Abstract

To analyse the potential future ecological state of estuaries located in the temperate climate (here exemplified with the Odense Fjord estuary, Denmark), we combined end-of-the-century climate change projections from four different climate models, four contrasting land use scenarios (“Agriculture for nature”, “Extensive agriculture”, “High-tech agriculture” and “Market driven agriculture”) and two different eco-hydrological models. By decomposing the variance of the model-simulated output from all scenario and model combinations, we identified the key sources of uncertainties of these future projections. There was generally a decline in the ecological state of the estuary in scenarios with a warmer climate. Strikingly, even the most nature-friendly land use scenario, where a proportion of the intensive agricultural area was converted to forest, may not be enough to counteract the negative effects of a future warmer climate on the ecological state of the estuary. The different land use scenarios were the most significant sources of uncertainty in the projections of future ecological state, followed, in order, by eco-hydrological models and climate models, albeit all three sources caused high variability in the simulated outputs. Therefore, when projecting the future state of aquatic ecosystems in a global warming context, one should at the very least consider to evaluate an ensemble of land use scenarios (nutrient loads) but ideally also include multiple eco-hydrological models and climate change projections. Our study may set precedence for future attempts to predict and quantify uncertainties of model and model input ensembles, as this will likely be key elements in future tools for decision-making processes.

Highlights

  • IntroductionFreshwater and marine ecosystems have been under pressure from a growing and increasingly prosperous human population

  • During the past century, freshwater and marine ecosystems have been under pressure from a growing and increasingly prosperous human population

  • The level of change when evaluating the effects of future climate scenarios (Fig. 2, right panel) was generally greater than the variations created by the two eco-hydrological model complexes

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Summary

Introduction

Freshwater and marine ecosystems have been under pressure from a growing and increasingly prosperous human population. This has caused increased abstraction of freshwater and increased nutrient export from land to the aquatic environment through intensive agricultural land use and discharges of urban sewage (EEA, 2012). Numerous studies suggest that long-term future climate change (e.g., end-of-the-century) will have detrimental effects on both freshwater (e.g., Jeppesen et al, 2010; Trolle et al, 2011; Moss et al, 2011) and marine ecosystems (Bendtsen and Hansen, 2013; Skogen et al, 2014) by further enhancing eutrophication processes. The ability to project the combined effects of climate and land use change is critically important in the decision-making processes for environmental managers as is the understanding of key uncertainties associated with such projections

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