Changing ice and changing light: trends in solar heat input to the upper Arctic ocean from 1988 to 2014

• Published in: Annals of Glaciology
• Main Authors: Donald Perovich, Bonnie Light, Suzanne Dickinson
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2020
• Subjects: Sea ice; sea-ice growth and decay; surface mass budget; Meteorology. Climatology; QC851-999; Arctic; Arctic Ocean; Annals of Glaciology
• Online Access: https://doi.org/10.1017/aog.2020.62; https://doaj.org/article/f4ef21783f3a4182baaf2a8face2aeb4

The Arctic sea-ice cover has undergone a significant decline in recent decades. The melt season is starting earlier, ice is thinner and seasonal ice dominates. Here we examine the effects of these changes on the solar heat input to the upper ocean in ice-covered Arctic waters from 1985 to 2014. Satellite observations of ice concentration, onset dates of melt and freeze-up and ice age, are combined with ice thicknesses from the PIOMAS model and incident solar irradiance from reanalysis products to calculate the contributions of open ocean and ice to the solar heat input in the upper ocean. Of the total, 86% of the area has positive trends for solar heat input to the ocean through leads due to decreases in ice concentration. Only 62% of the area shows positive trends of solar heat input to the ocean explicitly through the ice. Positive trends are due to thinning ice, while negative trends occur in regions where the ice-free season has lengthened. The annual total solar heat input to the ocean exhibits positive trends in 82% of the area. The spatial pattern of the cumulative annual total solar heat input is similar to the pattern of solar heat input directly to leads.