Estimate of Glacier Ablation under a Debris Layer from Surface Temperature and Meteorological Variables

Abstract A simple model suggests that the ablation under a debris layer could be estimated from meteorological variables if the surface temperature data of the layer are available. This method was tested by analyzing the data obtained from experiments with artificial debris layers. Fairly good agree...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Nakawo, M., Young, G.J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1982
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300001176x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001176X
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Summary:Abstract A simple model suggests that the ablation under a debris layer could be estimated from meteorological variables if the surface temperature data of the layer are available. This method was tested by analyzing the data obtained from experiments with artificial debris layers. Fairly good agreement was obtained between the estimated and the experimental data.