Early Warnings of Regime Shifts
School on biological physics across scales: phase transitions
Outline
Discussion
Early warning signals:
Critical slowing down
Flickering
Critical speeding up
Long term memory & potential analysis
Spatial patterns
Break
Do they work?
Discuss
What are early warning signals?
What is suitable of early warning signals?
What needs to be in place for you to trust them?
Regime shifts and resilience
Magnitude of change that a system can absorb without undergoing a regime shift
Back to theory: Where is the tipping point?
\[\frac{d🐠}{d⏱️}=🐠 \left( 1- \frac{🐠}{🌎} \right) - 🎣 \left( \frac{🐠^2}{🐠^2+1} \right)\]
Different ways of tipping
Slow - fast systems
B-tipping: bifurcations
Saddle, Folk, Hopf, pitchfork…
N-tipping: noise induced (stochasticity)
R-tipping: rate induced
Most early warnings are tailored to B-tipping, limited applications for N- and R- tipping
Resilience indicators
Resilience indicators
\(\Delta\) Variance and autocorrelation
\(\Delta\) skewness and kurtosis
Model-based indicators:
Diffusion jump models
Time varying AR(p) models
Threshold AR(p) models
Potential analysis
Spatial indicators:
Fourier transforms
Power spectrum
Patch-size distributions
Dakos et al. 2012. PLoS ONE Kéfi et al. 2014. PLoS ONE .
Resilience indicators
Critical slowing down
Resilience ~ slowness
\(\uparrow\) Variance and autocorrelation
NDVI: normalized difference vegetation index
VOD: vegetation optical depth
Limited spatial and temporal resolution
Confirm a threshold: 1500mm
Limitations: fail when dynamics are driven by stochastic processes or when signals have too much noise
Hastings & Wysham. 2010. Ecology Letters
Exit time
Mean exit time: average time it takes to leave the basin for first time
The potential derived includes state-dependent stochasticity
You can compute confidence intervals
Applications in lakes (plankton), and climate
Time series with multiple shifts
Useful for fast systems
Arani et al 2021 Science
Potential analysis
How many basins has the potential landscape?
Statistically infer by fitting polynomials at different time windows
Time series with multiple shifts
Useful for fast systems
Levina & Lenton 2010 Clim Past
Model selection
Applications in climate (ice cores 60kyrs)
Red: 1 basin
Green: 2 basins
Cyan: 3
Purple: 4
Flickering
\(\Delta\) Skewness and Kurtosis
System explore alternative states
Biases the distribution towards new attractor
Increase or decrease
Only works on fast systems
Spatial patterns
Spatial patterns
One real pattern, but multiple possible generative models
Bayesian approach to chose generative model
similarity of models on feature space
Back to theoretical model: how close is the instance to tipping?
Approximation in real life setting
Where on Earth are regime shifts likely to occur?
Depends on our ability to observe and measure resilience
VIDEO
Terrestrial: - Gross primary productivity (2001:2018) - Ecosystem respiration (2001:2018) - Leaf area index (1994:2017)
Marine: - Chlorophyll A (1998:2018)
>1M pixels, weekly obs, 0.25 degree grid resolution
Analysis: one pixel
The generic resilience indicators do not necessarily align with critical slowing down or speeding up theories: higher co-dimensions (multiple drivers).
Detection
In the absence of ground truth, if \(\Delta\) is > 95% or < 5% of the distribution is considered a signal of resilience loss
~30% of ecosystem show symptoms of resilience loss, boreal forest and tundra particularly strong signals
~25% of ecosystem show symptoms of resilience loss, Easter Indo-Pacific and Tropical Eastern Pacific Oceans particularly strong signals
Discuss:
Why do you think there is so little agreement?
Can these assessments be trusted? If yes, where?
If not, how would you improve it?
Contradictory signals?
Attempts to validate: triangulation
Permutation test
Attempts to validate: triangulation
Compare with alternative methods
XAI methods to explore detection of EWS:
If CSD was the main route to tipping, only one driver should be of high predicting value and it should be the slope of the linear trend
Multiple factors, and multiple scales of influence are at play
Experiments showed that under higher co-dims, increase/decrease in Var and AC1 can be expected
Machine learning
Trained on synthetic (low dim) models, researchers know when collapse occurred – truncate
Machine learning
Trained on synthetic (low dim) models, researchers know when collapse occurred – truncate
Machine learning: R-tipping
Challenges
Most progress is based on CSD approach (B-tipping)
There is some improvements with ML, but not accuracy assessment against ground truth
Do EWS work?
Early warning signals don’t predict forest die-offs
Early warning signals don’t predict forest die-offs
Resilience of the water cycle: Single metrics are not enough
Lessons
Measuring resilience from data is an open problem [B-tipping, N-tipping, R-tipping]
Benefit from ML and XAI approaches to quantify accuracy and uncertainty
But it needs to be trained on observations, not synthetic models
Open invitation to explore collaborations
Summary
Early warning signals
Evolving field, mainly focused on CSD
B-tipping, N-tipping, R-tipping…
ML hold promises
Better than other statistical approaches (but trained on synthetic models)
Still focused on CSD, with one paper on R-tipping
Open question if they work on real world settings
EWS have low accuracy
Ground truth: forest die-offs
Ground truth: break points in water variables
How to improve them? – open area of research