dugongs in palau - C3
dugongs in palau - C3
dugongs in palau - C3
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Prelim<strong>in</strong>ary surveys<br />
The sel ected sites were visited and prelim<strong>in</strong>ary surveys were done to determ<strong>in</strong>e the overall composition of<br />
the area. These surveys were very quick qualitative surveys. The techniques <strong>in</strong>volved <strong>in</strong> the survey were<br />
fairly simple. At the site, random po<strong>in</strong>ts were chosen and the GPS coord<strong>in</strong>ates were noted. At each<br />
random po<strong>in</strong>t a diver swam around for about five or ten m<strong>in</strong>utes and noted down observations such as<br />
bot tom character, visibility and the absence or presence of seagrass. If there was seagrass present, the<br />
estimated abundance and species was recorded. The <strong>in</strong>formation collected along with the satellite imagery<br />
was then used later to determ<strong>in</strong>e the position and number of transects at the sites and also was used <strong>in</strong> the<br />
classification of seagrass meadows.<br />
Imagery used<br />
The images used for the survey were IKONOS imagery. IKONOS is a satellite-based platform operated<br />
by Space Imag<strong>in</strong>g Inc. that captures digital images <strong>in</strong> four spectral bands as well as panchromatic images.<br />
The four spectral bands are Red, Green, Blue and Near Infrared. Resolution for the spectral bands is 4<br />
meters while the panchromatic band offers a resolution of 1 meter. The images were taken by the satellite<br />
<strong>in</strong> November of 2000. Ma<strong>in</strong>ly because of their availability and their high resolution, IKONOS imagery<br />
was used for this survey.<br />
When provided, the images were already ortho-rectified and projected us<strong>in</strong>g the Universal Trans Mercator<br />
(UTM) method with WGS84 datum. Therefore, preprocess<strong>in</strong>g of the images was very limited. The only<br />
process<strong>in</strong>g needed was to subset the images of the selected sites and the conversion of the coord<strong>in</strong>ate<br />
system from UTM WGS84 to Lat/Long WGS84.<br />
Transects<br />
There are a variety of techniques and methods that can be used for ground-truth<strong>in</strong>g. The techniques differ<br />
accord<strong>in</strong>g to the locality features, depth and mapp<strong>in</strong>g objectives. For this survey it was decided that a<br />
comb<strong>in</strong>ation of transects and po<strong>in</strong>ts for the shallow areas (5 meters or less) would be used and GPS<br />
track<strong>in</strong>g for deeper zones (greater than 6 meters).<br />
A total of six transects were used on Ngederrak reef. These transects ran from east to west across the<br />
entire extent of the reef with an approximate distance of 300 m between each. Deep-water surveys were<br />
also conducted us<strong>in</strong>g SCUBA and GPS track<strong>in</strong>g along the <strong>in</strong>ner channel and along the eastern and<br />
western end of the reef flat (Figure 10).<br />
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