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<https://phys.org/news/2024-02-emergency-atmospheric-geoengineering-wouldnt-oceans.html>
Emergency
atmospheric geoengineering wouldn't save the oceans Rebecca Dzombak
29/02/2024
------------------------------
<https://phys.org/archive/29-02-2024/>

by Rebecca Dzombak, American Geophysical Union <http://www.agu.org/>
[image: Emergency atmospheric geoengineering wouldn't save the oceans] (a)
Annual mean global mean surface temperature above pre-industrial reference
temperature (b) Change in annual mean total depth ocean heat content (OHC)
relative to 2020–2030 conditions in Control. (c) Difference in vertical OHC
between end-of-simulation (2090–2100) conditions and present-day conditions
in Control. Credit: *Geophysical Research Letters* (2024). DOI:
10.1029/2023GL106132

Climate change is heating the oceans, altering currents and circulation
patterns responsible for regulating climate on a global scale. If
temperatures dropped, some of that damage could theoretically be undone.

But employing "emergency" atmospheric geoengineering later this century in
the face of continuous high carbon emissions would not be able to reverse
changes to ocean currents <https://phys.org/tags/ocean+currents/>, a new
study finds. This would critically curtail the intervention's potential
effectiveness on human-relevant timescales.

Oceans, especially the deep oceans, absorb and lose heat more slowly than
the atmosphere, so an intervention that cools the air would not be able to
cool the deep ocean on the same timescale, the authors found.

Stratospheric aerosol injection is a commonly discussed geoengineering
concept based on the idea that adding particles to the stratosphere could
help cool the surface of the planet by reflecting sunlight back into space.

This could help stabilize the planet if warming exceeds the 1.5 degree
Celsius (2.7 degrees Fahrenheit) cap set by the Paris Climate Agreement,
which the planet is on track to exceed under current emission rates.
(Global temperatures surpassed that threshold for several months in 2023
due to a combination of factors in addition to climate change
<https://phys.org/tags/climate+change/>, such as El Niño.)

But whether the injections would work is still heavily debated.

Previous research hints that a steady trickle of aerosol injections would
help cool the surface of the planet. But the new study suggests that while
an abrupt aerosol injection later this century could provide some ocean
cooling, it wouldn't be enough to nudge "stubborn" ocean patterns such as
Atlantic meridional overturning circulation, which some research
<https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023PA004629> finds is
already weakening
<https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GL103515>.

In that case, preexisting problems resulting from a warmed deep ocean, such
as altered weather patterns, regional sea level rise and weakened currents,
would remain in place even as the atmosphere and surface ocean cooled.

"The big picture result is that we believe we can control the surface
temperature of the Earth, but other components of the climate system will
not be so fast to respond," said Daniel Pflüger, a physical oceanographer
at Utrecht University who led the study. "We need to bring down emissions
as fast as possible. We're only talking about geoengineering because the
political will for emission mitigation is lacking."

The study was published in *Geophysical Research Letters*, AGU's journal
for high-impact, short-format reports with immediate implications spanning
all Earth and space sciences.

Warm planet, wild swings

Scientists know the surface of the planet can cool when large volumes of
particles are added to the atmosphere because of events such as volcanic
eruptions <https://phys.org/tags/volcanic+eruptions/>, which naturally emit
gases and fine particles. For instance, in 1815, an eruption at Mt. Tambora
in Indonesia launched so much material into the air that it cooled the
planet
<https://www.washingtonpost.com/news/capital-weather-gang/wp/2015/04/24/the-epic-volcano-eruption-that-led-to-the-year-without-a-summer/>
the following year.

Aerosol injection is based on a similar principle whereby the atmosphere is
made more reflective to send incoming solar radiation back into space,
cooling the planet.

Because of this, Pflüger wanted to test how the atmosphere, shallow ocean,
and deep ocean would respond to a steady trickle of aerosol injections over
decades as opposed to a big, abrupt injection beginning later in the
century. Would such an emergency measure be able to reverse ocean changes?

Pflüger and his colleagues simulated two aerosol injection scenarios, both
with high carbon emissions. In one scenario, people started slowly adding
particles into the atmosphere in 2020. In the other, beginning in 2080,
people inject a large initial quantity of aerosols to bring the amount of
warming back to 1.5 degrees Celsius and then continue to add enough
aerosols to maintain that level of cooling.

The team found that in the 2020 scenario, gradual stratospheric aerosol
injections maintain ocean temperatures, structure, and circulation patterns
roughly similar to today.

In the 2080 scenario, the abrupt aerosol injection cooled the Earth's
surface, including the top 100 meters (330 feet) of the ocean, to 1.5
degrees Celsius above the preindustrial average in about 10 years. However,
the deep oceans <https://phys.org/tags/deep+oceans/> remained warmer than
average, and critical ocean circulation patterns remained altered. The
intervention was not entirely successful.

The study shows that aerosol injection "might be able to slow down or
prevent climate tipping points from happening in the first place," said
Daniele Visioni, a climate scientist at Cornell University who was not
involved in the research. But aerosol injection "cannot magically restore
things."

"We cannot kick the can down the road forever," he said.

The extreme climate situations modeled here are neither desirable nor
likely, Pflüger said. However, they provide a good baseline for
understanding how Earth systems react to aerosol injections. Ultimately,
geoengineering can be useful—but it cannot be the whole solution, he said.

Relying on geoengineering is "in a way, madness," Pflüger said. "But the
situation is already quite mad."

The research is published
<https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2023GL106132> in the
journal *Geophysical Research Letters*.

*More information:* Daniel Pflüger et al, Flawed Emergency Intervention:
Slow Ocean Response to Abrupt Stratospheric Aerosol Injection, *Geophysical
Research Letters* (2024). DOI: 10.1029/2023GL106132
<https://dx.doi.org/10.1029/2023GL106132>

Le jeu. 15 févr. 2024 à 13:30, Geoengineering News <
geoengineeringne...@gmail.com> a écrit :

> *This item and others will be in the monthly “Solar Geoengineering Updates
> Substack” newsletter:* https://solargeoengineeringupdates.substack.com/
> -----------------------------------------------------------------
>
>
>
> https://essopenarchive.org/users/658235/articles/662678-flawed-emergency-intervention-slow-ocean-response-to-abrupt-stratospheric-aerosol-injection
>
>
> *Authors*
> Daniel Pflüger,Claudia Elisabeth Wieners,Leo van Kampenhout,René
> Wijngaard,Henk A. Dijkstra
>
> *Cite as*: Daniel Pflüger, Claudia Elisabeth Wieners, Leo van Kampenhout,
> et al. Flawed Emergency Intervention: Slow Ocean Response to Abrupt
> Stratospheric Aerosol Injection. ESS Open Archive . February 08, 2024.
> DOI: 10.22541/essoar.169447423.32818318/v2
>
> *08 February 2024*
>
> *Abstract*
> Given the possibility of irreversible, anthropogenic changes in the
> climate system, technologies such as solar radiation management (SRM) are
> sometimes framed as possible emergency interventions. However, little
> knowledge exists on the efficacy of such deployments. To fill in this gap,
> we perform Community Earth System Model 2 (CESM 2) simulations of an
> intense warming scenario on which we impose gradual early-century SRM or
> rapid late-century cooling (an emergency intervention), both realised via
> stratospheric aerosol injection (SAI). While both scenarios cool Earth's
> surface, ocean responses differ drastically. Rapid cooling fails to release
> deep ocean heat content or restore an ailing North Atlantic deep convection
> but partially stabilizes the Atlantic meridional overturning circulation.
> In contrast, the early intervention effectively mitigates changes in all of
> these features. Our results suggest that slow ocean timescales impair the
> efficacy of some SAI emergency interventions.
>
>
> *Source: ESS OPEN ARCHIVE *
>
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