Abstract

Land‐use and climate change are significantly affecting stream ecosystems, yet understanding of their long‐term impacts is hindered by the few studies that have simultaneously investigated their interaction and high variability among future projections. We modeled possible effects of a suite of 2030, 2060, and 2090 land‐use and climate scenarios on the condition of 70,772 small streams in the Chesapeake Bay watershed, United States. The Chesapeake Basin‐wide Index of Biotic Integrity, a benthic macroinvertebrate multimetric index, was used to represent stream condition. Land‐use scenarios included four Special Report on Emissions Scenarios (A1B, A2, B1, and B2) representing a range of potential landscape futures. Future climate scenarios included quartiles of future climate changes from downscaled Coupled Model Intercomparison Project ‐ Phase 5 (CMIP5) and a watershed‐wide uniform scenario (Lynch2016). We employed random forests analysis to model individual and combined effects of land‐use and climate change on stream conditions. Individual scenarios suggest that by 2090, watershed‐wide conditions may exhibit anywhere from large degradations (e.g., scenarios A1B, A2, and the CMIP5 25th percentile) to small degradations (e.g., scenarios B1, B2, and Lynch2016). Combined land‐use and climate change scenarios highlighted their interaction and predicted, by 2090, watershed‐wide degradation in 16.2% (A2 CMIP5 25th percentile) to 1.0% (B2 Lynch2016) of stream kilometers. A goal for the Chesapeake Bay watershed is to restore 10% of stream kilometers over a 2008 baseline; our results suggest meeting and sustaining this goal until 2090 may require improvement in 11.0%–26.2% of stream kilometers, dependent on land‐use and climate scenario. These results highlight inherent variability among scenarios and the resultant uncertainty of predicted conditions, which reinforces the need to incorporate multiple scenarios of both land‐use (e.g., development, agriculture, etc.) and climate change in future studies to encapsulate the range of potential future conditions.

Highlights

  • Our results suggest a highly variable response of stream conditions in the Chesapeake Bay watershed to future potential land-use and climatic changes

  • We incorporated multiple future land-use and climate scenarios to capture the range of potential future stream conditions as well as highlight projection uncertainties

  • The A2 land-use scenario that projects a global population of 13 billion by 2100 is slightly outdated (Van Vuuren & Carter, 2014), we incorporated it as a worst-case scenario

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Summary

| INTRODUCTION

Land-use and climate change are two factors that have dramatically altered freshwater ecosystems across the globe (Carpenter, Stanley, & Zanden, 2011; Davidson, 2014; Meyer, Sale, Mulholland, & Poff, 1999; Vörösmarty et al, 2010; Woodward, Perkins, & Brown, 2010), resulting in a disproportionately high number of imperiled species occupying these systems (Collen et al, 2014; Strayer & Dudgeon, 2010; Young, McCauley, Galetti, & Dirzo, 2016). The Chesapeake Bay watershed lies in the northeast United States and by some predictions will experience a 2.0°C air temperature increase by 2035, the greatest warming in the contiguous United States and a level that is two decades ahead of global average values (Dupigny-Giroux et al, 2018). Streams in this region may experience the effects of climate change earlier than in other regions. The predicted early onset of climatic and population changes in this region makes it an excellent test case of how land-use and climate change may affect global freshwater biological conditions

| MATERIALS AND METHODS
Environmental sustainability
Findings
| DISCUSSION
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