roadside_picnic
4 months ago
One thing that a lot of people seem to miss is that we talk about sea-level rise so much in relation to climate change because it's one of the things we can at least reasonably predict (even if the how much and when is hard). But the impacts of climate change increasing become hard to model as the world falls out of predictable patterns.
A great example of just how extreme things can get was the last major climate change event ~10,000-20,000 years ago (which will likely be minuscule in comparison to what we're going through now in the geological sense once this plays out).
The Channeled Scablands of Eastern Washington[0] have a very distinctive geology. For many years it was believed that these features were carved out slowly over hundreds of thousands of years. It turns out they we created in hours, around 15,000 years ago (humans were already living in WA at that time). They were created by the Missoula floods. There used to be a glacial lake over what is now Missoula Montana which would have current day Missoula under 1,000 feet of water. The glacial damns holding back this lake started to break down resulting in frequent floods the scale of which it's hard to fathom. The peak flow is estimated to have been 6.5 cubic miles per hour (for context, the peak flow observed over Horseshoe falls was 0.0055 cubic miles per hour, the Amazon river flows at an average of 0.18 cubic miles per hour)
Imagine driving East on 1-90 from Seattle towards Spokane, then as you get through the Cascades you suddenly see a 200 foot wall of water racing towards you across the horizon.
That event was in the past and it still took us a long time to piece together what actually happened. As we head into states of climate never witnessed by humans, it's genuinely hard to predict what might happen other than "this probably won't be good". Humans have made a lot of progress in the last 10,000 years, but it's no coincidence that the last 10,000 years have been some of the most stable in the Earth's climate history.