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Ice discharge error estimates using different cross-sectional area approaches: a case study for the Canadian High Arctic, 2016/17

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Figure

Fig. 1. (a) Main ice masses of Ellesmere, Axel Heiberg and Devon Islands, Canadian High Arctic (Wessel and Smith, 1996 )
Table 1. Operation IceBridge airborne radar profiles used in this study. Cross means cross-sectional profiles and Long means  longitu-dinal (along-flow, close to glacier centreline) profiles
Fig. 2. Geometry of the U-shaped cross-sectional approaches used in this study. The blue line represents the actual cross profile of Glacier North 3 (Fig
Table 2 shows the discharge results obtained, for the winters of 2016 and 2017, for all glaciers with available  cross-sec-tional radar profiles, together with their corresponding error estimates and the detail of the various error components
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