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Expert Voices

How fast can we stop Earth from warming?

The ocean retains heat for much longer than land does.
The ocean retains heat for much longer than land does. (Image credit: Aliraza Khatri's Photography via Getty Images)

This article was originally published at The Conversation. (opens in new tab) The publication contributed the article to Space.com's Expert Voices: Op-Ed & Insights.

Richard B. (Ricky) Rood (opens in new tab), Professor of Climate and Space Sciences and Engineering, University of Michigan

Global warming doesn't stop on a dime. If people everywhere stopped burning fossil fuels tomorrow, stored heat would still continue to warm the atmosphere.

Picture how a radiator heats a home. Water is heated by a boiler, and the hot water circulates through pipes and radiators in the house. The radiators warm up and heat the air in the room. Even after the boiler is turned off, the already heated water is still circulating through the system, heating the house. The radiators are, in fact, cooling down, but their stored heat is still warming the air in the room.

This is known as committed warming (opens in new tab). Earth similarly has ways of storing and releasing heat.

Emerging research is refining scientists' understanding of how Earth's committed warming will affect the climate. Where we once thought it would take 40 years or longer for global surface air temperature to peak once humans stopped heating up the planet, research now suggests temperature could peak in closer to 10 years (opens in new tab).

But that doesn't mean the planet returns to its preindustrial climate or that we avoid disruptive effects such as sea level rise.

I am a professor of climate science, and my research and teaching focus on the usability of climate knowledge by practitioners such as urban planners, public health professionals and policymakers. With a new report on mitigating climate change (opens in new tab) expected from the Intergovernmental Panel on Climate Change in early April, let's take a look at the bigger picture.

How understanding of peak warming has changed

Historically, the first climate models (opens in new tab) represented only the atmosphere and were greatly simplified. Over the years, scientists added oceans (opens in new tab), land, ice sheets, chemistry and biology.

Today's models can more explicitly represent the behavior of greenhouse gases, especially carbon dioxide. That allows scientists to better separate heating due to carbon dioxide in the atmosphere from the role of heat stored in the ocean.

Thinking about our radiator analogy, increasing concentrations of greenhouse gases in Earth's atmosphere keep the boiler on — holding energy near the surface and raising the temperature. Heat accumulates and is stored, mostly in the oceans (opens in new tab), which take on the role of the radiators. The heat is distributed around the world through weather and oceanic currents.

The current understanding (opens in new tab) is that if all of the additional heating to the planet caused by humans was eliminated, a plausible outcome is that Earth would reach a global surface air temperature peak in closer to 10 years than 40 (opens in new tab). The previous estimate of 40 or more years has been widely used over the years, including by me (opens in new tab).

It is important to note that this is only the peak, when the temperature starts to stabilize — not the onset of rapid cooling or a reversal of climate change.

I believe there is enough uncertainty to justify caution (opens in new tab) about exaggerating the significance of the new research's results. The authors applied the concept of peak warming to global surface air temperature. Global surface air temperature is, metaphorically, the temperature in the "room," and is not the best measure of climate change. The concept of instantly cutting off human-caused heating is also idealized and entirely unrealistic — doing that would involve much more than just ending fossil fuel use, including widespread changes to agriculture — and it only helps illustrate how parts of the climate might behave.

Even if the air temperature were to peak and stabilize, "committed ice melting (opens in new tab)," "committed sea level rise" and numerous other land and biological trends would continue to evolve from the accumulated heat. Some of these could, in fact, cause a release of carbon dioxide and methane (opens in new tab), especially from the Arctic and other high-latitude reservoirs that are currently frozen (opens in new tab).

For these reasons and others, it is important to consider the how far into the future studies like this one look.

Oceans in the future

Oceans will continue to store heat and exchange it with the atmosphere. Even if emissions stopped, the excess heat that has been accumulating in the ocean since preindustrial times would influence the climate for another 100 years or more.

Because the ocean is dynamic, it has currents, and it will not simply diffuse its excess heat back into the atmosphere. There will be ups and downs as the temperature adjusts.

The oceans also influence the amount of carbon dioxide in the atmosphere, because carbon dioxide is both absorbed and emitted by the oceans. Paleoclimate studies show (opens in new tab) large changes in carbon dioxide and temperature in the past, with the oceans playing an important role.

The chart shows how excess heat — thermal energy — has built up in ocean, land, ice and atmosphere since 1960 and moved to greater ocean depths with time. TOA CERES refers to the top of the atmosphere. (Image credit: Karina von Schuckman, LiJing Cheng, Matthew D. Palmer, James Hansen, Caterina Tassone, et al., CC BY-SA)

Countries aren't close to ending fossil fuel use

The possibility that a policy intervention might have measurable impacts in 10 years (opens in new tab) rather than several decades could motivate more aggressive efforts to remove carbon dioxide from the atmosphere. It would be very satisfying to see policy interventions having present rather than notional future benefits.

However, today, countries aren’t anywhere close to ending their fossil fuel use. Instead, all of the evidence points to humanity experiencing rapid global warming (opens in new tab) in the coming decades.

Our most robust finding is that the less carbon dioxide humans release, the better off humanity will be. Committed warming and human behavior point to a need to accelerate efforts both to reduce greenhouse gas emissions and to adapt to this warming planet now, rather than simply talking about how much needs to happen in the future.

This article is republished from The Conversation (opens in new tab) under a Creative Commons license. Read the original article (opens in new tab).

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Richard B. Rood

Richard Rood is a Professor at the University of Michigan in the Department of Climate and Space Sciences and Engineering (CLaSP) and he is also appointed in the School for Environment and Sustainability. He is part of the Core Team of the Great Lakes Integrated Sciences and Assessments (GLISA) Center. Rood teaches several course on climate change and the use of climate-knowledge in planning and management. This has evolved into a curriculum on climate change problem solving. Professor Rood has made research contributions to several fields. His numerical algorithms are used in climate models, weather-forecast models, and atmospheric chemistry models. He has also been a leader in developing merged model-observation datasets to study chemistry and climate. As a member of the Senior Executive Service at the National Aeronautics and Space Administration (NASA), Rood received recognition for his ability to lead both scientific and high performance computing activities.