economic and emissions data.
P61, Line 35-39
This is a vague paragraph.
P62, Line 15-17
What about emissions from inland waters?
Page 62, Line 15-26
The presentation here suggest equal uncertainty in the land and ocean sinks, which is not the case (Le Quéré et al., 2016; 2017). In addition, the approach to estimation of the ocean sink is mis-represented. The cumulative ocean sink is best constrained using ocean interior data (DeVries, 2014; Khatiwala et al., 2009; 2013; Sabine et al., 2004; Sabine and Tanhua, 2010), surface ocean pCO2 data can provide independent confirmation of the magnitude of the mean sink (Landschützer et al., 2013; 2014; 2015; 2016; Takahashi et al., 2009). There remains substantial uncertainty with respect to interannual variability in the global carbon cycle, with models believed to strongly underestimate the actual
variability (Landschützer et al., 2015). These models are quantitatively tied to the estimates from interior ocean data and surface ocean pCO2.
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