Thursday, 28 August 2025
A kind of tenderness
Thursday, 21 August 2025
This year's sum up motos
I am strong, I am steady, I am free. I carry my joy, my art and my peace with me. I notice without drowning. I honor my growth and I allow happiness to find me.
Wednesday, 20 August 2025
Monday, 18 August 2025
Europe's burning, understanding why
But the problem is that the melting is happening faster than expected. As ice melts, there’s less reflective surface, more dark water or land is exposed, and that absorbs heat instead of reflecting it. It’s like removing a blanket that was keeping the heat out—and then the heat just pours in.
On top of that, greenhouse gases trap heat in the atmosphere, which adds to the problem. So even if the ice hasn’t fully melted, the combination of faster melting, reduced reflection, and greenhouse gases makes the heat spikes worse.
It’s not that the “shield” failed entirely—it’s that the system is overwhelmed and accelerating faster than the natural checks and balances can keep up with.
Some areas feel much hotter than others even though we still have ice in the Arctic and Antarctic. That part can be really surprising.
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Polar amplification – The Arctic warms faster than the rest of the planet. As ice melts, the dark ocean absorbs more heat, which accelerates local warming. That might seem contradictory, because you’d think melting ice cools things, but it actually speeds up warming in that region.
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Jet stream changes – The jet stream, which is a fast-flowing river of air that circles the Northern Hemisphere, is influenced by the temperature difference between the poles and the tropics. As the Arctic warms, this difference shrinks, and the jet stream slows down or becomes wavy. That means hot air can stay stuck over certain regions longer, causing heat waves.
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Ocean currents and heat distribution – Oceans store and move heat around the planet. When currents are disrupted by melting ice or temperature changes, some regions get extra heat while others may be cooler.
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Feedback loops – Things like melting permafrost release methane, a potent greenhouse gas, which makes warming even faster. Plus, as land dries out, it heats up more quickly because dry soil holds less moisture to cool the air.
So basically, the ice isn’t gone yet, but the system that spreads and regulates heat is out of balance. That’s why some places are blazing hot, while others still have ice—but even that ice is melting faster than before.