Abstract
In deriving elevation change rates (dH/dt) from radar altimetry, the slope-induced error is usually assumed to cancel out in repeat measurements. These measurements, however, represent a location that can be significantly further upslope than assumed, causing an underestimate of the basin-integrated volume change. In a case-study for the fast-flowing part of Jakobshavn Isbr', we show that a relatively straightforward correction for slope-induced error increases elevation change rates by up to several metres per year and significantly reduces the volume change error with respect to laser altimetry for the area of interest.
| Translated title of the contribution | Importance of slope-induced error correction in volume change estimates from radar altimetry |
|---|---|
| Original language | English |
| Pages (from-to) | 447-451 |
| Number of pages | 5 |
| Journal | Cryosphere |
| Volume | 6 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 2012 |
Research Groups and Themes
- Bristol Glaciology Centre
Keywords
- GREENLAND ICE-SHEET
- CONTINENTAL ICE
- ELEVATION CHANGES
- LASER ALTIMETRY
- ACCURACY
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