Abstract

Glacier retreat poses risks and benefits for species of cultural and economic importance. One example is Pacific salmon (Oncorhynchus spp.), supporting subsistence harvests, and commercial and recreational fisheries worth billions of dollars annually. Although decreases in summer streamflow and warming freshwater is reducing salmon habitat quality in parts of their range, glacier retreat is creating new streams and lakes that salmon can colonize. However, potential gains in future salmon habitat associated with glacier loss have yet to be quantified across the range of Pacific salmon. Here we project future gains in Pacific salmon freshwater habitat by linking a model of glacier mass change for 315 glaciers, forced by five different Global Climate Models, with a simple model of salmon stream habitat potential throughout the Pacific Mountain ranges of western North America. We project that by the year 2100 glacier retreat will create 6,146 (±1,619) km of new streams accessible for colonization by Pacific salmon, of which 1,930 (±569) km have the potential to be used for spawning and juvenile rearing, representing 0 to 27% gains within the 18 sub-regions we studied. These findings can inform proactive management and conservation of Pacific salmon in this era of rapid climate change.

Highlights

  • Glacier retreat poses risks and benefits for species of cultural and economic importance

  • For the accessible glaciers within the 18 sub-regions of our study region, we model the timing of glacier retreat[23] and derive future stream networks based on sub-glacial terrain (Fig. 1b)

  • We show where and when glacier retreat will create thousands of kilometers of new streams accessible for colonization by Pacific salmon, many of which are potentially suitable for spawning and juvenile rearing

Read more

Summary

Introduction

Glacier retreat poses risks and benefits for species of cultural and economic importance. Over the entire study region, we estimate an increase of between 6146 (±1619; this and the following uncertainty corresponds to ± one standard deviation and originate from: GCM projections, ice thickness estimates, and stream segment length) kms and 9296 (±2740) kms of future salmon-accessible streams by 2100 using the RCP4.5 climate scenario under the 10% (Fig. 2) and 15% (Supplementary Fig. 2; Supplementary Table 3) gradient thresholds, respectively.

Results
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.