Overshooting moist hot air into the stratosphere will likely transfer much of the heat out into space, and the moisture will crystalize out at submicron size.The last large volcanic eruption demonstrated the physics, the southern hemisphere did temporarily cool due to the added cloud ice.
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"The Hunga Tonga volcanic eruption in early 2022 also affects the past two years. Jenkins et al.7 estimate that water vapor injected into the stratosphere caused a small warming forcing (+0.12 W/m2), but Schoeberl et al.8 found that the cooling effect of stratospheric aerosols injected by Hunga Tonga yielded a net cooling effect, with forcing peaking in mid-2022 at about –0.5 W/m2. Averaged over 2022, Hunga Tonga may have been about –0.3 W/m2, but by today it is smaller."
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Thanks, James. I've added a possible CDR linkage at the end.
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Michael et al
You might appreciate this section from the attached short (unpublished) paper from Franz Oeste and myself on our Climate Catalyst proposal:
Removal of black carbon aerosol
A largely unrecognised problem is that of black soot particles inducing convection that carries them up into the stratosphere, driven by sun heating. Soot particles actively collect and store halogenated gases from the air and deliver them to the stratosphere. Soot particles therefore have a disproportionately damaging effect on the stratospheric ozone layer. Since the stratosphere migrates generally poleward, some of these black carbon particles contribute to Arctic haze, and eventually sediment in snow, discolouring it and thereby increasing its melting rate.
Climate catalyst lightens soot particles and changes their water-repelling (hydrophobic) nature to water-attracting (hygroscopic). This both reduces their convection effect, and makes them wash out in rain more easily, preventing them from ascending to the stratosphere and polar regions.
Climate catalyst also removes methane from the troposphere in a photocatalytic cycle, leaving less methane to migrate to the stratosphere where it oxidises and releases water.
Just so there’s something relevant to this email group: Climate Catalyst with an iron content diffusely fertilises phytoplankton when it sediments in the sea, at least temporarily raising surface pH a little over a wide area (assuming it’s an HNLC ocean area), and reducing CO2 outgassing or absorbing CO2 over that area.
Clive
From: carbondiox...@googlegroups.com <carbondiox...@googlegroups.com> On Behalf Of Michael Hayes
Sent: Sunday, September 24, 2023 8:47 PM
To: James Bowery <jabo...@gmail.com>
Cc: Carbon Dioxide Removal <CarbonDiox...@googlegroups.com>
Subject: Re: [CDR] Tropopause overshoot as source of stratospheric greenhouse H2O
James, et al.,
Thank you for such interesting and challenging questions. I can't directly answer your questions at this time, yet there is a possible natural anolog to injection of hot air/BC at the tropopause level.
A large forest fire can create a spherical vortex with a heavy BC load in the middle stratosphere. Because of the solar heat collected by the BC, the spherical vortex is maintained for extended periods of time, days to months after the forest fire.
The stratospheric H20 that the wetted BC collects and takes out of the stratosphere may offset the immediate longwave heating of the stratosphere by the BC. However, While in the vortex, the BC likely only heats up the air volume in the vortex.
As a final note, matching the volume of the hot air/BC that a forest fire can generate is likely well beyond anything we can do with one structure, yet we may be able to generate hotter air with a higher BC content, and heavier BC particals, than what typically makes it past the tropopause. If so, the resulting stratospheric spherical vortex might gain higher altitudes thus increasing longwave radiation into space.
On Sat, Sep 23, 2023, 3:18 PM James Bowery <jabo...@gmail.com> wrote:
It would be really helpful to have a set of differential equations for just a column of air that takes as an input the partial pressure of various gasses at various altitudes and temperature at various altitudes, which describes the power spectrum at various altitudes. While I'm perfectly aware this dynamical system would not be representative of the global system, it could overcome some basic misunderstandings about forcing dynamics of global warming that afflict even PhD physicists:
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On Sep 24, 2023, at 5:27 PM, James Bowery <jabo...@gmail.com> wrote:
After some searching I found this python package:
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Belatedly, is there a CDR story in this thread?