To answer a 40-year-old question about Arctic ice thickness, scientists have treated the ice floes of the frozen seas like colliding molecules in a fluid or gas.
Although today’s highly precise satellites do a fine job of measuring the area of sea ice, measuring the volume has always been a tricky business.
The volume is reflected through the distribution of sea ice thickness—which is subject to a number of complex processes, such as growth, melting, ridging, rafting, and the formation of open water.
We transformed the intransigent term into something tractable and—poof—solved it.
, Yale University professor