Abstract

Regional climate change impact assessments are becoming increasingly important for developing adaptation strategies in an uncertain future with respect to hydro-climatic extremes. There are a number of Global Climate Models (GCMs) and emission scenarios providing predictions of future changes in climate. As a result, there is a level of uncertainty associated with the decision of which climate models to use for the assessment of climate change impacts. The IPCC has recommended using as many global climate model scenarios as possible; however, this approach may be impractical for regional assessments that are computationally demanding. Methods have been developed to select climate model scenarios, generally consisting of selecting a model with the highest skill (validation), creating an ensemble, or selecting one or more extremes. Validation methods limit analyses to models with higher skill in simulating historical climate, ensemble methods typically take multi model means, median, or percentiles, and extremes methods tend to use scenarios which bound the projected changes in precipitation and temperature. In this paper a quantile regression based validation method is developed and applied to generate a reduced set of GCM-scenarios to analyze daily maximum streamflow uncertainty in the Upper Thames River Basin, Canada, while extremes and percentile ensemble approaches are also used for comparison. Results indicate that the validation method was able to effectively rank and reduce the set of scenarios, while the extremes and percentile ensemble methods were found not to necessarily correlate well with the range of extreme flows for all calendar months and return periods.

Highlights

  • The process of regional climate change impact assessment with respect to water resources management typically involves the use of Global Climate Model (GCM) output to assess to the impact of a changing climate on river flow regimes

  • Significant trends across the distribution ranging from 0.07 to 0.36 ̊C/decade were found, with the largest changes concentrated at the lower quantiles (τ < 0.4 ). This is indicative of warmer winter temperatures, and accurately capturing this change could be crucial in assessing hydrologic extremes in the Upper Thames River Basin (UTRB) as this will likely change the timing of snowmelt and frozen ground in late winter to early spring

  • Incorporating climate change in regional vulnerability and impact assessments can be challenging given the presence of alternate climate models, model realizations, and future emission scenarios, especially if the impact assessment is computationally demanding

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Summary

Introduction

The process of regional climate change impact assessment with respect to water resources management typically involves the use of Global Climate Model (GCM) output to assess to the impact of a changing climate on river flow regimes. In this process, various bias correction and statistical or dynamic downscaling methods can be used to translate coarse scale GCM data to scales appropriate for regional impact analyses (e.g. hydrologic modeling). The process of climate model and scenario selection should be considered as an integral step in any regional analysis of vulnerability and adaptation to climate change

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