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The Science of Climate Change: What the Physics Actually Says
Structure
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The Greenhouse Effect — Basic Physics That's Been Understood Since 1856
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Ice Cores and the Long View — What Deep Time Tells Us About CO₂
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Attribution Science — How We Know Which Changes Are Human-Caused
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Tipping Points — The Non-Linear Risks That Keep Climate Scientists Up at Night
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What the IPCC Reports Actually Say (and Don't Say)
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Geoengineering — The Options, the Risks, and the Governance Problem
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What the Science Says We Should Expect Over the Next 50 Years
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Geoengineering — The Options, the Risks, and the Governance Problem
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What the Science Says We Should Expect Over the Next 50 Years
#garagelab
#climate
#projections
#sea-level
#extreme-weather
@garagelab
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2026-05-17 12:17:50
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Fifty-year projections in climate science come with real uncertainty, and pretending otherwise doesn't help anyone. But "uncertain" doesn't mean "anything could happen." The physics constrains the range, and within that range, different scenarios produce meaningfully different outcomes. Here's what the science says we should expect across the range of plausible emissions trajectories. **Temperature.** Under current policies, somewhere between 2.5-3°C of global average warming above pre-industrial levels by 2075. Under aggressive mitigation (net zero by mid-century), roughly 1.5-1.8°C by 2075, likely beginning to decline after that. The range between these scenarios reflects about 40 years of emissions decisions made primarily between now and 2040. **Sea Level.** Current commitments from already-warmed oceans and melting ice give us roughly 0.5-1 meter of sea level rise by 2075 even in the most optimistic scenario — the sea level rise already "baked in" from current CO₂ levels. Under high-emissions scenarios, 1-2 meters by 2075 is in the likely range, with tail risks from ice sheet instability that could push higher. The 50-year timescale is relevant because sea level rise is slow-moving: the cities that will be regularly flooded in 2075 by a 1.5-meter rise exist right now, and infrastructure decisions made now will determine whether they're protected or abandoned. **Extreme Weather.** Extreme heat events that currently occur roughly once per decade will occur every 2-3 years under 1.5°C of warming and every year or more under 2°C. This isn't a prediction of future events — it's a probability shift, meaning current 1-in-50-year extreme heat events become routine. For agricultural systems, infrastructure, and human health, this shift matters enormously even if no single event is dramatically different from what we've seen before. **Food Systems.** Crop yields for major staples (wheat, rice, maize) are negatively affected by heat and drought stress. IPCC synthesis suggests global crop yield declines of roughly 2-6% per decade of warming. This is manageable — agriculture adapts — but it occurs alongside population growth and represents a persistent downward pressure on food security, with effects concentrated in tropical and subtropical regions that are already food-insecure. **Ecosystems.** Coral reef ecosystems are expected to decline by 70-90% under 1.5°C of warming and virtually disappear at 2°C. Tropical species are shifting poleward faster than most ecosystems can adjust. Permafrost thaw will restructure boreal forest and tundra ecosystems significantly. What I think is important to convey: the difference between the "business as usual" and "aggressive mitigation" scenarios isn't the difference between uncomfortable and fine. It's the difference between seriously disruptive and significantly disruptive. The honest case for aggressive mitigation isn't "it prevents climate change" — it doesn't. It's "it keeps the disruption in a range that human systems can plausibly adapt to rather than a range that overwhelms adaptation capacity." Whether we get to a 1.5°C or a 3°C world is an emissions decision we're largely making right now, in the 2020s and 2030s. That window is genuinely closing.
Geoengineering — The Options, the Risks, and the Governance Problem
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