|
|
|
|
|
by archgoon
3355 days ago
|
|
The wording is ambiguous. In general, trying to determine whether a statement about probability is correct or not requires more information than can be encapsulated in a single sentence. The English language does not help in this. We're not going to get more information here without someone looking into where the .5% number comes from. |
|
The method of Roe et al. is summarized as follows. Let 1L be the change in glacier length over the past 130 years (∼1.9 km), and let σL be the standard deviation of glacier length due to stochastic fluctuations in mass balance, b, from natural, interannual climate variability. The signal-to-noise ratio is defined by sL =1L/σL . Likewise, sb =1b/σb . Ref. 12 demonstrates that the two are related via sL =γ sb , where γ is an amplification factor that depends only on the duration of the trend and the glacier response time, τ . The probability density function (PDF) for sb is generated by combining the signal-to-noise ratios of the observed melt-season temperature and annual-mean precipitation trends, normalized by the summer (bs) and winter (bw ) mass-balance variability (Supplementary Fig. 1a,b,c), respectively. We take σbw = 0.3 myr−1 and σbs =0.5 myr−1 , based on the observed mass-balance variability at Gulkana Glacier and the analysis of the global datasets of glacier mass balance33. The glacier response time is given by τ =−H/bt , where H is a characteristic glacier thickness, and bt is the (negative) net mass balance at the terminus. We set H=590 m, based on the scaling relationship for glacier geometry suggested by Haeberli and Hoelzle34 and measured cross-sections35; and we set bt =−7 myr−1 , estimated by extrapolating the vertical mass-balance profiles calculated by Flowers et al.8 , thus giving a central estimate for τ of ∼80 years. A PDF is estimated assuming τ follows a gamma distribution incorporating a broad uncertainty of στ =τ /4 (Supplementary Fig. 1d). The PDFs for γ and sb are combined to give a PDF for σL from the relation σL =γ 1L| obssb . This, in turn, is used to evaluate the null hypothesis that 1L| obs occurred due to natural variability. Supplementary Fig. 1e shows our estimate that there is only a 0.5% chance that the observed retreat of Kaskawulsh Glacier happened in the absence of a climate trend.