Ice bed topography mapping using InSAR and tomographic processes

Chris Allen; William Blake; Carl Leuschen; John Paden; Prasad Gogineni; Dorthe Dahl-Jensen; Ayyangar Harish

doi:10.1109/RADAR.2011.5960646

Ice bed topography mapping using InSAR and tomographic processes

Chris Allen, William Blake, Carl Leuschen, John Paden, Prasad Gogineni, Dorthe Dahl-Jensen, Ayyangar Harish

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › peer-review

3 Scopus citations

Abstract

Three-dimensional topographic maps of the bed 2.5-km beneath the Greenland ice sheet in a 10-km x 10-km region centered on the NEEM drill site (77.45°N 51.06°W) are produced using different processes - interpolation, interferometry, and tomography. Descriptions of the data collection and processing are followed by the terrain maps which are compared. Effects of basal slope and roughness on basal backscattering were modeled in an attempt to highlight the contribution of bed wetness variations in basal SAR intensity maps.

Original language	English
Title of host publication	RadarCon'11 - In the Eye of the Storm
Subtitle of host publication	2011 IEEE Radar Conference
Pages	793-797
Number of pages	5
DOIs	https://doi.org/10.1109/RADAR.2011.5960646
State	Published - 2011
Externally published	Yes
Event	2011 IEEE Radar Conference: In the Eye of the Storm, RadarCon'11 - Kansas City, MO, United States Duration: May 23 2011 → May 27 2011

Publication series

Name	IEEE National Radar Conference - Proceedings
ISSN (Print)	1097-5659

Conference

Conference	2011 IEEE Radar Conference: In the Eye of the Storm, RadarCon'11
Country/Territory	United States
City	Kansas City, MO
Period	05/23/11 → 05/27/11

Keywords

InSAR
VHF-band
depth sounding
multi-channel
tomography

Access to Document

10.1109/RADAR.2011.5960646

Cite this

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title = "Ice bed topography mapping using InSAR and tomographic processes",

abstract = "Three-dimensional topographic maps of the bed 2.5-km beneath the Greenland ice sheet in a 10-km x 10-km region centered on the NEEM drill site (77.45°N 51.06°W) are produced using different processes - interpolation, interferometry, and tomography. Descriptions of the data collection and processing are followed by the terrain maps which are compared. Effects of basal slope and roughness on basal backscattering were modeled in an attempt to highlight the contribution of bed wetness variations in basal SAR intensity maps.",

keywords = "InSAR, VHF-band, depth sounding, multi-channel, tomography",

author = "Chris Allen and William Blake and Carl Leuschen and John Paden and Prasad Gogineni and Dorthe Dahl-Jensen and Ayyangar Harish",

year = "2011",

doi = "10.1109/RADAR.2011.5960646",

language = "English",

isbn = "9781424489022",

series = "IEEE National Radar Conference - Proceedings",

pages = "793--797",

booktitle = "RadarCon'11 - In the Eye of the Storm",

note = "2011 IEEE Radar Conference: In the Eye of the Storm, RadarCon'11 ; Conference date: 23-05-2011 Through 27-05-2011",

}

Allen, C, Blake, W, Leuschen, C, Paden, J, Gogineni, P, Dahl-Jensen, D & Harish, A 2011, Ice bed topography mapping using InSAR and tomographic processes. in RadarCon'11 - In the Eye of the Storm: 2011 IEEE Radar Conference., 5960646, IEEE National Radar Conference - Proceedings, pp. 793-797, 2011 IEEE Radar Conference: In the Eye of the Storm, RadarCon'11, Kansas City, MO, United States, 05/23/11. https://doi.org/10.1109/RADAR.2011.5960646

TY - GEN

T1 - Ice bed topography mapping using InSAR and tomographic processes

AU - Allen, Chris

AU - Blake, William

AU - Leuschen, Carl

AU - Paden, John

AU - Gogineni, Prasad

AU - Dahl-Jensen, Dorthe

AU - Harish, Ayyangar

PY - 2011

Y1 - 2011

N2 - Three-dimensional topographic maps of the bed 2.5-km beneath the Greenland ice sheet in a 10-km x 10-km region centered on the NEEM drill site (77.45°N 51.06°W) are produced using different processes - interpolation, interferometry, and tomography. Descriptions of the data collection and processing are followed by the terrain maps which are compared. Effects of basal slope and roughness on basal backscattering were modeled in an attempt to highlight the contribution of bed wetness variations in basal SAR intensity maps.

AB - Three-dimensional topographic maps of the bed 2.5-km beneath the Greenland ice sheet in a 10-km x 10-km region centered on the NEEM drill site (77.45°N 51.06°W) are produced using different processes - interpolation, interferometry, and tomography. Descriptions of the data collection and processing are followed by the terrain maps which are compared. Effects of basal slope and roughness on basal backscattering were modeled in an attempt to highlight the contribution of bed wetness variations in basal SAR intensity maps.

KW - InSAR

KW - VHF-band

KW - depth sounding

KW - multi-channel

KW - tomography

UR - https://www.scopus.com/pages/publications/80052509538

U2 - 10.1109/RADAR.2011.5960646

DO - 10.1109/RADAR.2011.5960646

M3 - Conference contribution

AN - SCOPUS:80052509538

SN - 9781424489022

T3 - IEEE National Radar Conference - Proceedings

SP - 793

EP - 797

BT - RadarCon'11 - In the Eye of the Storm

T2 - 2011 IEEE Radar Conference: In the Eye of the Storm, RadarCon'11

Y2 - 23 May 2011 through 27 May 2011

ER -

Ice bed topography mapping using InSAR and tomographic processes

Abstract

Publication series

Conference

Keywords

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