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Record #210929:
Grounding-zone ice thickness from InSAR: inverse modelling of tidal elastic bending / Oliver J. Marsh, and 4 others.
Title: | Grounding-zone ice thickness from InSAR: inverse modelling of tidal elastic bending / Oliver J. Marsh, and 4 others. |
Author(s): | Marsh, Oliver J. |
Date: | 2014. |
In: | Journal of Glaciology. (2014.), Vol. 60(221) (2014) |
Abstract: | Demonstrates that inverse formulation of plate-bending equations, based on simple elastic assumptions, can be used to solve for ice thickness in Antarctic ice shelf grounding zones, using vertical deflection information. Estimates vertical displacement with differential synthetic aperture radar (SAR) interferograms for 2012. Tests and validates in grounding zone of Beardmore Glacier, Transantarctic mountains, Antarctica. |
Notes: | Journal of Glaciology. Vol. 60(221) :526-536 (2014). |
Keywords: | 551.32 -- Glaciology. 551.321 -- Glaciological methods and instruments. 551.321.6 -- Ice thickness, measurement. 551.324 -- Land ice. 551.324.22 -- Glaciers: Beardmore. 551.324.3 -- Land ice, depth measurements. 551.324.28 -- Ice shelves. 53.087.23 -- Remote sensing. 621.396.96 -- Radar. E3 -- Glaciology: instruments and methods. (*7) -- Antarctic regions. (*749.5) -- Transantarctic Mountains, Victoria Land. |
SPRI record no.: | 210929 |
LDR 01758naa#a2200000#a#4500 001 SPRI-210929 005 20240328210817.0 007 ta 008 240328s2014####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-210929 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMarsh, Oliver J. 245 10 ‡aGrounding-zone ice thickness from InSAR :‡binverse modelling of tidal elastic bending /‡cOliver J. Marsh, and 4 others. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2014. 300 ## ‡ap. 526-536 :‡bill., diags., tables. 500 ## ‡aJournal of Glaciology. Vol. 60(221) :526-536 (2014). 520 3# ‡aDemonstrates that inverse formulation of plate-bending equations, based on simple elastic assumptions, can be used to solve for ice thickness in Antarctic ice shelf grounding zones, using vertical deflection information. Estimates vertical displacement with differential synthetic aperture radar (SAR) interferograms for 2012. Tests and validates in grounding zone of Beardmore Glacier, Transantarctic mountains, Antarctica. 530 ## ‡aAlso issued online ‡uurn:doi:10.3189/2014JoG13J033‡uhttps://dx.doi.org/10.3189/2014JoG13J033 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.321 -- Glaciological methods and instruments.‡2udc 650 07 ‡a551.321.6 -- Ice thickness, measurement.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers: Beardmore.‡2udc 650 07 ‡a551.324.3 -- Land ice, depth measurements.‡2udc 650 07 ‡a551.324.28 -- Ice shelves.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a621.396.96 -- Radar.‡2udc 650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*749.5) -- Transantarctic Mountains, Victoria Land.‡2udc 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 60(221) (2014) ‡wSPRI-20534 916 ## ‡a2014/11/04 -- JHR 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240328 ‡bJHR