
Stop emissions, stop warming: A climate reality check
https://www.theclimatebrink.com/p/climat...op-when-we
EXCERPT (Andrew Dessler): . . . In case you want a slightly nerdier description of why temperatures stop rising, you’re in luck. When we stop emitting greenhouse gases, the future behavior of Earth’s temperature depends on the relative speed of two critical processes:
1. The rate at which CO₂ is removed from the atmosphere (through absorption by oceans and land).
2. The rate at which heat is transferred from the surface ocean (a layer with small heat capacity) into the deep ocean (which has very large heat capacity).
To illustrate this, consider two extreme scenarios:
Scenario 1: CO2 removal is very slow, ocean heat transfer is very fast. Under this scenario, the Earth’s temperature would continue to rise long after emissions stop. This happens because the persistent CO2 in the atmosphere would keep trapping heat, while rapid heat mixing into the deep ocean would increase the effective heat capacity of the surface ocean. A higher surface heat capacity means it would take longer for the surface ocean to reach equilibrium for any given CO2 level. Thus, when emissions cease, the surface layer is much cooler than equilibrium with atmospheric CO2 and it must warm over the following centuries to reach equilibrium.
Scenario 2: CO2 removal is very fast, ocean heat transfer is very slow. Under this scenario, CO2 levels drop quickly after emissions stopped. The slow mixing limits the heat capacity of the surface ocean, causing the temperature of the surface layer to remain very close to equilibrium with atmospheric CO2 levels. As CO2 concentrations decrease, the surface ocean will therefore cool to stay near equilibrium.
In our actual climate system, these two processes happen at roughly comparable rates. The cooling effect of declining CO2 levels tends to offset the warming caused by heat transfer into the deep ocean. This balance means that, after emissions stop, global temperatures are expected to remain relatively stable instead of significantly rising or falling... (MORE - missing details)
Other stuff. Twitter/X is dead for climate science. If you were someone who went to Twitter to read about climate, head over to Bluesky — most of the climate community I engage with are and, as an added bonus, it’s not a Nazi bar. Read more about Bluesky on Andrew Rumbach’s recent substack post. I’m almost exclusively on Bluesky; you can find me here,
If you can’t get enough of my perspectives on climate and energy, I gave a “fireside chat” at the Texas A&M Innovation Forward conference a few weeks ago. You can watch it here: https://youtu.be/E0M75Fao96M
https://www.theclimatebrink.com/p/climat...op-when-we
EXCERPT (Andrew Dessler): . . . In case you want a slightly nerdier description of why temperatures stop rising, you’re in luck. When we stop emitting greenhouse gases, the future behavior of Earth’s temperature depends on the relative speed of two critical processes:
1. The rate at which CO₂ is removed from the atmosphere (through absorption by oceans and land).
2. The rate at which heat is transferred from the surface ocean (a layer with small heat capacity) into the deep ocean (which has very large heat capacity).
To illustrate this, consider two extreme scenarios:
Scenario 1: CO2 removal is very slow, ocean heat transfer is very fast. Under this scenario, the Earth’s temperature would continue to rise long after emissions stop. This happens because the persistent CO2 in the atmosphere would keep trapping heat, while rapid heat mixing into the deep ocean would increase the effective heat capacity of the surface ocean. A higher surface heat capacity means it would take longer for the surface ocean to reach equilibrium for any given CO2 level. Thus, when emissions cease, the surface layer is much cooler than equilibrium with atmospheric CO2 and it must warm over the following centuries to reach equilibrium.
Scenario 2: CO2 removal is very fast, ocean heat transfer is very slow. Under this scenario, CO2 levels drop quickly after emissions stopped. The slow mixing limits the heat capacity of the surface ocean, causing the temperature of the surface layer to remain very close to equilibrium with atmospheric CO2 levels. As CO2 concentrations decrease, the surface ocean will therefore cool to stay near equilibrium.
In our actual climate system, these two processes happen at roughly comparable rates. The cooling effect of declining CO2 levels tends to offset the warming caused by heat transfer into the deep ocean. This balance means that, after emissions stop, global temperatures are expected to remain relatively stable instead of significantly rising or falling... (MORE - missing details)
Other stuff. Twitter/X is dead for climate science. If you were someone who went to Twitter to read about climate, head over to Bluesky — most of the climate community I engage with are and, as an added bonus, it’s not a Nazi bar. Read more about Bluesky on Andrew Rumbach’s recent substack post. I’m almost exclusively on Bluesky; you can find me here,
If you can’t get enough of my perspectives on climate and energy, I gave a “fireside chat” at the Texas A&M Innovation Forward conference a few weeks ago. You can watch it here: https://youtu.be/E0M75Fao96M