PExif MM * 0 zi \ Alfred-Wegener-Institut / [Name Fotograf] 0221 Alfred-Wegener-Institut / Flemming Dahlke et al d 0 zi \ Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the study area under Representative Concentration Pathways (RCPs). A–C, RCP8.5: Unabated ocean warming and acidification. D–F, RCP4.5: Intermediate warming (no acidification considered). G–I, RCP2.6: Less than 2 °C global warming (no acidification considered). Maps show the shift in potential egg survival (PES) between the baseline period (1985–2004, Spawning seasons of Atlantic cod: March–May and Polar cod: December–March, see Fig. 3) and the median of CMIP5 multimodel-based projections (seasonal sea surface temperature, 0-50m, see 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 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, 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. NEW, Northeast Water Polynya; FJL, Franz-Joseph-Land, NZ, Novaya Zemlya. . %http://ns.adobe.com/xap/1.0/ Alfred-Wegener-Institut / Flemming Dahlke et al Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the study area under Representative Concentration Pathways (RCPs). A–C, RCP8.5: Unabated ocean warming and acidification. D–F, RCP4.5: Intermediate warming (no acidification considered). G–I, RCP2.6: Less than 2 °C global warming (no acidification considered). Maps show the shift in potential egg survival (PES) between the baseline period (1985–2004, Spawning seasons of Atlantic cod: March–May and Polar cod: December–March, see Fig. 3) and the median of CMIP5 multimodel-based projections (seasonal sea surface temperature, 0-50m, see 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 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, 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. NEW, Northeast Water Polynya; FJL, Franz-Joseph-Land, NZ, Novaya Zemlya. All rights reserved / Editorial use only / With copyright notice only / No Sale / No Promotion – Alle Rechte vorbehalten / Freigegeben zur redaktionellen Berichterstattung über Arbeiten des Alfred-Wegener-Instituts zusammen mit dem Copyright-Vermerk / Kein Verkauf / Keine Werbung. Photoshop 3.0 8BIM hZ %G ( /Freigabe für Berichterstattung über das AWIi KChange in thermally suitable spawning habitat of Atlantic cod and Polar codn Flemming Dahlkes Alfred-Wegener-Institut, Helmholt /Alfred-Wegener-Institut / Flemming Dahlke et alxcChange in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the study area under Representative Concentration Pathways (RCPs). A–C, RCP8.5: Unabated ocean warming and acidification. D–F, RCP4.5: Intermediate warming (no acidification considered). G–I, RCP2.6: Less than 2 °C global warming (no acidification considered). Maps show the shift in potential egg survival (PES) between the baseline period (1985–2004, Spawning seasons of Atlantic cod: March–May and Polar cod: December–March, see Fig. 3) and the median of CMIP5 multimodel-based projections (seasonal sea surface temperature, 0-50m, see 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 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, 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. NEW, Northeast Water Polynya; FJL, Franz-Joseph-Land, NZ, Novaya Zemlya. 8BIM% }gqLCc) Adobe d
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