Measuring glacier surface roughness using plot-scale, close-range digital photogrammetry. Issue 223 (2014)
- Record Type:
- Journal Article
- Title:
- Measuring glacier surface roughness using plot-scale, close-range digital photogrammetry. Issue 223 (2014)
- Main Title:
- Measuring glacier surface roughness using plot-scale, close-range digital photogrammetry
- Authors:
- Irvine-Fynn, Tristram D.L.
Sanz-Ablanedo, Enoc
Rutter, Nick
Smith, Mark W.
Chandler, Jim H. - Abstract:
- Abstract: Glacier roughness at sub-metre scales is an important control on the ice surface energy balance and has implications for scattering energy measured by remote-sensing instruments. Ice surface roughness is dynamic as a consequence of spatial and temporal variation in ablation. To date, studies relying on singular and/or spatially discrete two-dimensional profiles to describe ice surface roughness have failed to resolve common patterns or causes of variation in glacier surface morphology. Here we demonstrate the potential of close-range digital photogrammetry as a rapid and cost-effective method to retrieve three-dimensional data detailing plot-scale supraglacial topography. The photogrammetric approach here employed a calibrated, consumer-grade 5 Mpix digital camera repeatedly imaging a plot-scale (≤25 m 2 ) ice surface area on Midtre Lovénbreen, Svalbard. From stereo-pair images, digital surface models (DSMs) with sub-centimetre horizontal resolution and 3 mm vertical precision were achieved at plot scales ≤4 m 2 . Extraction of roughness metrics including estimates of aerodynamic roughness length ( z 0 ) was readily achievable, and temporal variations in the glacier surface topography were captured. Close-range photogrammetry, with appropriate camera calibration and image acquisition geometry, is shown to be a robust method to record sub-centimetre variations in ablating ice topography. While the DSM plot area may be limited through use of stereo-pair images andAbstract: Glacier roughness at sub-metre scales is an important control on the ice surface energy balance and has implications for scattering energy measured by remote-sensing instruments. Ice surface roughness is dynamic as a consequence of spatial and temporal variation in ablation. To date, studies relying on singular and/or spatially discrete two-dimensional profiles to describe ice surface roughness have failed to resolve common patterns or causes of variation in glacier surface morphology. Here we demonstrate the potential of close-range digital photogrammetry as a rapid and cost-effective method to retrieve three-dimensional data detailing plot-scale supraglacial topography. The photogrammetric approach here employed a calibrated, consumer-grade 5 Mpix digital camera repeatedly imaging a plot-scale (≤25 m 2 ) ice surface area on Midtre Lovénbreen, Svalbard. From stereo-pair images, digital surface models (DSMs) with sub-centimetre horizontal resolution and 3 mm vertical precision were achieved at plot scales ≤4 m 2 . Extraction of roughness metrics including estimates of aerodynamic roughness length ( z 0 ) was readily achievable, and temporal variations in the glacier surface topography were captured. Close-range photogrammetry, with appropriate camera calibration and image acquisition geometry, is shown to be a robust method to record sub-centimetre variations in ablating ice topography. While the DSM plot area may be limited through use of stereo-pair images and issues of obliquity, emerging photogrammetric packages are likely to overcome such limitations. … (more)
- Is Part Of:
- Journal of Glaciology. Volume 60:Issue 223(2014)
- Journal:
- Journal of Glaciology
- Issue:
- Volume 60:Issue 223(2014)
- Issue Display:
- Volume 60, Issue 223 (2014)
- Year:
- 2014
- Volume:
- 60
- Issue:
- 223
- Issue Sort Value:
- 2014-0060-0223-0000
- Page Start:
- 957
- Page End:
- 969
- Publication Date:
- 2014
- Subjects:
- applied glaciology, -- energy balance, -- glaciological instruments and methods, -- snow/ice surface processes, -- surface melt
- Journal URLs:
- https://www.cambridge.org/core/journals/journal-of-glaciology ↗
- DOI:
- 10.3189/2014JoG14J032 ↗
- Languages:
- English
- ISSNs:
- 0022-1430
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library HMNTS - ELD Digital store
- Ingest File:
- 5756.xml