Preprints
https://doi.org/10.5194/bg-2020-279
https://doi.org/10.5194/bg-2020-279

  05 Aug 2020

05 Aug 2020

Review status: a revised version of this preprint was accepted for the journal BG and is expected to appear here in due course.

Coastal processes modify projections of some climate-driven stressors in the California Current System

Samantha A. Siedlecki1, Darren Pilcher2, Evan M. Howard3, Curtis Deutsch3, Parker MacCready3, Emily L. Norton2, Hartmut Frenzel3, Jan Newton4, Richard A. Feely5, Simone R. Alin5, and Terrie Klinger6 Samantha A. Siedlecki et al.
  • 1Department of Marine Sciences, University of Connecticut, Groton, CT 06340, USA
  • 2CICOES, University of Washington, Seattle, WA 98195, USA
  • 3School of Oceanography, University of Washington, Seattle, WA 98195, USA
  • 4Applied Physics Laboratory, University of Washington, Seattle, WA 98105, USA
  • 5NOAA Pacific Marine Environmental Lab (PMEL), Seattle, WA 98115, USA
  • 6School of Marine Environment and Affairs, University of Washington, Seattle, WA 98105, USA

Abstract. Global projections for ocean conditions in 2100 predict that the North Pacific will experience some of the largest changes. Coastal processes that drive variability in the region can alter these projected changes, but are poorly resolved by global coarse resolution models. We quantify the degree to which local processes modify biogeochemical changes in the eastern boundary California Current System (CCS) using multi-model regionally downscaled climate projections of multiple climate-associated stressors (temperature, O2, pH, Ω, and CO2). The downscaled projections predict changes consistent with the directional change from the global projections for the same emissions scenario. However, the magnitude and spatial variability of projected changes are modified in the downscaled projections for carbon variables. Future changes in pCO2 and surface Ω are amplified while changes in pH and upper 200 meter Ω are dampened relative to the projected change in global models. Within the CCS, differences in global and downscaled climate stressors are spatially variable, and the northern CCS experiences the most intense modification. These projected changes are consistent with source waters lower in oxygen, higher in nutrients, and in combination with solubility-driven changes, altered future upwelled waters in the CCS. The results presented here suggest coastal process resolving projections are necessary for adequate representation of the magnitude of projected change in pH and carbon stressors in the CCS.

Samantha A. Siedlecki et al.

 
Status: closed
Status: closed
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Samantha A. Siedlecki et al.

Samantha A. Siedlecki et al.

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Short summary
Future ocean conditions can be assessed using present trends in fossil fuel use paired with earth system models. Global earth system models generally do not include the full range of local processes important to coastal ecosystems. Compared to global changes, these coastal processes alter the degree of change observed. Higher resolution models that include local processes driven by the global earth system simulations predict modified changes in carbon stressors than projected by global models.
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