paraview software v 5.2.0  (Kitware Inc)

Journal: Scientific Reports

Article Title: A unified framework for modelling sediment fate from source to sink and its interactions with reef systems over geological times

doi: 10.1038/s41598-018-23519-8

Figure Lengend Snippet: ( a ) Map shows the extend of the 2 regions (i-north, ii-south) of the GBR used in this study (source: Project 3DGBR-eAtlas.org.au ). ( b ) Background map shows the average rainfall annual distribution based on 30-year records (1961–1990) encompassing several ENSO events (7 El Niño - 5 La Niña) (source: Bureau of Meteorology ). White lines highlight precipitation 0.5 m/a contours. Red arrows define prevailing annual offshore wave directions scaled based on their annual activity. Wave heights (H) imposed for the considered 2 climatic scenarios from 14 to 5 ka and from 5 ka to present. Both maps were generated using Paraview (V 5.2.0).

Article Snippet: All the model outputs were visualised using the Paraview software (V 5.2.0) from Kitware, Sandia National Labs and CSimSoft.

Techniques: Activity Assay, Generated

Journal: Scientific Reports

Article Title: A unified framework for modelling sediment fate from source to sink and its interactions with reef systems over geological times

doi: 10.1038/s41598-018-23519-8

Figure Lengend Snippet: Sensitivity analysis of erodibility coefficient ( κ e in eq. ) at final time step for 5 simulations showing its effects on sediment accumulation (Mt/yr) and Fitzroy delta progradation (Fitzroy area is shown in Fig. ) visualised with Paraview (V 5.2.0). Lower right panel presents today’s topography from Map Data @2018 GBRMPA, Google.

Article Snippet: All the model outputs were visualised using the Paraview software (V 5.2.0) from Kitware, Sandia National Labs and CSimSoft.

Techniques:

Journal: Scientific Reports

Article Title: A unified framework for modelling sediment fate from source to sink and its interactions with reef systems over geological times

doi: 10.1038/s41598-018-23519-8

Figure Lengend Snippet: Model outputs for initial time step (14 ka), 10 ka, 6 ka and final step. Left and right panels show the evolution for the northern ( a ) and southern ( b ) parts of the GBR through the Holocene period (respectively i & ii regions in Fig. ). Pink color displays presence of coral reef at given time intervals. Model outputs are visualised using Paraview (V 5.2.0).

Article Snippet: All the model outputs were visualised using the Paraview software (V 5.2.0) from Kitware, Sandia National Labs and CSimSoft.

Techniques: Northern Blot

Journal: Scientific Reports

Article Title: A unified framework for modelling sediment fate from source to sink and its interactions with reef systems over geological times

doi: 10.1038/s41598-018-23519-8

Figure Lengend Snippet: Maps of cumulative erosion/deposition in metres at final time step for the northern (a and b panels) and southern ( c and d ) GBR regions visualised using Paraview (V 5.2.0). Left panels (a and c) display the cumulative effects of wave-induced erosion and deposition over the simulated period (14 ka). Right panels (b and d) show the erosion, deposition and reef evolution for the 14 ka induced by the combination of fluvial and waves processes as well as reef growth. Sections 1 and 2 are the locations of the stratigraphic cross-sections displayed in Fig. .

Article Snippet: All the model outputs were visualised using the Paraview software (V 5.2.0) from Kitware, Sandia National Labs and CSimSoft.

Techniques: Northern Blot

Journal: Scientific Reports

Article Title: A unified framework for modelling sediment fate from source to sink and its interactions with reef systems over geological times

doi: 10.1038/s41598-018-23519-8

Figure Lengend Snippet: ( a ) 3D view of the GBR between Cairns and Cooktown highlighting sediment transport from mountain ranges to the coast, and from the coast to the Queensland Trough (generated using Paraview (V 5.2.0)). On the inner shelf dominant wave direction (SE) rework sediments to the North (black arrows). On the mid shelf, coral reef develops. Sediment transfer across the slope happens through V-shaped canyons. White lines (1–2–3) mark the location of seismic lines in b. ( b ) Topas seismic section illustrating sediment gravity flow (SGF) and thin-bedded deposits for Canyon 8. ( c ) 3D view of the Noggin region (canyons and slope) with draped GLORIA side-scan sonar backscatter imagery. High-reflectivity (white toned) areas correspond to SGFs and landslide deposits ( b and c are adapted from Puga-Bernabéu et al . ).

Article Snippet: All the model outputs were visualised using the Paraview software (V 5.2.0) from Kitware, Sandia National Labs and CSimSoft.

Techniques: Generated