Aerial imaging of sea ice with LiDAR and photos

An integrated airborne imaging system with scanning LiDAR (Light Detecting And Ranging) and high resolution, digital aerial photography is used by the Australian Antarctic Program for various purposes, in East Antarctica. One of the main objectives is the measurement of surface elevation of sea ice...

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Bibliographic Details
Main Author: Lieser, JL
Format: Conference Object
Language:English
Published: Australian Antarctic Division and Antarctica New Zealand 2013
Subjects:
Online Access:http://ecite.utas.edu.au/90792
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spelling ftunivtasecite:oai:ecite.utas.edu.au:90792 2023-05-15T13:37:23+02:00 Aerial imaging of sea ice with LiDAR and photos Lieser, JL 2013 http://ecite.utas.edu.au/90792 en eng Australian Antarctic Division and Antarctica New Zealand Lieser, JL, Aerial imaging of sea ice with LiDAR and photos, Strategic Science in Antarctica conference program, 24-26 June 2013, Hobart, Tasmania, pp. 1. (2013) [Conference Extract] http://ecite.utas.edu.au/90792 Earth Sciences Physical Geography and Environmental Geoscience Physical Geography and Environmental Geoscience not elsewhere classified Conference Extract NonPeerReviewed 2013 ftunivtasecite 2019-12-13T21:54:06Z An integrated airborne imaging system with scanning LiDAR (Light Detecting And Ranging) and high resolution, digital aerial photography is used by the Australian Antarctic Program for various purposes, in East Antarctica. One of the main objectives is the measurement of surface elevation of sea ice (ice freeboard) and glacial ice to estimate its thickness. To understand the effects and feedbacks of a changing climate in polar regions information on the rate of change of ice thickness is vital. Large-scale coverage of the East Antarctic ice sheet, ice shelves, and the sea ice zone is currently very sparse, with latterly relying on satellite altimetry measurements that are unvalidated and uncalibrated.We describe the combined instrument system and present in-situ results acquired over sea ice in the vicinity of 122 East, 65 South. Validation of the airborne surface elevation data is done by drill-hole measurements of sea ice freeboard and shows agreement to within the centimetre-level. This allows confidence to use the system for large-scale aerial surveys (up to 200 km range) to calibrate and validate space-borne sea ice thickness products, for example from CryoSat-2. Conference Object Antarc* Antarctic Antarctica Australian Antarctic Program East Antarctica Ice Sheet Ice Shelves Sea ice eCite UTAS (University of Tasmania) Antarctic East Antarctic Ice Sheet East Antarctica
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
spellingShingle Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
Lieser, JL
Aerial imaging of sea ice with LiDAR and photos
topic_facet Earth Sciences
Physical Geography and Environmental Geoscience
Physical Geography and Environmental Geoscience not elsewhere classified
description An integrated airborne imaging system with scanning LiDAR (Light Detecting And Ranging) and high resolution, digital aerial photography is used by the Australian Antarctic Program for various purposes, in East Antarctica. One of the main objectives is the measurement of surface elevation of sea ice (ice freeboard) and glacial ice to estimate its thickness. To understand the effects and feedbacks of a changing climate in polar regions information on the rate of change of ice thickness is vital. Large-scale coverage of the East Antarctic ice sheet, ice shelves, and the sea ice zone is currently very sparse, with latterly relying on satellite altimetry measurements that are unvalidated and uncalibrated.We describe the combined instrument system and present in-situ results acquired over sea ice in the vicinity of 122 East, 65 South. Validation of the airborne surface elevation data is done by drill-hole measurements of sea ice freeboard and shows agreement to within the centimetre-level. This allows confidence to use the system for large-scale aerial surveys (up to 200 km range) to calibrate and validate space-borne sea ice thickness products, for example from CryoSat-2.
format Conference Object
author Lieser, JL
author_facet Lieser, JL
author_sort Lieser, JL
title Aerial imaging of sea ice with LiDAR and photos
title_short Aerial imaging of sea ice with LiDAR and photos
title_full Aerial imaging of sea ice with LiDAR and photos
title_fullStr Aerial imaging of sea ice with LiDAR and photos
title_full_unstemmed Aerial imaging of sea ice with LiDAR and photos
title_sort aerial imaging of sea ice with lidar and photos
publisher Australian Antarctic Division and Antarctica New Zealand
publishDate 2013
url http://ecite.utas.edu.au/90792
geographic Antarctic
East Antarctic Ice Sheet
East Antarctica
geographic_facet Antarctic
East Antarctic Ice Sheet
East Antarctica
genre Antarc*
Antarctic
Antarctica
Australian Antarctic Program
East Antarctica
Ice Sheet
Ice Shelves
Sea ice
genre_facet Antarc*
Antarctic
Antarctica
Australian Antarctic Program
East Antarctica
Ice Sheet
Ice Shelves
Sea ice
op_relation Lieser, JL, Aerial imaging of sea ice with LiDAR and photos, Strategic Science in Antarctica conference program, 24-26 June 2013, Hobart, Tasmania, pp. 1. (2013) [Conference Extract]
http://ecite.utas.edu.au/90792
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