Fig. 5 Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the Seas of Norden under RCPs. Change in thermally.

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Fig. 5 Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the Seas of Norden under RCPs. Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the Seas of Norden under RCPs. (A to C) RCP8.5: Unabated OWA. (D to F) RCP4.5: Intermediate warming (no acidification considered). (G to I) RCP2.6: Less than 2°C global warming (no acidification considered). Maps show the shift in PES between the baseline period (1985–2004; spawning season of Atlantic cod: March to May; spawning season of Polar cod: December to March; see Fig. 3) and the median of CMIP5 multimodel-based projections (seasonal sea surface temperature, 0 to 50 m; see Materials and Methods) for this century’s end (2081–2100). Black shading indicates areas (cells, 1° × 1°) with high uncertainty (that is, the shift in PES within that cell is smaller than the CMIP5 ensemble spread; see Materials and Methods). Dotted magenta lines represent the sea-ice edge positions of the respective species-specific spawning season (defined as areas with ice concentrations > 70%). (C, F, and I) For each map, values (change in PES) of individual cells are summarized by kernel density estimations, with the width corresponding to the relative occurrence of values. Box plots show the 25th, 50th, and 75th percentile; the ends of the whiskers mark the 95% intervals. Flemming T. Dahlke et al. Sci Adv 2018;4:eaas8821 Copyright © 2018 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).