11th ICRS Abstract book - Nova Southeastern University
11th ICRS Abstract book - Nova Southeastern University
11th ICRS Abstract book - Nova Southeastern University
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Poster Mini-Symposium 17: Emerging Techniques in Remote Sensing and Geospatial Analysis<br />
17.553<br />
GIS Derived Spatial Analysis as a Tool to Predict Nearshore Coral Reef Fish<br />
Species in American Samoa<br />
D. Paul BROWN* 1 , Gerald ALLEN 2<br />
1 National Park Service, Pago Pago, American Samoa, 2 Department of Aquatic Zoology,<br />
Western Australian Museum, Perth, Australia<br />
The U.S. National Park Service has undertaken a monumental task of inventorying<br />
species found within park boundaries both below water and on land. This is part of the<br />
Inventory & Monitoring program aimed to increase our management efforts in all the<br />
U.S. National Parks. In the National Park of American Samoa, the inventory of coral reef<br />
fish has helped to discover 44 new species records for the territory of American Samoa.<br />
This was done using both GIS polygons derived from known geographic distributions of<br />
marine fish as well as in-water surveys using SCUBA and technical diving procedures. A<br />
distribution map was created for all known coral reef fish species from the central South<br />
Pacific. Using ArcInfo GIS software, a point was generated on an equal area map of the<br />
South Pacific for each recorded occurrence of a given species. These point records,<br />
whether collection or observational records, were then used to create a GIS polygon.<br />
Although these polygons include broad expanses of deepsea/ pelagic habitat, it is<br />
assumed that fish species only occur in suitable habitat. When American Samoa fell<br />
inside this polygon, it was assumed that this species could be found. GIS benthic habitat<br />
maps were then used to locate suitable and likely locations for a given species. In-water<br />
surveys were then conducted to look for the assumed present species. Using this<br />
technique 118 additional species were presumed to be located in Am. Samoa. To date the<br />
in-water surveys have found 44 new records, of these, 27 were assumed present from the<br />
GIS modeling but had never previously been found. Many of the remaining species are<br />
small and cryptic and are unlikely to be encountered without the use of icthyocides.<br />
17.554<br />
Monitoring The Health Of Coral Reef Using Multi-Temporal Remote Sensing -A<br />
Case Study Of Pirotan Island, Marine National Park, Gulf Of Kachchh, Gujarat ,<br />
India<br />
Sahadev SHARMA* 1 , Anjali BAHUGUNA 2 , Nandini Ray CHAUDHARY 2 , Shailesh<br />
NAYAK 3 , Sachin CHAVAN 4 , Chavi Nath PANDEY 4<br />
1 <strong>University</strong> of the Ryukyus, Okinawa, Japan, Nishihara, Japan, 2 Space Applications<br />
Centre (ISRO) Ahmedabad, India, Ahmedabad, India, 3 Indian National Centre for Ocean<br />
Information Service, Hyderabad, India, hyderabad, India, 4 Gujarat Ecological Education<br />
and Research Foundation, Gandhinagar, India, Gandhinagar, India<br />
Multi-temporal coral reef study is required for monitoring the climate and human impact<br />
changes. We have evolved an indicator-based (mainly satellite-derivable indicators)<br />
approach for monitoring health of reefs. The indicators tell about the damage already<br />
done, current ecological condition and early warning to the reefs. Early warning<br />
indicators are Sea Surface Temperature Anomaly, Turbidity, and Delay in Onset of<br />
Algae. The ecological indicators are diversity (both floral, faunal and habitat), percentage<br />
cover of live and dead corals, etc., and the Damage indicators are the deposition of mud<br />
and sand on the reef, erosion, phase shift, etc. The health status for Pirotan reef (22.6 0 N,<br />
70 0 E) located in the Gulf of Kachchh, India, has been assessed using health indicators.<br />
Indicators of Pirotan Reef health are temperature rise, high salinity, increase in macroalgae,<br />
over-fishing, high sedimentation rate, human influences, and deposition of mud<br />
over reef, etc. Indian Remote Sensing Satellite LISS III sensor data of periods 1998, 2000<br />
and 2005 were analysed to zone the eco-morphological zones of the reef like algal ridge,<br />
mud over reef, sandy muddy reef flat, live coral zone, seagrass, macro-algae, algae on<br />
muddy reef flat, etc. with an accuracy of 87% at 90% confidence level. NOAA-AVHRR<br />
average monthly SST data was analyzed from 1998 to 2005 (March, April, May and<br />
June) to identify the effect of temperature rise on coral reef like bleaching and increased<br />
macro-algae cover. Depositions of sand and mud have increased owing to the high<br />
sedimentation rate, sand mining and cutting of mangroves. Coral bleaching and stress has<br />
resulted in increased macro-algal growth. Onset of coral reef friendly macro-alga<br />
(Sargassum) has shifted from September-October to early December. The Pirotan reef is<br />
under severe degradation as is apparent from the indicators of health. Efforts are currently<br />
underway to model the indicators for establishing health.<br />
17.555<br />
Coral Color - Reflection And Absorption<br />
Noga STAMBLER* 1<br />
1 Life Sciences, Bar Ilan <strong>University</strong>, Ramat Gan, Israel<br />
Light absorption per unit of coral surface area decreased with increase in colony size, with a<br />
clear effect of different coral morphologies. In branched colonies, shading among branches<br />
reduced the absorbed light per unit area and per zooxanthellae.<br />
Corals often have different colors; color is variable, even among colonies of the same species<br />
growing together. While the colors blue, pink, and green are due to the protein pigments in the<br />
host tissue, the brown color is due to the absorption of the zooxanthellae pigments.<br />
Coral colors change as a result of acclimation and adaptation to environmental conditions. Dark<br />
brown colors, representing higher absorption, are due to low-light intensities or exposure to<br />
high-nutrient concentration, while lightness colors are due to low pigment concentrations, in<br />
some cases due to natural conditions while others indicate stress conditions.<br />
The absorption range of the corals and their symbiotic zooxanthellae, and their ability to change<br />
their color by photo-acclimation and photoadaptation enable the coral to grow and survive.<br />
These variations can monitor on a reef level, however corals can exhibit different colors in the<br />
same colony. The spectral variation between color morphs of the hermatypic corals Stylophora<br />
pistillata and Pocillopora damicornis in the northern Red Sea was found to be higher than<br />
between species. Therefore species recognition based on reflectance spectra is only possible in<br />
certain cases.<br />
17.556<br />
Geomorphological Symbolization Of Coral Reef Environments Along The Southeast<br />
Coast Of Florida: Interpretation Of Airborne Laser Bathymetry And Development Of An<br />
Extension For Arcinfo GIS<br />
Jacob ESTEBANELL BECERRA 1 , Victoria ACHATZ 2 , Charles FINKL* 3<br />
1 Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain, 2 School of Geoinformation,<br />
<strong>University</strong> of Applied Sciences Villach, Villach, Austria, 3 Coastal Geology & Geomatics,<br />
Coastal Planning & Engineering, Boca Raton, FL<br />
Interpretation of laser airborne depth sounding (LADS) imagery along the SE Florida coast<br />
initially identified numerous coral reef environments that were displayed as discrete polygons<br />
on maps. Although this recognition of morphoforms provided a comprehensive overview of<br />
spatial differentiation and interrelationships between reef subsystems, the topology lacked clear<br />
integration of form with function and morphodynamic processes. In an effort to glean more<br />
information from the LADS imagery that would better reflect the detailed distribution of<br />
morphoforms, we amalgamated symbolization as recommended in manuals for meso- and<br />
microscale geomorphological mapping as seen in the Geomorphological Map of Europe. The<br />
procedure involved detailed subdivision of mapping units already derived for the 600 km2<br />
study area by interpretation of morphoforms and onscreen digitizing using symbols specifically<br />
created for this purpose. The characterization of coral reef environments involved classification<br />
of different geomorphic forms and processes followed by the creation of index forms for maps.<br />
After adapting existing landscape symbols to seafloor forms and adding new symbols, hand<br />
drawn maps including all patterns (point, line, polygon) were prepared as overlays to the LADS<br />
imagery. Polygon and point patterns were digitized in a graphics drawing program while line<br />
patterns were created in the ArcGIS Style Manager. After importing geomorphic symbols into<br />
the ArcGIS Library, shape and color patterns were adjusted for final digitalization of the<br />
geomorphic map with a self programmed extension for ArcGIS. The result produced maps<br />
showing coral reef environments displayed in terms of true geomorphic symbolization.<br />
402