Document Title - Geoscience Australia
Document Title - Geoscience Australia
Document Title - Geoscience Australia
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Lord Howe High Resolution Grids<br />
SATELLITE DERIVED BATHYMETRY DATA<br />
Two sources of satellite derived bathymetric data were available.<br />
Quickbird<br />
In shallow water areas less than about 20 metres deep it is possible to use multi-spectral satellite data<br />
for the determination of water depth. Images from the Quickbird satellite were obtained and<br />
processed to extract bathymetry in areas close to shore. A complete explanation of the processes<br />
involved in obtaining bathymetry from multi-spectral satellite data is given in Appendix 2. The data<br />
distribution is shown in Figure 19.<br />
ETOPO1<br />
In deep water areas, satellite observations of sea height can be processed to determine the<br />
gravitational field over the ocean surface and estimate an underlying bathymetry (Smith and<br />
Sandwell, 1997). The latest release of this bathymetric dataset is known as ETOPO1 which was<br />
mentioned earlier as one of the publicly available grids covering the Lord Howe Island area.<br />
Unfortunately in the Lord Howe Island area ETOPO1 was found to be about 150 metres too shallow<br />
in many places and too deep in others when compared to soundings data. It was decided to only use<br />
subsets of this dataset in the vicinity of two seamounts. This data was obtained from the NGDC and<br />
is shown with other NGDC data as the two squares of data in Figure 17.<br />
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