Abstract
A statistical analysis has been made of the annual balances collected during 16 consecutive years at 32 sites on the ablation area of the Glacier de Saint-Sorlin (French Alps). Only 38% of the 32 × 16 balances are known; moreover in 8 cases only the total balance for 2 consecutive years is known, and in one case the balance for 4 consecutive years. A comprehensive study of the errors leads us to assume the following linear model for the annual balancexjtat site j for yeart:whereαjandβtare parameters depending upon the site and the year respectively,ηjtandη’jtare random errors with a Gaussian distribution and standard errorsσandσ’respectively. Assuming some known value forσ’2/σ2=ρ, the parametersαjandβt,their variance–covariance matrix, and the variance covariance matrix of the residuals are estimated in the most general case. The estimators being stable against variations inρ,the valueρ= o may be assumed; this value docs not conflict with the behaviour of the estimates of the residuals. A test of the linear model derived from Tukey’s non-additivity test is positive. Although a much more general, non-linear modelgives a better representation of 13 × 6 balances forming a complete table of data, the linear model withσ≈ 0.20 m is good enough to be used in theoretical studies or in routine work.
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