Paris Agreement climate proposals need a boost to keep warming well below 2 °C

Joeri Rogelj, Michel den Elzen, Niklas Höhne, Taryn Fransen, Hanna Fekete, Harald Winkler, Roberto Schaeffer, Fu Sha, Keywan Riahi, Malte MeinshausenView original
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Let's start with the simple question that sat under the Paris climate talks: if every country did what it put on paper in those early national pledges—the Intended Nationally Determined Contributions, or INDCs—where would the world end up? Not in the abstract. In tonnes of emissions in 2030 and in degrees of warming by 2100. That's the lens Rogelj, den Elzen, Höhne and colleagues used to look at the first wave of pledges lodged around 2015 to 2016. Their answer is both encouraging and sobering. The pledges clearly bend the global curve downward, but they don't bend it far enough to keep us "well below" two degrees. First, what exactly are we comparing? Think of four families of futures. There's a no-policy baseline, where countries keep doing what they were doing before climate policy had real bite. There's a current-policy track, reflecting measures already on the books. Then there are the INDC pathways themselves—what countries said they would do unconditionally and what more they'd consider if financial or technology support showed up. Finally, there's a set of least-cost two-degree pathways: stylized, globally coordinated routes that spread effort to minimize overall costs while staying under two degrees with high confidence. The team gathered global assessments covering about eighty-eight to ninety-six percent of 2012 greenhouse gas emissions, harmonized them into the same accounting system—one hundred-year global warming potentials—and translated each emissions pathway into temperatures using MAGICC, a climate model set up to give full probability ranges rather than single points. Now the headline. If countries deliver their unconditional INDCs, global greenhouse gas emissions in 2030 land around fifty-five billion tonnes of carbon-dioxide equivalent, with most studies falling between fifty-two and fifty-eight. That's a meaningful step down—roughly nine billion tonnes below a no-policy world, and about four below the median projection for "current policies only." It is progress you can point to, but it is not the trajectory that takes you on a smooth, affordable glidepath to well below two degrees. Some of that gap hides in how the pledges are written. Many are tidy, quantitative targets, but many are not. About three quarters lean on a "business-as-usual" baseline that the government defines, which means the absolute emissions level implied by the pledge depends on the shape of that baseline. Roughly forty-five percent of submissions packaged both an unconditional and a conditional element. About a third were conditional only, and the rest were noncommittal about conditions. If every conditional element were fully met, the aggregate two thousand thirty total would fall by another two point four billion tonnes—small on the global scale, but not trivial. Other uncertainties are more technical but just as important. Land-use emissions—changes in forests and soils—can be counted as part of a country's total, or handled separately under Kyoto-style rules. That choice moves national tallies around. International aviation and shipping, big and growing sectors, generally sit outside national pledges. When you exclude sectors that the INDCs don't actually cover, the share of global emissions clearly addressed drops by at least eight percentage points from those optimistic coverage claims you sometimes hear. And when you allow for market transfers—where one country can buy credited reductions from another—modeling teams disagree on how to add those up. That disagreement alone injects on the order of one billion tonnes of uncertainty into the two thousand thirty total. Set those caveats to one side and line the curves up. Against a no-policy median of about sixty-five billion tonnes in two thousand thirty, the unconditional INDCs are better by design. But the distance to a cost-optimal two-degree pathway is large. The median gap in two thousand thirty is about fourteen billion tonnes, with most estimates falling between ten to sixteen. Even if every conditional element of the pledges materialized on time, you're still roughly eleven billion tonnes too high. In plain terms: the Paris proposals took a real bite out of projected emissions, and they still left a very large slice on the plate. What does that mean for temperatures? Translate the two thousand thirty INDC world through the probabilistic lens of MAGICC and you get a median warming by two thousand one hundred of about two point nine degrees Celsius. If you ask for a two-in-three chance, that median nudges up to around three point two degrees, and if you care about the high-end risks—the nine-in-ten bound—you're looking near three point nine. Fully delivering the conditional pieces shaves only about two tenths of a degree off those medians. Better than where we were headed, yes. Consistent with "well below two"? No. The team also asks what happens after two thousand thirty, because the path you take next depends on the foundations you lay now. They sketch three archetypes. One is stall: policy momentum fades and emissions drift back toward a world without climate policy. Another is continue: post-two thousand thirty effort hums along at something like pre-two thousand thirty ambition. The third is accelerate: the world decides to push much harder. Start from the INDC two thousand thirty level and stay in the "continue" lane, and you still end up with that two point six to three point one degree window by century's end, centered around two point nine. Even in the "accelerate" lane, you're starting late and high. Budgets tell the story more starkly. The carbon budget often cited for a fifty percent chance of holding one point five degrees—on the order of five hundred to six hundred billion tonnes of carbon-dioxide equivalent—is essentially exhausted under these pledges. And for two degrees at a two-in-three chance, the budget is already overspent by around two thousand thirty on an INDC path. When you burn through the budget early, the math forces you to do two hard things later. One is to bring net carbon-dioxide emissions to zero faster, typically somewhere between two thousand sixty and two thousand eighty in these scenarios, with overall greenhouse gases balancing sometime between two thousand eighty and two thousand one hundred in about two thirds of the least-cost cases. The other is to pull a lot of carbon back out of the atmosphere. That's where negative-emissions technologies come in. Carbon capture and storage—stripping carbon-dioxide from smokestacks and storing it underground—expands dramatically in the models, on the order of a ten- to one hundred-fold increase between two thousand thirty and two thousand fifty, reaching roughly ten billion tonnes a year by mid-century, with most studies bracketed between eight and fourteen. Hitting that would require building about eighty-five gigawatts of capture capacity every year, year after year—roughly comparable to today's global annual additions of wind and solar combined. Bioenergy with carbon capture and storage, or BECCS, looks attractive on paper because it can go carbon-negative, but at large scales it collides with land, water, and food. The authors are clear: these technologies appear pivotal in many two-degree and one point five-degree pathways, but their practical limits, costs, and public acceptance are unsettled. So if the near-term pledges don't yet hit the bullseye, where can more come from? One obvious lever is to raise the ambition of the contributions that cover two thousand twenty-five and two thousand thirty. Analyses like Climate Action Tracker point to theoretical headroom on the order of ten billion tonnes a year by two thousand thirty from tightening targets or simply over-delivering on what's already promised. Other levers exist, but they're smaller. Pull more sectors and gases under the umbrella, including the international transport sectors, and you're typically adding savings in the tenths to single gigaton range. Better finance, technology cooperation, and international initiatives—along with the surge of city, regional, and corporate action—can also help. The important point is additive momentum. No single lever closes the gap alone, but several together could. Under the hood, the temperature results carry explicit uncertainty bars because the team treats the climate system probabilistically. Rather than quote a single "Paris equals X degrees" answer, they give you a spread—what you expect at the median, what you get if you want a two-in-three confidence, and where the high tail sits. Post-two thousand thirty assumptions are made transparent too: does ambition stall, does it continue, or does it accelerate? It's a useful way to talk about risk, because what we choose after two thousand thirty matters as much as where we land in two thousand thirty. One more layer is how we count. Some countries propose targets as a percentage reduction from a historical year; others as an emissions intensity relative to gross domestic product; still others as a deviation from a hypothetical business-as-usual line. About thirty submissions were qualitative rather than quantitative. Historical inventory methods differ. The gases you include differ. Even with careful harmonization across studies, these choices move national and global totals around. That's why the paper spends time on the architecture of uncertainty, not just the medians. All of this sits inside the Paris framework's political engine: a ratchet and a mirror. Countries submit plans, they report transparently on progress, and every five years the world takes stock—looking at the science, at equity, and at what's actually happening on the ground—and then tightens. Non-state and sub-national action isn't a sideshow here; it's part of the ratchet. More than a thousand entities signed the Paris Pledge for Action in that first wave, and since then cities, regions, and firms have been racing ahead. Those moves don't replace national policy, but they can unlock co-benefits—cleaner air, better public health, stronger energy security—that make higher national ambition easier to sell and to sustain. So here's the bottom line. Those first Paris-era pledges did two things at once. They made a dent—roughly nine billion tonnes below where we'd be with no policy by two thousand thirty, roughly four below where current policies were pointing—and they left a large ambition gap compared to a least-cost two-degree path, on the order of eleven to fourteen billion tonnes in two thousand thirty. In temperature space, they moved us off a four-degree world toward something nearer three. That's a big shift. It's not the finish line. What comes next is about narrowing that gap without pretending it isn't there. Strengthen the pledges. Widen what's covered. Back it with finance, technology, and cooperation that make delivery plausible. Be honest about the role that carbon capture and potential negative-emissions options play in many model pathways, and just as honest about their limits. And keep the ratchet turning every five years, guided by a transparent read of the numbers and a shared sense of fairness. If there's a hopeful note in this analysis, it's that trajectories are not destiny. The system has inertia, yes, but it also has momentum. And momentum is something we can build.

Let's start with the simple question that sat under the Paris climate talks: if every country did what it put on paper in those early national pledges—the Intended Nationally Determined Contributions, or INDCs—where would the world end up? Not in the abstract. In tonnes of emissions in 2030 and in degrees of warming by 2100.

That's the lens Rogelj, den Elzen, Höhne and colleagues used to look at the first wave of pledges lodged around 2015 to 2016. Their answer is both encouraging and sobering. The pledges clearly bend the global curve downward, but they don't bend it far enough to keep us "well below" two degrees.

First, what exactly are we comparing? Think of four families of futures. There's a no-policy baseline, where countries keep doing what they were doing before climate policy had real bite.

There's a current-policy track, reflecting measures already on the books. Then there are the INDC pathways themselves—what countries said they would do unconditionally and what more they'd consider if financial or technology support showed up. Finally, there's a set of least-cost two-degree pathways: stylized, globally coordinated routes that spread effort to minimize overall costs while staying under two degrees with high confidence.

The team gathered global assessments covering about eighty-eight to ninety-six percent of 2012 greenhouse gas emissions, harmonized them into the same accounting system—one hundred-year global warming potentials—and translated each emissions pathway into temperatures using MAGICC, a climate model set up to give full probability ranges rather than single points.

Now the headline. If countries deliver their unconditional INDCs, global greenhouse gas emissions in 2030 land around fifty-five billion tonnes of carbon-dioxide equivalent, with most studies falling between fifty-two and fifty-eight. That's a meaningful step down—roughly nine billion tonnes below a no-policy world, and about four below the median projection for "current policies only." It is progress you can point to, but it is not the trajectory that takes you on a smooth, affordable glidepath to well below two degrees.

Some of that gap hides in how the pledges are written. Many are tidy, quantitative targets, but many are not. About three quarters lean on a "business-as-usual" baseline that the government defines, which means the absolute emissions level implied by the pledge depends on the shape of that baseline.

Roughly forty-five percent of submissions packaged both an unconditional and a conditional element. About a third were conditional only, and the rest were noncommittal about conditions. If every conditional element were fully met, the aggregate two thousand thirty total would fall by another two point four billion tonnes—small on the global scale, but not trivial.

Other uncertainties are more technical but just as important. Land-use emissions—changes in forests and soils—can be counted as part of a country's total, or handled separately under Kyoto-style rules. That choice moves national tallies around.

International aviation and shipping, big and growing sectors, generally sit outside national pledges. When you exclude sectors that the INDCs don't actually cover, the share of global emissions clearly addressed drops by at least eight percentage points from those optimistic coverage claims you sometimes hear. And when you allow for market transfers—where one country can buy credited reductions from another—modeling teams disagree on how to add those up.

That disagreement alone injects on the order of one billion tonnes of uncertainty into the two thousand thirty total.

Set those caveats to one side and line the curves up. Against a no-policy median of about sixty-five billion tonnes in two thousand thirty, the unconditional INDCs are better by design. But the distance to a cost-optimal two-degree pathway is large.

The median gap in two thousand thirty is about fourteen billion tonnes, with most estimates falling between ten to sixteen. Even if every conditional element of the pledges materialized on time, you're still roughly eleven billion tonnes too high. In plain terms: the Paris proposals took a real bite out of projected emissions, and they still left a very large slice on the plate.

What does that mean for temperatures? Translate the two thousand thirty INDC world through the probabilistic lens of MAGICC and you get a median warming by two thousand one hundred of about two point nine degrees Celsius. If you ask for a two-in-three chance, that median nudges up to around three point two degrees, and if you care about the high-end risks—the nine-in-ten bound—you're looking near three point nine.

Fully delivering the conditional pieces shaves only about two tenths of a degree off those medians. Better than where we were headed, yes. Consistent with "well below two"? No.

The team also asks what happens after two thousand thirty, because the path you take next depends on the foundations you lay now. They sketch three archetypes. One is stall: policy momentum fades and emissions drift back toward a world without climate policy.

Another is continue: post-two thousand thirty effort hums along at something like pre-two thousand thirty ambition. The third is accelerate: the world decides to push much harder. Start from the INDC two thousand thirty level and stay in the "continue" lane, and you still end up with that two point six to three point one degree window by century's end, centered around two point nine.

Even in the "accelerate" lane, you're starting late and high. Budgets tell the story more starkly. The carbon budget often cited for a fifty percent chance of holding one point five degrees—on the order of five hundred to six hundred billion tonnes of carbon-dioxide equivalent—is essentially exhausted under these pledges.

And for two degrees at a two-in-three chance, the budget is already overspent by around two thousand thirty on an INDC path.

When you burn through the budget early, the math forces you to do two hard things later. One is to bring net carbon-dioxide emissions to zero faster, typically somewhere between two thousand sixty and two thousand eighty in these scenarios, with overall greenhouse gases balancing sometime between two thousand eighty and two thousand one hundred in about two thirds of the least-cost cases. The other is to pull a lot of carbon back out of the atmosphere.

That's where negative-emissions technologies come in. Carbon capture and storage—stripping carbon-dioxide from smokestacks and storing it underground—expands dramatically in the models, on the order of a ten- to one hundred-fold increase between two thousand thirty and two thousand fifty, reaching roughly ten billion tonnes a year by mid-century, with most studies bracketed between eight and fourteen. Hitting that would require building about eighty-five gigawatts of capture capacity every year, year after year—roughly comparable to today's global annual additions of wind and solar combined.

Bioenergy with carbon capture and storage, or BECCS, looks attractive on paper because it can go carbon-negative, but at large scales it collides with land, water, and food. The authors are clear: these technologies appear pivotal in many two-degree and one point five-degree pathways, but their practical limits, costs, and public acceptance are unsettled.

So if the near-term pledges don't yet hit the bullseye, where can more come from? One obvious lever is to raise the ambition of the contributions that cover two thousand twenty-five and two thousand thirty. Analyses like Climate Action Tracker point to theoretical headroom on the order of ten billion tonnes a year by two thousand thirty from tightening targets or simply over-delivering on what's already promised.

Other levers exist, but they're smaller. Pull more sectors and gases under the umbrella, including the international transport sectors, and you're typically adding savings in the tenths to single gigaton range. Better finance, technology cooperation, and international initiatives—along with the surge of city, regional, and corporate action—can also help.

The important point is additive momentum. No single lever closes the gap alone, but several together could.

Under the hood, the temperature results carry explicit uncertainty bars because the team treats the climate system probabilistically. Rather than quote a single "Paris equals X degrees" answer, they give you a spread—what you expect at the median, what you get if you want a two-in-three confidence, and where the high tail sits. Post-two thousand thirty assumptions are made transparent too: does ambition stall, does it continue, or does it accelerate?

It's a useful way to talk about risk, because what we choose after two thousand thirty matters as much as where we land in two thousand thirty.

One more layer is how we count. Some countries propose targets as a percentage reduction from a historical year; others as an emissions intensity relative to gross domestic product; still others as a deviation from a hypothetical business-as-usual line. About thirty submissions were qualitative rather than quantitative.

Historical inventory methods differ. The gases you include differ. Even with careful harmonization across studies, these choices move national and global totals around.

That's why the paper spends time on the architecture of uncertainty, not just the medians.

All of this sits inside the Paris framework's political engine: a ratchet and a mirror. Countries submit plans, they report transparently on progress, and every five years the world takes stock—looking at the science, at equity, and at what's actually happening on the ground—and then tightens. Non-state and sub-national action isn't a sideshow here; it's part of the ratchet.

More than a thousand entities signed the Paris Pledge for Action in that first wave, and since then cities, regions, and firms have been racing ahead. Those moves don't replace national policy, but they can unlock co-benefits—cleaner air, better public health, stronger energy security—that make higher national ambition easier to sell and to sustain.

So here's the bottom line. Those first Paris-era pledges did two things at once. They made a dent—roughly nine billion tonnes below where we'd be with no policy by two thousand thirty, roughly four below where current policies were pointing—and they left a large ambition gap compared to a least-cost two-degree path, on the order of eleven to fourteen billion tonnes in two thousand thirty.

In temperature space, they moved us off a four-degree world toward something nearer three. That's a big shift. It's not the finish line.

What comes next is about narrowing that gap without pretending it isn't there. Strengthen the pledges. Widen what's covered.

Back it with finance, technology, and cooperation that make delivery plausible. Be honest about the role that carbon capture and potential negative-emissions options play in many model pathways, and just as honest about their limits. And keep the ratchet turning every five years, guided by a transparent read of the numbers and a shared sense of fairness.

If there's a hopeful note in this analysis, it's that trajectories are not destiny. The system has inertia, yes, but it also has momentum. And momentum is something we can build.

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