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Home » How Aerosols Brighten Clouds — and Cool the Planet: Sarah J. Doherty (Transcript)

How Aerosols Brighten Clouds — and Cool the Planet: Sarah J. Doherty (Transcript)

Here is the full transcript of atmospheric scientist Sarah J. Doherty’s talk titled “How Aerosols Brighten Clouds — and Cool the Planet” at TED 2024 conference.

Listen to the audio version here:

TRANSCRIPT:

So I’m a climate scientist, and based on that, I bet you think I’m here to tell you about all the ways that we’re making the climate warmer. But I’m not actually going to do that today because I think you already know that part of the story. I want to tell you instead a story about unintended consequences.

For many of us, it’s really easy to forget that in addition to emitting a lot of greenhouse gases, humans have been adding a lot of particulate pollution to the atmosphere. These small particles, which we scientists call aerosols, are responsible for the death of between four and 10 million people a year around the globe. For much of the world, this remains a major public health crisis.

And because of that, there are significant efforts underway to clean up the source of these emissions, which is fantastic. But here’s the thing. The unintended consequence of doing that is that we might actually be accelerating climate warming.

The Cooling Effect of Aerosols

And that’s because most of these aerosols actually cool climate. I spent my career as a climate scientist studying how aerosols in the atmosphere around the globe absorb sunlight in the atmosphere and increase the reflection of sunlight away from our planet. Aerosols directly scatter sunlight back to space, and when they mix into clouds, they can make clouds brighter or more reflective.

And both of these effects act to cool the climate by reducing the amount of sunlight that’s available to heat the surface. We estimate that right now, aerosols from human activities are cooling climate by about half a degree Celsius. In other words, if it weren’t for these climate effects, we would already be experiencing significantly worse climate impacts than we already are.

The Conundrum of Cleaning Up the Air

So here’s a conundrum. As we clean up the air for human health, we’re reducing the concentration of these aerosols in the atmosphere, and we’re removing the source of climate cooling. And because these aerosols only last in the atmosphere for about a week, their cooling effect goes away almost immediately after we stop emitting them, unlike greenhouse gases, which continue to warm for decades to centuries.

Here’s a second conundrum. While our best estimate is that aerosols are cooling climate by about half a degree Celsius, this effect could be quite a bit smaller, or it could be a lot bigger.

It’s possible that aerosols right now are cooling climate by up to almost a full degree Celsius. And because we don’t know how much of a cooling effect these aerosols are currently providing, we don’t know how much of a climate warming they’re going to unmask as we clean up the air. So let’s step back and talk a little bit more about how it is that aerosols cool climate and why these effects are so uncertain.

How Aerosols Cool Climate

So aerosols mostly cool climate by increasing the reflection of sunlight from clouds. This increase in cloud brightness from aerosols is not generally very visibly apparent because clouds are just so naturally variable in their brightness. But a case where it is really visually obvious is in what we call ship tracks.

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So what you’re looking at here is a satellite image off the west coast of North America. And you can see that there are these lines of clouds that are brighter or more reflective than the clouds around them. So to understand what’s going on here, you first have to know that cloud droplets always form on an aerosol.

Out over the ocean, there’s just not generally that many aerosols in the atmosphere. So what you end up with is a cloud with a small number of larger droplets. Well, along comes your ship, and it’s adding aerosols to the atmosphere and to the clouds.

The Variability of Cloud Brightness

The water gets distributed over those aerosols, and you now have a cloud with a large number of smaller droplets. This change in droplet size increases the reflectivity of the cloud. Now this is not just happening where ship emissions are mixing into clouds.

This is actually mostly happening over broad regions of the planet where pollution aerosols mix into clouds. So I’ve shown you here a very striking example of where pollution aerosols are clearly making clouds more reflective. But this actually doesn’t always happen.

And why is that? Well, I’m going to give you scientists’ two very favorite answers. It’s complicated. And it depends. If you have ever looked at clouds for very long, you could see that they’re incredibly complex, and they are constantly evolving. When you add aerosols to clouds, it doesn’t just change their droplet size, it actually can then change how they evolve in ways that also affect cloud brightness. Depending on the details of the atmospheric conditions, clouds can be made either more or less reflective with the addition of aerosols, or not really changed at all.

Mimicking the Effect of Pollution Aerosols

But what we do know is that under the right conditions, aerosol additions to clouds can make them quite a bit brighter. So this poses an interesting question. Might it be possible to rapidly reduce climate warming by mimicking this effect that pollution aerosols are already having on clouds, but do so by adding natural aerosols rather than pollution to clouds?

Specifically by adding sea salt aerosol to clouds over the ocean, where sea salt aerosols already act as seeds for cloud droplet formation. Well we start with studying this problem using computer models. And when we add tiny sea salt aerosols to the clouds over the ocean in global climate models, we find that brightening just a fraction of the clouds over the ocean does, in fact, rapidly and significantly reduce climate warming from greenhouse gases.

So these models indicate it is possible.