Abstract

Near-term, ecological forecasting with iterative model refitting and uncertainty partitioning has great promise for improving our understanding of ecological processes and the predictive skill of ecological models, but to date has been infrequently applied to predict biogeochemical fluxes. Bubble fluxes of methane (CH4) from aquatic sediments to the atmosphere (ebullition) dominate freshwater greenhouse gas emissions, but it remains unknown how best to make robust near-term CH4 ebullition predictions using models. Near-term forecasting workflows have the potential to address several current challenges in predicting CH4 ebullition rates, including: development of models that can be applied across time horizons and ecosystems, identification of the timescales for which predictions can provide useful information, and quantification of uncertainty in predictions. To assess the capacity of near-term, iterative forecasting workflows to improve ebullition rate predictions, we developed and tested a near-term, iterative forecasting workflow of CH4 ebullition rates in a small eutrophic reservoir throughout one open-water period. The workflow included the repeated updating of a CH4 ebullition forecast model over time with newly-collected data via iterative model refitting. We compared the CH4 forecasts from our workflow to both alternative forecasts generated without iterative model refitting and a persistence null model. Our forecasts with iterative model refitting estimated CH4 ebullition rates up to 2 weeks into the future [RMSE at 1-week ahead = 0.53 and 0.48 loge(mg CH4 m−2 d−1) at 2-week ahead horizons]. Forecasts with iterative model refitting outperformed forecasts without refitting and the persistence null model at both 1- and 2-week forecast horizons. Driver uncertainty and model process uncertainty contributed the most to total forecast uncertainty, suggesting that future workflow improvements should focus on improved mechanistic understanding of CH4 models and drivers. Altogether, our study suggests that iterative forecasting improves week-to-week CH4 ebullition predictions, provides insight into predictability of ebullition rates into the future, and identifies which sources of uncertainty are the most important contributors to the total uncertainty in CH4 ebullition predictions.

Highlights

  • Near-term ecological forecasting can improve our understanding and quantification of ecosystem processes (Dietze et al, 2018)

  • After 16 October, CH4 ebullition rates dropped to ≤1.32 loge for the remainder of the forecasting period, which ended on 7 November

  • To understand why the forecast workflow with iterative model refitting consistently performed better than the workflow without refitting and the persistence null model, we explored the sources of forecast uncertainty in the workflow with iterative model refitting

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Summary

Introduction

Near-term (day to year) ecological forecasting can improve our understanding and quantification of ecosystem processes (Dietze et al, 2018). Near-term, iterative forecasting creates a model-data feedback loop that evaluates how effectively a model predicts future ecosystem states, with the forecasts evolving as the ecosystem experiences different environmental conditions. One biogeochemical process that near-term, iterative forecasts may improve predictions for is methane (CH4) ebullition, or bubble fluxes of CH4 from organic-rich sediments to the waterbody surface. Among the different types of freshwater CH4 emissions, ebullition can make up anywhere from 0 to 99.6% of total emissions to the atmosphere (Deemer and Holgerson, 2021) and it is considered one of the most uncertain fluxes in both inland water and global CH4 budgets (Wik et al, 2016; Saunois et al, 2020)

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