Quantcast
Environmental News for a Healthier Planet and Life

Michael Mann: How Close Are We to 'Dangerous' Planetary Warming?

Climate

It is worth noting, incidentally, that this graph refutes an assertion recently made by climate change contrarian Judith Curry of Georgia Tech, during her remarks at a recent senate hearing where she appeared as a witness at the invitation of presidential hopeful and climate change denier Ted Cruz (R-TX). At the hearing, Curry bizarrely claimed that the rise in temperatures over the past 200 years is "not human" caused and that something other than industrial greenhouse gases is causing temperatures to climb. Examining the graph above, we can see that the statement is transparently false.

Now let us consider the implications that this all has for defining the limit of dangerous interference with the climate. In my Scientific American article last year Earth Will Cross the Climate Danger Threshold by 2036, I examined this precise question using a set of climate model simulations where the "equilibrium climate sensitivity" (ECS) of the model (how much warming one observes for a doubling of CO2 concentrations once the climate equilibrates to the rise) was varied. The results are shown in Fig. 3 below.

Fig 3. Greenhouse warming (in degrees C) as estimated by IPCC climate models.
Source: Scientific American (2014)

In these simulations, I used a 1750-1850 base period to define the pre-industrial average temperature baseline. As we can see from Fig. 2, there is little evidence of greenhouse warming over this early period. I focused on the Northern Hemisphere where data are available to meaningfully extend the record that far back (this was based on using the "Berkeley Earth Surface Temperature" dataset which extends back to AD 1750; details of data, code, etc. are provided here).

There are a number of things to note from Fig. 3. First of all, using the more appropriate 1750-1850 pre-industrial baseline, we see that the Northern Hemisphere average temperature (gray squiggly curve) has already warmed nearly 1.2C. Temperatures have exceeded 1C above pre-industrial levels for most of the past decade. So 2015 obviously won't be the first time this has happened, despite press reports to the contrary.

But let us return to the discussion of dangerous planetary warming. In the piece, I argued that the 3C value of ECS (i.e. where 3C warming of the globe ultimately results from increasing CO2 concentrations from their pre-industrial level of 280 ppm to a level of 560 ppm) is most likely given the various lines of scientific evidence. For this value of ECS I showed that limiting CO2 concentrations to 450 ppm (orange dashed curve in Fig. 3) would indeed limit warming to about 2C relative to pre-industrial. Problem solved? Not quite ...

While greenhouse warming would abate, the cessation of coal burning (if we were truly to go cold-turkey on all fossil fuel burning) would mean a disappearance of the reflective sulphate pollutants ("aerosols") produced from the dirty burning of coal. These pollutants have a regional cooling effect that has offset a substantial fraction of greenhouse warming, particularly in the Northern Hemisphere. That cooling would soon disappear, adding about 0.5C to the net warming. When we take this factor into account (orange dotted curve), the warming for 450 ppm stabilization is now is seen to approach 2.5C, well about the "dangerous" limit. Indeed, CO2 concentrations now have to be kept below 405 ppm (where we'll be in under three years at current rates of emissions) to avoid 2C warming (blue dotted curve).

So evidently, we don't have 1/3 of our total carbon budget left to expend, as implied by the IPCC analysis. We've already expended the vast majority of the budget for remaining under 2C. And what about 1.5C stabilization? We're already overdrawn.

The more we delay rapid reductions in fossil fuel burning, the more we will need to offset additional carbon emissions by sequestration of atmospheric carbon, either through massive reforestation projects, or 'geoengineering' technology such as "direct air capture," which involves literally sucking the CO2 back out of the atmosphere (It would be expensive, but the alternative—allowing dangerous planetary warming or implementing other potentially dangerous geoengineering schemes—could be far more costly).

Let's summarize. We're already close to 1.2C net warming for the Northern Hemisphere relative to a true pre-industrial baseline. If we were to suddenly halt all fossil fuel burning (and other human activities generating carbon emissions), then greenhouse warming would cease [interestingly, this is actually a consequence of two offsetting factors: there is future warming in the pipeline owing to the slow response of ocean warming to greenhouse gases, the so-called 'committed warming.' Offsetting this potential for additional future warming, however, is the fact that the ocean begins to absorb CO2 from the atmosphere, lowering CO2 concentrations. Recent work has argued that these two factors essentially cancel]. However, we would see another ~0.5C warming owing to the disappearance of sulphate pollutants, yielding 1.2C+0.5C = 1.7C total warming, perilously close to the 2C limit.

So what's the bottom line? Well, we're actually closer to the dangerous 2C warming mark than many experts acknowledge. And yet there is still hope for limiting warming to 2C despite claims to the contrary by some (see also this response).

Doing so would require rapid decarbonization of our economy and, perhaps, implementation of strategies and technologies for removing carbon from the atmosphere. If we decide that 2C is still too much warming, and seek a lower target of 1.5C, the challenge is more uphill. Reducing emissions alone won't be adequate, and sequestration of atmospheric carbon will be critical.

We can do this. No, we must do this.

Prev Page

EcoWatch Daily Newsletter

A view of a washed out road near Utuado, Puerto Rico, after a Coast Guard Air Station Borinquen MH-65 Dolphin helicopter crew dropped relief supplies to residents Tuesday, Oct. 3, 2017. The locals were stranded after Hurricane Maria by washed out roads and mudslides. U.S. Coast Guard photo by Petty Officer 3rd Class Eric D. Woodall / CC BY-NC-ND 2.0

By Coral Natalie Negrón Almodóvar

The Earth began to shake as Tamar Hernández drove to visit her mother in Yauco, Puerto Rico, on Dec. 28, 2019. She did not feel that first tremor — she felt only the ensuing aftershocks — but she worried because her mother had an ankle injury and could not walk. Then Hernández thought, "What if something worse is coming our way?"

Read More
Flooded battery park tunnel is seen after Hurricane Sandy in 2012. CC BY 2.0

President Trump has long touted the efficacy of walls, funneling billions of Defense Department dollars to build a wall on the southern border. However, when the U.S. Army Corps of Engineers (USACE) released a study that included plans for a sea wall to protect New Yorkers from sea-level rise and catastrophic storms like Hurricane Sandy, Trump mocked it as ineffective and unsightly.

Read More
Sponsored
A general view of fire damaged country in the The Greater Blue Mountains World Heritage Area near the town of Blackheath on Feb. 21, 2020 in Blackheath, Australia. Brook Mitchell / Getty Images

In a post-mortem of the Australian bushfires, which raged for five months, scientists have concluded that their intensity and duration far surpassed what climate models had predicted, according to a study published yesterday in Nature Climate Change.

Read More
Sea level rise causes water to spill over from the Lafayette River onto Llewellyn Ave in Norfolk, Virginia just after high tide on Aug. 5, 2017. This road floods often, even when there is no rain. Skyler Ballard / Chesapeake Bay Program

By Tim Radford

The Texan city of Houston is about to grow in unexpected ways, thanks to the rising tides. So will Dallas. Real estate agents in Atlanta, Georgia; Denver, Colorado; and Las Vegas, Nevada could expect to do roaring business.

Read More
Malala Yousafzai (left) and Greta Thunberg (right) met in Oxford University Tuesday. Wikimedia Commons / CC BY 2.0

What happens when a famous school striker meets a renowned campaigner for education rights?

Read More