609
Views
6
CrossRef citations to date
0
Altmetric
Original Articles

Disintegration and acceleration of Thwaites Ice Shelf on the Amundsen Sea revealed from remote sensing measurements

, , , &
Pages 498-509 | Received 22 Jan 2015, Accepted 14 Apr 2015, Published online: 11 May 2015

Figures & data

Figure 1. a. Moderate Resolution Imaging Spectroradiometer composite image of the study area and in situ survey and bottom topography in the Amundsen Sea coast, West Antarctica. b. Detailed bathymetry beneath Thwaites and its eastern Ice Shelves.

Figure 1. a. Moderate Resolution Imaging Spectroradiometer composite image of the study area and in situ survey and bottom topography in the Amundsen Sea coast, West Antarctica. b. Detailed bathymetry beneath Thwaites and its eastern Ice Shelves.

Table 1. The specification of remote sensing data used in this study.

Figure 2. Landsat 7 ETM+ images from 2000 to 2012, shown by the black dotted box in . The hatched pattern is the result of the failure of the Scan Line Corrector (SLC) of Landsat in 2003, according to the statement from the United States Geological Survey.

Figure 2. Landsat 7 ETM+ images from 2000 to 2012, shown by the black dotted box in Figure 1a. The hatched pattern is the result of the failure of the Scan Line Corrector (SLC) of Landsat in 2003, according to the statement from the United States Geological Survey.

Figure 3. Spatial distribution of the shear and rift zones between Thwaites and its eastern ice shelf.

Figure 3. Spatial distribution of the shear and rift zones between Thwaites and its eastern ice shelf.

Figure 4. Variations of ice flow velocities at various locations on Thwaites Ice Shelf derived from multi-temporal Landsat images acquired from 2000 to 2012, except 2005.

Figure 4. Variations of ice flow velocities at various locations on Thwaites Ice Shelf derived from multi-temporal Landsat images acquired from 2000 to 2012, except 2005.

Figure 5. Mean ice flow speeds estimated from time series of Landsat data (from 2000 to 2012, except 2005) at three sites (A, B, and C) shown in .

Figure 5. Mean ice flow speeds estimated from time series of Landsat data (from 2000 to 2012, except 2005) at three sites (A, B, and C) shown in Figure 3.

Figure 6. Profiles of conductivity–temperature–depth (CTD) data shown in . The solid and dashed lines indicate observed temperature–freezing temperature (TTf) and observed salinity, respectively.

Figure 6. Profiles of conductivity–temperature–depth (CTD) data shown in Figure 1a. The solid and dashed lines indicate observed temperature–freezing temperature (T–Tf) and observed salinity, respectively.

Figure 7. Comparisons of crevasse patterns in TerraSAR-X and GeoEye-1 images captured on 25 September 2009, and 27 January 2010, respectively, shown by the green dotted box in .

Figure 7. Comparisons of crevasse patterns in TerraSAR-X and GeoEye-1 images captured on 25 September 2009, and 27 January 2010, respectively, shown by the green dotted box in Figure 3.

Figure 8. Comparisons of crevasse patterns in Landsat 7 ETM+, aerial photography, and spaceborne SAR images near the grounding line of Thwaites Ice Shelf.

Figure 8. Comparisons of crevasse patterns in Landsat 7 ETM+, aerial photography, and spaceborne SAR images near the grounding line of Thwaites Ice Shelf.

Figure 9. Comparisons of crevasse patterns in Landsat 7 ETM+, aerial photography, airborne, and spaceborne SAR images of Thwaites Ice Shelf terminus.

Figure 9. Comparisons of crevasse patterns in Landsat 7 ETM+, aerial photography, airborne, and spaceborne SAR images of Thwaites Ice Shelf terminus.

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.