Looking at both area and extent for September from the NSIDC Sea Ice Index I have calculated the interannual differences and expressed them as their absolute values (i.e. no sign, + or -). Interannual variability increased in the late a 1990s due to dynamic impacts such a Fram Strait export, due to the Arctic Oscillation (and the Pacific Decadal Oscillation).
The seven year average suggests a recent increase in variability, however this is almost totally due to the 2007 and 2012 record lows, and the increase of extent in years following those record years.
So why should we should see an increase in variability as winter thickness approaches summer thinning? The answer is quite intuitive, small variations in the actual amount of winter thickness or summer thinning have a greater impact on how much open water forms by the end of the summer as summer thinning gets closer to winter thickness. That's just intuition, what might a simple model show?
I have made a very simple illustrative model of an ocean with static sea ice. There are 30 boxes of ice, the initial (winter) thickness is 3 thickness units (could be metres), the nominal summer loss of thickness is 2 units. The initial thickness and the nominal summer thickness are both varied separately in each box using a random number from a normal distribution with a standard deviation of 0.5 thickness units. This simulates weather effects on both initial thickness and summer melt.
Then the initial thickness is reduced each 'year' by 0.01 thickness units, this simulates a thinning of the ice model, at a very slow linear rate.
Each of the 30 'boxes' of ice is set such that it has an area of 1 if the difference between initial thickness and summer loss of thickness. i.e. if there is even a small amount of ice the area is 1 and counts towards overall area. The overall area is calculated by summing the area of all the boxes.
20 runs of the simple model have been done. Here is the result of all runs as initial (winter) thickness declines from 3 thickness units to 1 unit.
The application of a random normally distributed noise to the calculations introduces substantial variabilty to the trajectories of individual years. Those used to following sea ice might see a hint of a sigmoid curve. I shall return to this issue shortly. What is notable is that the steepest curve is at 2 thickness units, which is the central value of the summer loss of thickness.
The following graph is the average area of the above 20 runs for each increment together with the line defining the underlying decline in initial thickness (before the random variation is applied to each of the 30 boxes).
So the linear decline of thickness (red) is being transformed into a sigmoid decline of area (blue). This cannot be due to any feedbacks in the ice, the model contains no such physics.
Consider the behaviour of my illustrative model with no noise. Area will be 30 until the thinning of initial thickness goes below 2 thickness units, at which point summer thinning removes all ice and the area crashes abruptly to zero. This gives a step function with a value of 30 above a thickness of 2 and 0 below 2.
When I introduce noise (weather) into the picture the effect is to introduce a normal distribution bell curve. Essentially what is going on is the the step loss of area where initial thickness equals summer melt is smeared (actually a convolution) by the bell curve of the random noise and the result is a curve similar to a sigmoid function.
So back to the original purpose of the post, a supposed increase in variability as the pack thins. I have taken the 20 runs, calculated the average interannual difference for all 20 at each increment of initial thickness and the result is plotted below.
As the ice in this simple illustrative model thins to around the summer thinning amount, the interannual variance increases and peaks as summer thinning equals winter initial thickness.
Across much of the Arctic Ocean at present, peak winter ice thickness in April is very close to summer thinning. There has been an increase in interannual variability but this is mainly related to two record crash years, it might be that we need more years of data to see the real pattern. The illustrative model here uses a shallow decline of thickness over what is in effect 200 years, the actual transition to a seasonally ice free state is progressing much faster.
One implication is that greater variability from year to year does not necessarily herald a rapid collapse of the Arctic sea ice, since this is seen in an illustrative model with a strictly linear decline in initial thickness. It is also interesting that the sigmoid shape arises without any thermodynamics in this simple illustrative model.