frustratedartist
9 February 2012 1:08PM
Next to this story I notice there is a link to a story about the retreat of Himalayan glaciers over the last 50 years- a slightly longer timescale. Glaciers in other parts of the world are also retreating, causing serious problems to water supply in mountain cities like La Paz, Bolivia.
So- two questions I'd like to ask professor Bamber: question 1: Is it reasonable to assume that the general tendency is that, globally, glaciers are retreating?
And also, question 2 : for people studying climate change, what is the most meaningful timescale? Does it make most sense to look at changes (in whatever indicators are being measured) on a year-by-year basis, a decade by decade basis, a century by century basis- or some other timescale?
@frustratedartist. Here's my answer two your two good questions
1) Yes. If you look at the larger glaciers systems (Alaska, Canadian Arctic, Patagonia, Antarctica, Greenland) they all show a significant -ve trend that is larger than the uncertainty. For the smaller systems such as the Alps, where there is relatively good in-situ observations, these also show a -ve trend. The uncertainties in the GRACE estimates for these smaller systems are about the same size as the signal, which is why hard to use them to determine smaller loss terms.
2) So what is the right timescale? This all depends on the system you're interested in and what you want to know. For example, the deep, abyssal circulation in the ocean takes thousands of years, while mesoscale eddies at the surface come and go over a few weeks. Generally, 30 years is considered to be a reasonable period for looking at climatological means that are controlled be atmospheric processes. In other words, over this timescale, inter-annual variability is reduced so that trends should be visible. In my article, and in the authors paper, we acknowledge that 8 years is a short time period and it is important, therefore, not to over-interpret the results.