A Climate Change Code Red

By Craig B. Smith and William D. Fletcher | 2021-10-01 12:00:00

In August 2021, the Intergovernmental Panel on Climate Change (IPCC) issued a report Climate Change 2021: The Physical Science Basis. This is the Sixth Assessment Report (AR6) covering the physical science of climate change. The report was written by 284 scientists from 66 countries. This is the first major international assessment of climate-change research since AR5 in 2013.

Because of the importance of this report, we developed this plain English summary to make the report more accessible to the general reader. The original report is 3,800 pages long with an Executive Summary and a summary of Frequently Asked Questions.

AR6 was issued in advance of the next major international climate conference, COP26, to be held in Glasgow in November 2021. It will be a gathering of representatives from almost every nation in the world to update commitments to reduce the greenhouse gas emissions made in the 2015 Paris Agreement. The Paris Agreement’s objective is to limit future global temperature increases to 2.0°C (3.6°F) and try to limit increases to 1.5 °C (2.7°F). This requires that net zero be reached by 2050, about 30 years from now.


  1. It is indisputable that human activities are causing climate change.
  2. Rising greenhouse gas concentrations are driving profound changes to the earth’s system.
  3. Climate change is already affecting every inhabited region across the globe with many changes in weather extremes.
  4. The scale of recent changes is unprecedented over many centuries to many thousands of years.
  5. Global warming of 1.5°C and 2°C will be exceeded during this century unless deep reductions in carbon dioxide and other greenhouse gas emissions occur in the coming decades.
  6. To stop global warming, it is necessary to achieve net zero, no net emissions of carbon dioxide and other greenhouse gases.
  7. Without aggressive actions, the earth’s temperature could exceed 3.0 °C by the end of this century and sea level could increase as much as 1 to 3 feet.
  8. Some changes, such as a rising sea level, will persist for centuries.



The IPCC report stresses the need to reach net zero. That is reducing emissions of CO2 and other greenhouse gases as low as practical. Any emissions that cannot be eliminated have to be offset by removing CO2 and other greenhouse gases from the atmosphere by artificial or natural means, such as by planting billions more trees. Only by eliminating human-caused greenhouse gases can global warming be stopped. Even then, much of the CO2 already in the atmosphere stay there for hundreds of years until slowly removed by natural processes.

* A metric ton is 1,000 kilograms or about 1.1 U.S. tons.


The earth’s surface temperature is the key indicator of the overall state of the earth’s climate. The likely total human-caused temperature increase of the earth’s average surface temperature is 1.07°C (1.9°F) as of 2019 [The temperature in 2021 is 1.17°C (2.1°F)]. The average temperature for 1850 to 1900 is used as a baseline by the IPCC.

The temperature increase is larger over land (1.59°C or 2.8°F) than over the ocean (0.88°C or 1.6°F). It is virtually certain that the land surface will continue to warm 1.4 to 1.7 times or more than the ocean surface.

It is unequivocal that human influence, mainly through the emissions of greenhouse gases, has warmed the atmosphere, ocean, and land. Global surface temperature has increased faster since 1970 than in any other 50- year period over at least the last 2,000 years. It is higher now than it has been for over 1,000 years.

Natural, nonhuman-caused, global warming is not significant.

The heat produced by global warming since the 1970s has mainly gone into warming the ocean (91%), followed by warming of land (5%) and the melting ice sheets and glaciers (3%). The atmosphere has warmed substantially since 1970 but, because it is composed of gases, it has absorbed only 1% of this heat.

Greenhouse gas warming has been partly masked by aerosol cooling. Total warming contributions equals approximately 1.5°C, with the cooling effect amounting to approximately 0.4°C, leaving the net increase approximately 1.1°C.

The global surface temperatures in any single year can vary above or below the long-term human-induced trend, due to substantial natural variability. There are at least four major differences between the recent warming and those of the past:

  1. It is warming almost everywhere.
  2. It is warming very rapidly.
  3. Recent warming reverses a long- term global cooling trend.
  4. It has been a long time since it has been this warm.


Increases in greenhouse gas concentrations since the start of the industrial revolution are unequivocally caused by human activities. Concentrations reached an annual average of 410 parts per million (ppm) for carbon dioxide in 2019. (Concentrations reached 415 ppm in 2021.)

In 2019, atmospheric CO2 concentrations were higher than at any time in at least 2 million years. Concentrations of methane and nitrous oxides were higher than at any time in at least 800,000 years.


The frequency and intensity of heavy precipitation events have increased since the 1950s over most land area where measurements are sufficient to establish trends. Monsoon precipitation has increased in some areas and decreased in others.


The global nature of glacier retreat is unusual with almost all the world glaciers retreating synchronously since the 1950s. Mountain and polar glaciers will continue melting for decades to centuries as long as the earth’s temperature is elevated.


The Arctic is warming faster than anywhere else on earth. It is virtually certain that the Arctic will continue to warm more than two times faster than the global average.

Late-summer Arctic sea ice was smaller than at any time in at least the past 1,000 years. The Arctic is likely to be practically ice free in September at least once before 2050 with more frequent occurrences for higher warming levels. The Greenland ice sheet will continue to lose ice for the rest of this century and beyond.

The Arctic is the biggest climate sensitive carbon pool on earth, storing twice as much carbon in its frozen soils, or permafrost than is currently stored in the atmosphere. Arctic warming could release greenhouse gases to the atmosphere and therefore significantly amplify climate change. Loss of permafrost carbon following permafrost thawing is irreversible.

The loss of sea ice and snow cover reduces the Arctic’s ability to reflect heat and contributes to warming of the Arctic.


There has been no significant trend in Antarctic sea ice area from 1979 to 2020 due to regionally opposing trends and large local variability. Antarctic sea ice is not expected to decrease. However, NASA‘s Grace satellite measurements indicate that the Antarctic ice cap is declining and has lost about 2,500 billion tons of ice since 2005.


It is virtually certain that the global upper ocean (0-700 m or 0-2,300 ft) has warmed since the 1970s. The ocean has warmed faster over the past century than since the end of the last deglacial transition, around 11,000 years ago.


Man-made carbon dioxide emissions are the main cause of global acidification of the open ocean. This acidification is unusual in the last 2 million years. Ocean acidification and ocean deoxygenation will continue and changes are irreversible over centuries or longer.


Global mean sea level increased by 0.2 meters (7.9 inches) between 1901 and 2018. Thermal expansion explained 50 percent of sea level rise during 1971 to 2018, while ice loss from glaciers contributed 22 percent, from ice sheets 20 percent, and changes in land water storage 8 percent.

The average rate of sea level rise was 1.3 mm (0.05 inches) per year between 1901 and 1971 but has increased to 3.7 mm (0.15 inches) per year between 2000 and 2018. The global mean sea level has risen faster since 1900 than over any preceding century in at least the last 3,000 years.

Sea level rise will continue throughout this century.

Approximately two-thirds of the global coastline will see sea level rise within +/- 20 percent of the global increase. Due to sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by the end of this century.

In the longer-term, sea level is committed to rise for centuries or longer due to continuing deep ocean warming and ice sheet melt and could rise as much as 2-6 m (6.6-20 ft).


Climate zones have shifted pole-ward in both hemispheres. The growing season has on average lengthened by up to two days per decade since the 1950s in the northern hemisphere, excluding the tropics.


Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. Observed changes in extremes such as heat waves, heavy precipitation, droughts, and tropical cyclones (hurricanes and typhoons) are occurring. The frequency of these unprecedented extreme events will increase with increasing global warming. Compound events are likely to be more common, such as when two weather events occur simultaneously. This includes increases in the frequency of concurrent heat waves and droughts on the global scale, fire weather in some regions of all inhabited continents, and compound flooding in some locations.


Latency, the delay between cause and effect, is likely with many of the climate-induced changes the earth is experiencing. It takes a very long time for the earth to fully adjust to climate changes. If greenhouse gas emissions were to stop today, it could be decades before the full effects of past emissions becomes apparent. Many changes due to past and future greenhouse gas emissions are irreversible for centuries, especially changes in the ocean, ice sheets and the sea level.


A carbon budget is the amount of cumulative CO2 that can be released for a given increase in the earth’s average temperature. About 2,390 billion metric tons CO2 have been released into the atmosphere by human activities between 1850 and 2019. For every 1,000 billion metric tons of CO2 emitted, the temperature rise is likely to be about 0.45°C.

The IPCC estimates that the remaining carbon budget to reach 1.5°C is about 400 billion metric tons and to reach 2.0°C is about 1,150 billion metric tons. Today’s annual CO2 emissions are about 40 billion metric tons per year and increasing. At this rate, it will take about 10 years for the earth’s temperature to reach 1.5°C and less than 30 years to reach 2.0°C.


About 45 percent of greenhouse gas emissions remain in the atmosphere, causing the greenhouse effect. The ocean and land have taken up the remainder, about 55 percent, over the past sixty years. This fraction is expected to decline in the future if CO2 emissions continue to increase, causing more CO2 to remain in the atmosphere.

It is becoming apparent that the natural processes are beginning to respond to increasing CO2 emissions in a way that will weaken nature’s capacity to take up CO2 in the future. Land and ocean become less effective in absorbing emissions. If a higher proportion of emitted CO2 remains in the atmosphere it will accelerate global warming.

The ability to remove CO2 from the atmosphere is under development. The technical and economic feasibility of removing enough CO2 from the atmosphere to make a difference has not yet been demonstrated.


There is a near-linear relationship between cumulative man-made CO2 emissions and the global warming they cause. Global warming extremes become larger in frequency and intensity with every increment of greenhouse gas emission.

Increasing emissions increase the frequency and intensity of hot extremes, marine heat waves, heavy precipitation, agricultural ecological droughts in some regions, and the intensity of tropical cyclones, as well as reductions in Arctic sea ice, snow cover, and permafrost.


Emissions reductions in 2020 associated with measures to reduce the spread of COVID-19 led to temporary but detectable reductions of air pollution. Global and regional climate responses to this temporary event are, however, undetectable above natural variability. Atmospheric CO2 concentrations continued to rise in 2020, with no detectable decrease in observed CO2 growth rate.


To assess the future, the IPCC used computer models to develop scenarios depicting the range of realistic possibilities, depending upon the global response to global warming. AR6 states that these scenarios are not predictions. They provide “what-if’” investigations of various realistic future developments. They span the range of possibilities from “business as usual” with no real effort to reduce greenhouse gas emissions, to aggressive global efforts to limit global warming to no more that 1.5 or 2.0°C. The scenarios are summarized in Table 1.


The IPCC scenarios resulted in a wide range of climate futures, largely dependent upon the rate at which greenhouse gas emissions are reduced. The first two scenarios represent what could happen if aggressive actions are taken immediately to reduce emissions. The last two represent what could happen if less aggressive or no real efforts are taken. The middle scenario is what would happen if the current Paris Agreement targets are met.

According to this analysis, global warming of 1.5°C and 2°C will be exceeded during this century unless deep reductions in CO2 and other greenhouse gas emissions occur in the coming decades. (The authors of this summary believe the earth’s temperature will exceed 2°C.)

If global net negative CO2 emissions were to be achieved and be sustained, the global CO2 induced surface temperature increase would be gradually reversed but other climate changes would continue in their current direction for decades to thousands of years. For instance, it would take several centuries or longer for global mean sea level to reverse course even under large net negative CO2 emissions.

Many regions are predicted to experience an increase in the probability of compound events with higher global warming. In particular, concurrent heat waves and droughts are likely to become more frequent.


It is unlikely that major tipping points will be exceeded this century. Many systems have natural or structural thresholds. If conditions exceed those thresholds, the result can be sudden changes or even collapses in health, productivity, utility, or behavior. The probability of low likelihood but high impact outcomes increases with higher global warming levels. Abrupt responses and tipping points of the climate system, such as increased Antarctic ice sheet melt and forest dieback cannot be ruled out.


Due to the fact that greenhouse gases in the atmosphere, especially CO2, will stay there for a very long time, it will take time before reduced global surface warming will be detectable — about twenty to thirty years.


Very low or low greenhouse gas emission scenarios would have rapid and sustained effects to limit human caused climate change compared with scenarios with high or very high greenhouse gas emissions effects. A near-term benefit would be reduced air pollution and improved public health.


The specific actions needed to reduce greenhouse gas emissions were beyond the scope of the IPCC report.

Smith and Fletcher are co-authors of Reaching Net Zero: What It Takes To Solve The Global Climate Crisis. Oxford, UK: Elsevier 2020

Peace Magazine October-December 2021

Peace Magazine October-December 2021, page 12. Some rights reserved.

Search for other articles by Craig Smith here
Search for other articles by William Fletcher here

Peace Magazine homepage