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submitted 6 months ago by silence7@slrpnk.net to c/climate@slrpnk.net
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[-] Coasting0942@reddthat.com 4 points 6 months ago

it would take well over a decade for the effects to even start setting in.

lol. Every fascist wannabe around the world would win in a landslide.

[-] umbrella@lemmy.ml 3 points 6 months ago
[-] Coasting0942@reddthat.com 8 points 6 months ago

As more extreme policies become required, fascists gain power because of the increasing disruption to the way of life that the average person in the region is accustomed to.

“They’re taking away your hamburgers, your cars, etc etc”

[-] umbrella@lemmy.ml 2 points 6 months ago* (last edited 6 months ago)

i think the people who were gonna be fascists anyway are already drunk on that mentality, regardless of what we tell them at this point.

i think theres already a foundation being built in the world's stage to fight back.

i guess we will have to see on that one.

this post was submitted on 19 Mar 2024
175 points (98.3% liked)

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Discussion of climate, how it is changing, activism around that, the politics, and the energy systems change we need in order to stabilize things.

As a starting point, the burning of fossil fuels, and to a lesser extent deforestation and release of methane are responsible for the warming in recent decades: Graph of temperature as observed with significant warming, and simulated without added greenhouse gases and other anthropogentic changes, which shows no significant warming

How much each change to the atmosphere has warmed the world: IPCC AR6 Figure 2 - Thee bar charts: first chart: how much each gas has warmed the world.  About 1C of total warming.  Second chart:  about 1.5C of total warming from well-mixed greenhouse gases, offset by 0.4C of cooling from aerosols and negligible influence from changes to solar output, volcanoes, and internal variability.  Third chart: about 1.25C of warming from CO2, 0.5C from methane, and a bunch more in small quantities from other gases.  About 0.5C of cooling with large error bars from SO2.

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