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The potential of sea ice leads as a predictor for summer Arctic sea ice extent

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Figure

Figure 1. (a) MODIS cloud fraction (%), (b) SAR backscatter coefficient image, and (c) MODIS sea ice leads in the highlighted area (thenorthern Beaufort Sea) as shown by the box in (d) on 11 April 2015.
Figure 2 shows the evolution of the daily total area of seaice leads in the Arctic Ocean from 1 January to 30 Aprilaveraged for the period of 2003–2015
Figure 4. Spatial distribution of significant negative correlations between the area of sea ice leads integrated for 30 daysf, j)correlation exceeding the 95 % confidence level are marked with black crosses and the color shading is the averaged area of sea i
Figure 5. Evolution of correlation coefficients between the totalarea of sea ice leads integrated from 1 January to 30 April and thetotal Arctic sea ice extent in July (blue line), August (green line)and September (red line) during 2003–2015
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