the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Benchmarking Conditioners in Liang–Kleeman Information Flow: Application to Land–Atmosphere Interactions
Abstract. The Liang–Kleeman Information Flow (LKIF) framework has been increasingly used to identify causality in Earth–system dynamics in recent years. Yet, uncertainties remain regarding how the causal graph changes when mediators and confounders (conditioners) are introduced, i.e., divergence between the bivariate and conditioned forms. A controlled synthetic experiment shows that LKIF preserves correct causal directions under hidden confounding, while differences between bivariate and multivariate estimates still occur. We characterize these differences using time–varying LKIF (ΔIF) and introduce several quantifiers, including Mediator Dominance Index, Moderation Gain, Confounding Pressure, and Convergence Rate, to evaluate the contributions of conditioners. This is illustrated in an application to soil moisture (SM) and vapor pressure deficit (VPD) couplings with vegetation (Leaf Area Index (LAI) and Gross Primary Productivity (GPP)). We find that the influence of SM on LAI remains consistently direct and stable, whereas its influence on GPP and that of VPD on vegetation exhibit substantial divergence between bivariate and multivariate estimates. This divergence peaks under compound dry–hot conditions, with VPD and temperature emerging as dominant mediators. These results demonstrate that bivariate and multivariate LKIF can yield markedly different conclusions across time and space, especially under compound environmental stress. This highlights the need for multivariate conditioning when assessing vegetation responses.
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RC1: 'Comment on egusphere-2026-267', Anonymous Referee #1, 27 Mar 2026
- AC1: 'Reply on RC1', Daniel Hagan, 30 Apr 2026
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RC2: 'Comment on egusphere-2026-267', Anonymous Referee #2, 10 Apr 2026
Please see the attached PDF with the reviewer comments.
- AC2: 'Reply on RC2', Daniel Hagan, 30 Apr 2026
Status: closed
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RC1: 'Comment on egusphere-2026-267', Anonymous Referee #1, 27 Mar 2026
This paper investigates when and why bivariate and multivariate Liang–Kleeman Information Flow (L-K IF) estimates diverge in land–atmosphere applications. The manuscript has clear potential and addresses an interesting methodological problem of practical relevance. However, substantial revisions are required to strengthen the manuscript.
Reviewer's comments:
- The paper defines ΔIF as an absolute difference in Section 2.2, but Appendix A later writes ΔIF expressions without absolute value signs.
- The significance assessment of ΔIF via a paired two-tailed Student’s t-test at each time step is not sufficiently justified. Because the IF estimates are time-varying, serially dependent, and derived from filtered time series, the independence assumptions behind a pointwise t-test may not hold.
- The choice of four quantile-based regimes is reasonable but somewhat arbitrary. The manuscript should explain why quartiles were selected instead of terciles, quintiles, or physically defined thresholds. A short sensitivity test would be helpful.
- According to the authors, the definition of CR depends on a threshold ε_abs chosen as, for example, the 10th percentile of ΔIF across all couplings. This choice strongly affects CR yet is not sufficiently justified or stress-tested. Sensitivity analysis is needed because CR may change substantially under alternative thresholds.
- The paper should report the employed Kalman filter parameter settings.
- ANOVA is interesting, but readers need reassurance that its assumptions are not severely violated under quantile-conditioned, potentially heteroscedastic, non-independent data. A discussion on robustness is required.
- The new indices (MDI, MG, CP, and CR) are interesting, but they currently read more as descriptive summary statistics than as fully validated methodological advances. Their novelty would be stronger if the authors demonstrated formal properties, sensitivity (do results change if noise increases? time series length changes? conditioning set slightly changes?), robustness, and interpretability (What does a high MDI physically mean?) across more than one showcased pathway.
- The decomposition in Eqs. (7)–(9) is order-dependent, since conditioners are added progressively. The manuscript does not discuss whether MDI, MG, and CP change if the order of VPD, T, and SSR is permuted. This is a major issue because the estimated “contribution” of each conditioner may partly reflect the order rather than intrinsic causal relevance. The authors should test all permutations.
- Careful language editing is required throughout the manuscript. Examples include awkward phrasing such as “This begs a spatio–temporal quality…,” “more direct SM→LAI,” “VPD_driver-based,”.
Citation: https://doi.org/10.5194/egusphere-2026-267-RC1 - AC1: 'Reply on RC1', Daniel Hagan, 30 Apr 2026
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RC2: 'Comment on egusphere-2026-267', Anonymous Referee #2, 10 Apr 2026
Please see the attached PDF with the reviewer comments.
- AC2: 'Reply on RC2', Daniel Hagan, 30 Apr 2026
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This paper investigates when and why bivariate and multivariate Liang–Kleeman Information Flow (L-K IF) estimates diverge in land–atmosphere applications. The manuscript has clear potential and addresses an interesting methodological problem of practical relevance. However, substantial revisions are required to strengthen the manuscript.
Reviewer's comments: