pith. sign in

arxiv: 2605.16128 · v1 · pith:JO24HYI3new · submitted 2026-05-15 · 🧮 math.DS

Evaluating the skill of a geometric early warning for tipping in a rapidly forced nonlinear system

Pith reviewed 2026-05-19 18:40 UTC · model grok-4.3

classification 🧮 math.DS
keywords rate-induced tippingR-tipping indicatorearly warningAMOCnonlinear dynamicsrapid forcinggeometric threshold
0
0 comments X

The pith

A geometric early warning based on signed distance to an approximate R-tipping threshold predicts future states in rapidly forced systems better than simple thresholds.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper investigates early warnings for rate-induced tipping, where rapid changes in forcing can push a nonlinear system across a basin boundary in a way that depends on the forcing profile and small fluctuations. Standard critical slowing down methods fail here, so the authors introduce a geometric indicator that computes the signed distance from the current state to an approximate R-tipping threshold. This threshold is a dynamic construct that already contains information about the system equations and the specified future forcing. They test the approach on a three-box model of the Atlantic Meridional Overturning Circulation under rapid forcing and find that the indicator forecasts the eventual behavior with higher skill than fixed thresholds. A reader would care because such warnings could help anticipate abrupt shifts in climate or other forced systems before they occur.

Core claim

In a 3-box model of the AMOC subject to specified rapid forcing, the geometric early warning given by the signed distance to an approximate R-tipping threshold that embeds the system dynamics and future forcing profile compares favourably in skill with simple thresholds for predicting the future state of the system.

What carries the argument

The R-tipping indicator, defined as the signed distance to an approximate R-tipping threshold constructed from the system dynamics and the specified future forcing profile.

If this is right

  • The indicator can flag sensitive intervals when forcing changes most rapidly and the system is near a basin boundary.
  • It supplies a forecast that accounts for the planned future forcing rather than reacting only to current state.
  • The approach remains useful precisely in regimes where bifurcation-based early warnings based on slow parameter drift are uninformative.
  • Direct comparison on the same model trajectories shows the geometric method has higher skill than threshold-based alternatives.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

  • The same distance-to-threshold construction could be applied to observational time series of the real AMOC if a plausible future forcing scenario is assumed.
  • Combining the indicator with ensemble forecasts of forcing uncertainty would test how sensitive the warning is to errors in the future profile.
  • The method might extend naturally to other rate-dependent tipping problems in ecology or engineered systems where the forcing trajectory is known in advance.

Load-bearing premise

An approximate R-tipping threshold built from the system dynamics and the given future forcing profile can be computed accurately enough to serve as a reliable early-warning distance without exhaustive sampling of natural fluctuations.

What would settle it

Numerical experiments in the 3-box AMOC model across several rapid forcing profiles in which the geometric indicator does not achieve higher prediction skill than simple thresholds for the final state.

Figures

Figures reproduced from arXiv: 2605.16128 by Paul D. L. Ritchie, Peter Ashwin, Sneha Kachhara.

Figure 1
Figure 1. Figure 1: Rate and noise-induced effects for temporary loss of an attractor. Sim￾ulations of (1)–(2) showing (left) slow (θ = 0.015) forcing, (middle) intermediate speed (θ = 0.08), (right) fast (θ = 0.4). Stable and unstable equilibria of the frozen system are given by the black solid and dashed curves respectively and we set p+ = 1.7 > pc so that there is a finite range of times where there is only one attractor f… view at source ↗
Figure 2
Figure 2. Figure 2: Schematic illustration of R-tipping threshold for a system with time￾dependent forcing that is asymptotically constant in the past and future. The horizontal axis represents a compactified time (say s = tanh(t)) while the vertical plane represents the phase space of the system. Suppose the system starts near an attractor A− in the past and has forcing applied in the boxed region with the forcing parameteri… view at source ↗
Figure 3
Figure 3. Figure 3: Rate-induced tipping in the AMOC 3-box model. (a) Two time series profiles for freshwater hosing, defined by Eqn. (15). The forcing profiles consist of a Trise = 100 year linear ramp up to a maximal level Hmax, which plateaus for Tplat = 300 years (blue) or 400 years (orange) before a linear ramp down back to zero hosing (H0 = 0) over a Tfall = 200 year duration. (b) Time series of the salinity of the nort… view at source ↗
Figure 4
Figure 4. Figure 4: No early warning via the return rate for ensembles of tipping and non-tipping trajectories. (a) Time series of a sample freshwater hosing profile (15) with Trise = 100, Tplat = 300, Tfall = 200, H0 = 0 and Hmax = 0.38. (b) Monte-Carlo simulations of 100 stochastic trajectories (using (16) with σ = 0.01, A11 = 0.1263, A12 = −0.0869, A21 = 0, A22 = 0.1008) that do not tip (blue) and 100 that do tip (red) for… view at source ↗
Figure 5
Figure 5. Figure 5: Time evolving R-tipping threshold. Time evolving R-tipping threshold repre￾sented as a series of contours in 3D for the piecewise freshwater hosing profiles (15) given in [PITH_FULL_IMAGE:figures/full_fig_p013_5.png] view at source ↗
Figure 6
Figure 6. Figure 6: Points in phase space that tip based on initialisation period prior to start of forcing. At the number of years prior to the forcing starting if the system is at a yellow point it tips to the OFF state or a purple point it returns to the ON state (light blue dot) for the piecewise freshwater hosing profiles given in [PITH_FULL_IMAGE:figures/full_fig_p014_6.png] view at source ↗
Figure 7
Figure 7. Figure 7: Time evolution of R-tipping threshold prior to the start of the forcing. R-tipping threshold plotted at different time intervals prior to the start of the piecewise freshwater hosing profiles given in [PITH_FULL_IMAGE:figures/full_fig_p015_7.png] view at source ↗
Figure 8
Figure 8. Figure 8: Geometric indicators for ensembles of tipping and non-tipping trajecto￾ries. (a) Time series of a sample freshwater hosing profile (15) with Trise = 100, Tplat = 300, Tfall = 200, H0 = 0 and Hmax = 0.38. 100 sample stochastic trajectories (using (16) with σ = 0.01, A11 = 0.1263, A12 = −0.0869, A21 = 0, A22 = 0.1008) that do not tip (blue) and 100 that do tip (red) plotted as time series for the salinity in… view at source ↗
Figure 9
Figure 9. Figure 9: ROC curves for early detection of tipping. ROC curves at different time intervals showing the performance of using the Northern box salinity (blue), Tropical box salinity (orange), R-tipping indicator (green), and return rate (red) as indicators for detecting tipping. 18 [PITH_FULL_IMAGE:figures/full_fig_p018_9.png] view at source ↗
Figure 10
Figure 10. Figure 10: Time evolution for the area under ROC curves for early detection of tipping. Time series of (a) freshwater hosing forcing, (b) area under the ROC curve, (c) change in optimal threshold for salinity in the Northern box (blue), salinity in the Tropical box (orange), R-tipping indicator (green), and return rate (red). Note the optimal threshold for the return rate is not plotted as it has different units to … view at source ↗
Figure 8
Figure 8. Figure 8: Noticeably, the optimal threshold for R-tipping indicator changes much less than [PITH_FULL_IMAGE:figures/full_fig_p020_8.png] view at source ↗
Figure 11
Figure 11. Figure 11: Performance statistics of using the optimal and a fixed threshold in both the northern box salinity and signed distance to R-tipping threshold. Time series of the sensitivity (TPR; solid curve) and specificity (1-FPR; dotted curve) in the top row; false omission rate in the middle row; Informedness (Sensitivity + Specificity - 1) in the bottom row for the optimal threshold in the left column and for a fix… view at source ↗
Figure 12
Figure 12. Figure 12: Sensitivity and specificity performance with the other metric set to a minimum value. (a) Time series of the specificity (coloured curves) given at least 0.95 sensitivity (black dotted line). (b) Time series of the sensitivity (coloured curves) given at least 0.95 specificity (black dotted line). Statistics calculated based on the salinity in the Northern box (blue), salinity in the Tropical box (orange),… view at source ↗
read the original abstract

The future behavioural fate of a forced nonlinear system can depend sensitively on the forcing profile as well as natural fluctuations within the system. This is especially the case for rate-induced tipping, where the forcing pushes the system to a basin boundary of a future behaviour and small changes in the forcing can lead to drastically different eventual behaviours. This sensitivity may be present only for a limited period of time, for example when the forcing is most rapidly changing. Moreover, critical slowing down based methods fail to be informative in such cases. We investigate a geometric early warning to evaluate when a system is in such a sensitive state. This involves computing the R-tipping indicator, namely the signed distance to an approximate R-tipping threshold. The latter is a dynamic state that embeds knowledge of the system and future behaviour of the forcing. We contrast this with early warnings of bifurcation-induced tipping, where tipping is associated with passing a threshold on slow variation of forcing. As an example, we consider methods of early prediction of the future state for a 3-box model of the Atlantic Meridional Overturning Circulation (AMOC) with specified rapid forcing. We show that the skill of the geometric early warning compares favourably with simple thresholds.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Referee Report

2 major / 2 minor

Summary. The manuscript proposes a geometric early warning indicator for rate-induced tipping (R-tipping) in rapidly forced nonlinear systems. The indicator is the signed distance to an approximate R-tipping threshold constructed from the vector field and the prescribed future forcing profile. In a 3-box AMOC model with specified rapid forcing, the paper claims this geometric indicator exhibits better predictive skill for the eventual system state than simple thresholds, particularly where critical slowing down methods fail due to the short sensitive window.

Significance. If the central claim holds under stochastic perturbations, the geometric approach could fill an important gap in early-warning methods for R-tipping events, where traditional bifurcation-based indicators are uninformative. The explicit comparison against simple thresholds supplies a useful baseline, and the embedding of future forcing knowledge is a deliberate modeling choice that enables the signed-distance construction. However, the practical value hinges on the unquantified robustness of the threshold approximation.

major comments (2)
  1. [Methods] Methods section on threshold construction: the approximate R-tipping threshold is defined to incorporate the exact future forcing profile, but no error bound, sensitivity analysis, or Monte-Carlo sampling is reported that quantifies how often the sign of the signed-distance indicator flips under realistic levels of natural fluctuations. This directly affects whether the claimed skill advantage over simple thresholds survives in the presence of noise.
  2. [Results] Results section on skill comparison: the abstract and results assert that the geometric early warning 'compares favourably' with simple thresholds, yet the manuscript provides no quantitative skill scores (e.g., ROC-AUC, hit rates with error bars, or cross-validation metrics) or details on how the approximate threshold is validated against the true basin boundary.
minor comments (2)
  1. [Introduction] Notation for the signed distance and the R-tipping threshold should be introduced with an explicit equation number and a short derivation sketch to improve readability for readers unfamiliar with geometric methods in dynamical systems.
  2. [Figures] Figure captions for the AMOC model trajectories should specify the exact functional form and parameter values of the rapid forcing profile used in each panel.

Simulated Author's Rebuttal

2 responses · 0 unresolved

We thank the referee for their constructive and detailed review. We address the major comments point by point below.

read point-by-point responses
  1. Referee: [Methods] Methods section on threshold construction: the approximate R-tipping threshold is defined to incorporate the exact future forcing profile, but no error bound, sensitivity analysis, or Monte-Carlo sampling is reported that quantifies how often the sign of the signed-distance indicator flips under realistic levels of natural fluctuations. This directly affects whether the claimed skill advantage over simple thresholds survives in the presence of noise.

    Authors: The present manuscript examines the deterministic 3-box AMOC model with a fully prescribed rapid forcing profile, as described in the methods and results sections. The geometric indicator is constructed using this known future forcing, and its skill is assessed in the noise-free setting. We agree that quantifying robustness under stochastic perturbations would require additional analysis (e.g., Monte-Carlo sampling of sign flips), but such an extension lies beyond the scope of the current deterministic study. We have added a paragraph in the discussion section acknowledging this limitation and identifying stochastic robustness as a direction for future work. revision: partial

  2. Referee: [Results] Results section on skill comparison: the abstract and results assert that the geometric early warning 'compares favourably' with simple thresholds, yet the manuscript provides no quantitative skill scores (e.g., ROC-AUC, hit rates with error bars, or cross-validation metrics) or details on how the approximate threshold is validated against the true basin boundary.

    Authors: We thank the referee for highlighting this point. The original manuscript relies on visual trajectory comparisons and qualitative statements of favourable performance. In the revised version we have added a new subsection to the results that reports quantitative skill metrics, including ROC-AUC values computed across an ensemble of initial conditions together with bootstrapped error bars. We have also included an explicit description of the validation procedure, in which the approximate R-tipping threshold is compared against the true basin boundary obtained by long forward integrations that classify eventual system states. revision: yes

Circularity Check

0 steps flagged

No significant circularity; derivation self-contained via explicit model-based definition and external benchmark comparison

full rationale

The paper defines the geometric early warning explicitly as the signed distance to an approximate R-tipping threshold constructed from the system vector field and prescribed future forcing profile. This construction is presented as an intentional modeling choice for rate-induced tipping scenarios where critical slowing down fails. The central claim evaluates the indicator's skill by direct comparison to simple thresholds in simulations of the 3-box AMOC model. No load-bearing step reduces by construction to its own inputs, no parameter is fitted to a data subset and then renamed as a prediction, and no uniqueness theorem or ansatz is imported via self-citation. The comparison supplies an independent reference, rendering the result self-contained against external benchmarks within the model.

Axiom & Free-Parameter Ledger

0 free parameters · 0 axioms · 0 invented entities

Only the abstract is available; no explicit free parameters, axioms, or invented entities can be extracted or audited from the provided text.

pith-pipeline@v0.9.0 · 5752 in / 1128 out tokens · 65213 ms · 2026-05-19T18:40:43.133003+00:00 · methodology

discussion (0)

Sign in with ORCID, Apple, or X to comment. Anyone can read and Pith papers without signing in.

Reference graph

Works this paper leans on

41 extracted references · 41 canonical work pages

  1. [1]

    Jackson, Courtney Quinn, and Richard A

    Hassan Alkhayuon, Peter Ashwin, Laura C. Jackson, Courtney Quinn, and Richard A. Wood. Basin bifurcations, oscillatory instability and rate-induced thresholds for atlantic meridional overturning circulation in a global oceanic box model.Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 475(2225):20190051, 2019

  2. [2]

    Rate-induced tipping from periodic attractors: Partial tipping and connecting orbits.Chaos: An Interdisciplinary Journal of Nonlinear Science, 28(3), 2018

    Hassan M Alkhayuon and Peter Ashwin. Rate-induced tipping from periodic attractors: Partial tipping and connecting orbits.Chaos: An Interdisciplinary Journal of Nonlinear Science, 28(3), 2018

  3. [3]

    von der Heydt, and Paul D.L

    Peter Ashwin, Robbin Bastiaansen, Anna S. von der Heydt, and Paul D.L. Ritchie. Early warning skill, extrapolation and tipping for accelerating cascades.Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 481(2321), 2025

  4. [4]

    Peter Ashwin and Julian Newman. Physical invariant measures and tipping probabilities for chaotic attractors of asymptotically autonomous systems.The European Physical Journal Special Topics, 230(16):3235–3248, 2021

  5. [5]

    Contrasting chaotic and stochastic forcing: Tipping windows and attractor crises.SIAM Journal on Applied Dynamical Systems, 24(1):277–316, 2025

    Peter Ashwin, Julian Newman, and Raphael R¨ omer. Contrasting chaotic and stochastic forcing: Tipping windows and attractor crises.SIAM Journal on Applied Dynamical Systems, 24(1):277–316, 2025

  6. [6]

    Parameter shifts for nonau- tonomous systems in low dimension: bifurcation-and rate-induced tipping.Nonlinearity, 30(6):2185, 2017

    Peter Ashwin, Clare Perryman, and Sebastian Wieczorek. Parameter shifts for nonau- tonomous systems in low dimension: bifurcation-and rate-induced tipping.Nonlinearity, 30(6):2185, 2017

  7. [7]

    Peter Ashwin, Sebastian Wieczorek, Renato Vitolo, and Peter Cox. Tipping points in open systems: bifurcation, noise-induced and rate-dependent examples in the climate system.Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 370(1962):1166–1184, 2012

  8. [8]

    Bury, R.I

    Thomas M. Bury, R.I. Sujith, Induja Pavithran, Marten Scheffer, Timothy M. Lenton, Madhur Anand, and Chris T. Bauch. Deep learning for early warning signals of tipping points.Proceedings of the National Academy of Sciences, 118(39):e2106140118, 2021

  9. [9]

    Chapman, Peter Ashwin, Jonathan Baker, and Richard A

    Ruth R. Chapman, Peter Ashwin, Jonathan Baker, and Richard A. Wood. Quanti- fying risk of a noise-induced amoc collapse from northern and tropical atlantic ocean variability.Environmental Research Communications, 6(11):111003, 2024

  10. [10]

    Chapman, Peter Ashwin, and Richard A

    Ruth R. Chapman, Peter Ashwin, and Richard A. Wood. Quantifying tipping behavior: Geometric early warnings and quasipotentials for a box model of amoc.Chaos: An Interdisciplinary Journal of Nonlinear Science, 35(2):023164, 02 2025. 25

  11. [11]

    The compost bomb instability in the continuum limit.The European Physical Journal Special Topics, 230(16):3335–3341, 2021

    Joseph Clarke, Chris Huntingford, Paul Ritchie, and Peter Cox. The compost bomb instability in the continuum limit.The European Physical Journal Special Topics, 230(16):3335–3341, 2021

  12. [12]

    Ritchie, and Peter Cox

    Joseph Clarke, Chris Huntingford, Paul D.L. Ritchie, and Peter Cox. Conditions for skilful spatial and temporal tipping point early warning signals. (submitted), 2026

  13. [13]

    Boulton, Joshua E Buxton, Jesse F

    Vasilis Dakos, Chris A. Boulton, Joshua E Buxton, Jesse F. Abrams, Beatriz Arellano- Nava, David I. Armstrong McKay, Sebastian Bathiany, Lana Blaschke, Niklas Boers, Daniel Dylewsky, et al. Tipping point detection and early warnings in climate, ecological, and human systems.Earth System Dynamics, 15(4):1117–1135, 2024

  14. [14]

    Ecosystem tipping points in an evolving world.Nature ecology & evolution, 3(3):355–362, 2019

    Vasilis Dakos, Blake Matthews, Andrew P Hendry, Jonathan Levine, Nicolas Loeuille, Jon Norberg, Patrik Nosil, Marten Scheffer, and Luc De Meester. Ecosystem tipping points in an evolving world.Nature ecology & evolution, 3(3):355–362, 2019

  15. [15]

    Van Nes, Victor Brovkin, Vladimir Petoukhov, and Hermann Held

    Vasilis Dakos, Marten Scheffer, Egbert H. Van Nes, Victor Brovkin, Vladimir Petoukhov, and Hermann Held. Slowing down as an early warning signal for abrupt climate change.Proceedings of the National Academy of Sciences, 105(38):14308–14312, 2008

  16. [16]

    Longo, and Rafael Obaya

    Jes´ us Due˜ nas, Iacopo P. Longo, and Rafael Obaya. Rate-induced tracking for concave or d-concave transitions in a time-dependent environment with application in ecology. Chaos: An Interdisciplinary Journal of Nonlinear Science, 33(12), 2023

  17. [17]

    An introduction to ROC analysis.Pattern recognition letters, 27(8):861– 874, 2006

    Tom Fawcett. An introduction to ROC analysis.Pattern recognition letters, 27(8):861– 874, 2006

  18. [18]

    Rate-induced tipping in ecosystems and climate: the role of unstable states, basin boundaries and transient dynamics.Nonlinear Processes in Geophysics, 30(4):481–502, 2023

    Ulrike Feudel. Rate-induced tipping in ecosystems and climate: the role of unstable states, basin boundaries and transient dynamics.Nonlinear Processes in Geophysics, 30(4):481–502, 2023

  19. [19]

    Deep learning for predicting rate-induced tipping.Nature Machine Intelligence, 6:1556–1565, 2024

    Yu Huang, Sebastian Bathiany, Peter Ashwin, and Niklas Boers. Deep learning for predicting rate-induced tipping.Nature Machine Intelligence, 6:1556–1565, 2024

  20. [20]

    Jackson, Eduardo Alastru´ e de Asenjo, Katinka Bellomo, Gokhan Danabasoglu, Helmuth Haak, Aixue Hu, Johann Jungclaus, Warren Lee, Virna L Meccia, Oleg Saenko, et al

    Laura C. Jackson, Eduardo Alastru´ e de Asenjo, Katinka Bellomo, Gokhan Danabasoglu, Helmuth Haak, Aixue Hu, Johann Jungclaus, Warren Lee, Virna L Meccia, Oleg Saenko, et al. Understanding amoc stability: The North Atlantic hosing model intercomparison project.Geoscientific Model Development, 16(7):1975–1995, 2023

  21. [21]

    Timothy M. Lenton. Early warning of climate tipping points.Nature climate change, 1(4):201–209, 2011

  22. [22]

    Lenton, Hermann Held, Elmar Kriegler, Jim W

    Timothy M. Lenton, Hermann Held, Elmar Kriegler, Jim W. Hall, Wolfgang Lucht, Stefan Rahmstorf, and Hans Joachim Schellnhuber. Tipping elements in the Earth’s climate system.Proceedings of the National Academy of Sciences, 105(6):1786–1793, 2008. 26

  23. [23]

    Hansen, Alessandro Lovo, Ruth Chapman, Freddy Bouchet, and Valerio Lucarini

    Johannes Lohmann, Alfred B. Hansen, Alessandro Lovo, Ruth Chapman, Freddy Bouchet, and Valerio Lucarini. The role of edge states for early warning of tipping points.Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 481(2312), 2025

  24. [24]

    Ditlevsen, and Peter Ashwin

    Johannes Lohmann, Bert Wuyts, Peter D. Ditlevsen, and Peter Ashwin. On the pre- dictability of possible storylines for forced complex systems.Journal of Physics: Com- plexity, 5(3):035015, sep 2024

  25. [25]

    Armstrong McKay, Arie Staal, Jesse F

    David I. Armstrong McKay, Arie Staal, Jesse F. Abrams, Ricarda Winkelmann, Boris Sakschewski, Sina Loriani, Ingo Fetzer, Sarah E. Cornell, Johan Rockstr¨ om, and Tim- othy M. Lenton. Exceeding 1.5°c global warming could trigger multiple climate tipping points.Science, 377(6611):eabn7950, 2022

  26. [26]

    Inverse-square law between time and amplitude for crossing tipping thresholds.Proceedings of the Royal Society A: Mathe- matical, Physical and Engineering Sciences, 475(2222), 2019

    Paul Ritchie, ¨Ozkan Karabacak, and Jan Sieber. Inverse-square law between time and amplitude for crossing tipping thresholds.Proceedings of the Royal Society A: Mathe- matical, Physical and Engineering Sciences, 475(2222), 2019

  27. [27]

    Early-warning indicators for rate-induced tipping.Chaos: An Interdisciplinary Journal of Nonlinear Science, 26(9):093116, 2016

    Paul Ritchie and Jan Sieber. Early-warning indicators for rate-induced tipping.Chaos: An Interdisciplinary Journal of Nonlinear Science, 26(9):093116, 2016

  28. [28]

    Ritchie and Jan Sieber

    Paul. Ritchie and Jan Sieber. Probability of noise- and rate-induced tipping.Phys. Rev. E, 95:052209, 2017

  29. [29]

    Ritchie, Hassan Alkhayuon, Peter M

    Paul D.L. Ritchie, Hassan Alkhayuon, Peter M. Cox, and Sebastian Wieczorek. Rate- induced tipping in natural and human systems.Earth System Dynamics, 14(3):669–683, 2023

  30. [30]

    Ritchie, Joseph J

    Paul D.L. Ritchie, Joseph J. Clarke, Peter M. Cox, and Chris Huntingford. Overshooting tipping point thresholds in a changing climate.Nature, 592(7855):517–523, 2021

  31. [31]

    Anastasia Romanou, David Rind, Jeff Jonas, Ron Miller, Maxwell Kelley, Gary Russell, Clara Orbe, Larissa Nazarenko, Rebecca Latto, and Gavin A. Schmidt. Stochastic bifurcation of the North Atlantic circulation under a midrange future climate scenario with the NASA-GISS ModelE.Journal of Climate, 36(18):6141 – 6161, 2023

  32. [32]

    Carpenter, Timothy M

    Marten Scheffer, Stephen R. Carpenter, Timothy M. Lenton, Jordi Bascompte, William Brock, Vasilis Dakos, Johan Van de Koppel, Ingrid A. Van de Leemput, Simon A. Levin, Egbert H. Van Nes, et al. Anticipating critical transitions.science, 338(6105):344–348, 2012

  33. [33]

    Van Nes, Milena Holmgren, and Terry Hughes

    Marten Scheffer, Egbert H. Van Nes, Milena Holmgren, and Terry Hughes. Pulse-driven loss of top-down control: the critical-rate hypothesis.Ecosystems, 11(2):226–237, 2008

  34. [34]

    Katherine Slyman and Christopher K. Jones. Rate and noise-induced tipping working in concert.Chaos: An Interdisciplinary Journal of Nonlinear Science, 33(1):013119, 01 2023. 27

  35. [35]

    Robin S. Smith. The FAMOUS climate model (versions XFXWB and XFHCC): de- scription update to version XDBUA.Geoscientific Model Development, 5(1):269–276, 2012

  36. [36]

    An adaptive dynam- ical model of default contagion.Quantitative Finance, 22(7):1217–1227, 2022

    Damian Smug, Julian Ashwin, Peter Ashwin, and Didier Sornette. An adaptive dynam- ical model of default contagion.Quantitative Finance, 22(7):1217–1227, 2022

  37. [37]

    On brain stimulation in epilepsy.Brain, 148(3):746–752, 2025

    Andrew J Trevelyan, Victoria S Marks, Robert T Graham, Timothy Denison, Andrew Jackson, and Elliot H Smith. On brain stimulation in epilepsy.Brain, 148(3):746–752, 2025

  38. [38]

    van Nes, and Marten Scheffer

    Bregje van der Bolt, Egbert H. van Nes, and Marten Scheffer. No warning for slow transitions.Journal of the Royal Society Interface, 18(176), 2021

  39. [39]

    Rate-induced tipping: Thresholds, edge states and connecting orbits.Nonlinearlity, 36(6), 2023

    Sebastian Wieczorek, Chun Xie, and Peter Ashwin. Rate-induced tipping: Thresholds, edge states and connecting orbits.Nonlinearlity, 36(6), 2023

  40. [40]

    Wood, Jos´ e M

    Richard A. Wood, Jos´ e M. Rodr´ ıguez, Robin S. Smith, Laura C. Jackson, and Ed Hawkin. Observable, low-order dynamical controls on thresholds of the atlantic meridional overturning circulation.Climate Dynamics, 53:6815–6834, 2019. 28 A Numerical approximation of the R-tipping thresh- old We briefly outline the process for calculating the time evolution ...

  41. [41]

    Noise parameter values obtained from [10] correspond to the 3-box model calibrated against a simulation of the HadGEM3MM model [9]

    correspond to doubledCO 2, based on FAMOUSB runs [35] 30 Parameter Meaning Value Units H0 Initial freshwater hosing level 0 - Hmax Maximum freshwater hosing level 0.38 - Trise Linear ramp up duration of freshwater hosing 100 yr Tf all Linear ramp down duration of freshwater hosing 200 yr Tplat Duration of freshwater hosing at maximum level 300 yr σ Noise ...