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In 2014 a marine heatwave wiped out more than ninety percent of the bull kelp canopy along more than 350 kilometres of northern California's coast. The water started to recover, and a model built on ocean data expected the kelp to come partway back. It didn't. We start with why we blame the last push: a basketball bet, the loss of the shuttle Columbia, and a fish kill on Australia's Darling River. Then we look past the push, at what keeps a system broken. Ecologists treat a reef as a complex adaptive system, and systems like that can show hysteresis: the way back isn't the way in. Across thirteen reef systems worldwide, kelp forests collapse at about 700 grams of urchin per square metre and return only below about 70, ten times lower. We follow the loops that keep a bare reef bare, what it takes to bring one back, and the two numbers that would show whether this coast is stuck or just missing its predators. Then the counterexample, the ozone hole, which is recovering down the same path it came, because nothing holds it open. Last, where else to look: shallow lakes, the ice sheets, jobs after a recession, a cow-sized poverty line, antibiotic resistance and insomnia, each tested against three questions. Are there two states? Is the way back further than the way in? Can you name what keeps the bad state going? Where all three hold, prevention is far less work than repair.

Chapters

00:00 Cold open: bare rock and a big question

04:03 Welcome, and the map of the episode

05:31 Part one: why the last push gets the blame

09:49 Part one: three losses, and the only one that left

11:48 Part two: what hysteresis is

13:35 Part two: the gap, in numbers

15:40 Part two: why a reef does it

17:59 Part three: what it takes to come back

20:40 What would settle it

24:26 The counterexample: a hole in the sky

28:18 Where else to look: lakes and ice

32:24 Where else to look: work and money

35:34 Where else to look: health, and you

38:53 Close

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