Why the Climate Is Like a House of Cards ✎

Original: "Basin stability and limit cycles in a conceptual model for climate tipping cascades"
arXiv:2009.09902 · 2020-09-14 · arXiv non-exclusive · independent analysis · 1 min
Scientists built a model of five climate systems and found that with more than 4°C of warming, nearly all of them topple, with ice sheets mattering most.

A house of cards stands as long as every card is in place. Remove one, and the neighbors start to fall. Earth's climate works the same way: ice sheets, ocean currents, and forests are interconnected. If one part breaks, it can drag others down with it.

Scientists in Potsdam built a computer model of five major climate systems: the Greenland and Antarctic ice sheets, the great Atlantic ocean current, temperature fluctuations in the Pacific Ocean, and the Amazon rainforest.

Each system in the model can be in one of two states: normal or broken. For example, an ice sheet either exists or has melted. The scientists ran more than 3.5 billion computer simulations, varying conditions to see what would happen under different levels of warming.

They found that if Earth warms by more than 4 degrees, nearly all systems collapse. And under modest warming, it is usually the ice sheets that break first. That makes them the most important cards in the house: if they fall, the whole climate becomes highly unstable. That is why it is so crucial not to let the planet overheat.

The model ran over 3.5 billion simulations: if one simulation were executed per second, it would take more than 110 years.

The idea of cascading climate transitions echoes Kim Stanley Robinson's novel 'The Ministry for the Future,' which describes chain reactions in the climate system.

\tau_i \dot{x}_i = -a_i x_i^3 + b_i x_i + c_i + \sum_j A_{ij} x_j
The rate of change of an element's state is determined by its internal nonlinear dynamics and the linear influence of other elements.
Concepts
climate ENSO Atlantic multidecadal oscillation El Niño tropospheric biennial oscillation Jin-Timmermann model spring predictability barrier ecosystem tipping point Warm water volume climate network seasonal cycle Niño 4 metastable state Earth's energy imbalance ecological resilience non equilibrium state GPCP intertropical convergence zone ERSST