Here is a comparison of 2015 to 2018, during the past three days (24-26 July),
How high is the 100% concentration bin for this year?
I don't have that data file with me (I'm away from home today) but it was quite high, suggesting to me that there is something slightly odd going on. Maybe the algorithm that produces ice concentration from brightness temperature would assign some grid cells a concentration over 100%, and those are set to 100, resulting in a "spike" at that value? But there were no 100% cells in the three-day average from 2015, just in the 2018 data set. I'll post the exact numbers when I get a chance.
Or, if someone is interested, they can go here:
ftp://sidads.colorado.edu/DATASETS/NOAA/G02135/north/daily/geotiff/2018/07_Jul/and download the concentration GeoTIFF files for the three days of 2018 (and 2015), and count the number of pixels with values of 1000 (the GeoTIFF concentration data are scaled by a factor of 10).
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Edited to add:
OK, I found the numbers, here they are.
For 2018, there was 398.75k km2 with an average concentration of 100% over the three-day window. An additional 1266.25k km2 had a concentration of 90% to 99.9%.
For 2015, there were no grid cells that had an average concentration of 100%. There was 510k km2 with a concentration of 90% to 99.9%.
Maps below of the 3-day averages. Red = 100% concentration; orange = 90% to 99.9%.
2015:
2018:
I am wondering whether the difference is because the 2018 data are based on the NRT version of the CDR process, while the 2015 data are the final version of the CDR. I probably ought to have a better understanding of that.