United States Geological Survey Center for Coastal and Watershed Studies 2005 First remote-sensing image EAARL Lidar Submarine Topographic Maps The USGS, in cooperation with the National Park Service (NPS) and the National Aeronautics and Space Administration (NASA), provide the coastal management community with digital elevation products. The USGS processes aircraft lidar data provided by NASA, develops software tools and algorithms to use and analyze the data, and makes products available to the coastal management community. \\BISC77823-HQ-SP\LIDAR\DRTO\LIDAR\e304n2722\e304n2722edit.tif e304n2722edit.tif Lidar is a remote sensing technique that uses laser light to detect, range, or identify remote objects based on light reflected by the object or emitted through it subsequent fluorescence. Airborne ranging lidar is now being applied in coastal environments to produce accurate, cost-efficient elevation datasets with high data density. The USGS in cooperation with NASA and NPS is using airborne lidar to measure the submerged topography of the Dry Tortugas reef tract and Subaerail topography of land features; secondarily, the data will be assessed for its potential in terms of benthic characterization. Elevation measurements were collected over Dry Tortugas National Park using the NASA Experimental Advanced Airborne Research Lidar (EAARL), a pulsed laser ranging system mounted onboard an aircraft to measure subaerial and submarine coastal topography. With the NASA EAARL lidar system, submarine data is generally acquired to a maximum of approximately 1.5 secchi depths (a measure of water clarity). The system uses a high frequency laser beam directed at the earth's surface through an opening in the bottom of the aircraft's fuselage. The laser system records the time difference between emission of the laser beam and the reception of the reflected laser signal in the aircraft. The Experimental Advanced Airborne Research Lidar, developed by the National Aeronautics and Space Administration (NASA) Wallops Flight Facility (WFF) in Virginia, measures ground elevation with a vertical resolution of roughly 15 centimeters. A sampling rate of up to 3 kHz results in an extremely dense spatial elevation data set. One objective of this research is the creation of techniques for the surveying of coral reefs for the purposes of habitat mapping, ecological monitoring, change detection, and event assessment (e.g., bleaching, hurricanes, disease outbreaks, etc.). As part of this project, data from an innovative instrument developed at NASA Wallops Flight Facility, the NASA Experimental Airborne Advanced Research Lidar (EAARL), was used. This sensor has the potential to make significant contributions in this realm for measuring water depth and conducting cross-environment surveys. High spectral resolution, water-column correction, and low costs were found to be key factors in providing accurate and affordable imagery to managers of coastal tropical habitats. Raw lidar data is not in a format that is generally usable by Park Service resource managers and scientists for scientific analysis. Converting dense lidar elevation data into a readily usable format without loss of essential information requires specialized processing. The USGS converts raw lidar data into a GIS-compatible map product to be provided to National Park Service GIS specialists, managers, and scientists. The primary tool used in the conversion process is Airborne Lidar Processing System (ALPS), a multi-tiered processing system developed by a USGS/NASA collaborative project for the use of subaerial and submarine lidar in coastal change assessment. Specialized processing algorithms are used to convert raw waveform lidar data acquired by the EAARL to georeferenced spot (x,y,z) returns for submarine topography. These data are then converted to the NAD83 horizontal and NAVD88 vertical datum (using the Geoid 99 model). The final products are 2x2-km map tiles written out in a standard geotiff format with associated metadata information. These tiles are created for visual interpretation and regional quantitative analysis. Metadata files include the standard FGDC format. en 073104,080104,080304,080404,080504,080804,080904 ground condition Complete Unknown -82.935852 -82.915832 24.599926 24.581620 304001.000000306001.0000002720000.0000002722000.000000 None LIDAR Experimental Advanced Airborne Research Lidar digital elevation model elevation change laser altimetry derived surface coastal resource management submerged topography Airborne Lidar Processing System benthic cover types bare earth elevations None Dry Tortugas National Park Atlantic Coast Florida United States East Coast Florida Reef Tract Coastal Florida Fort Jefferson Any use of these data signifies a user's agreement to comprehension and compliance of the USGS Standard Disclaimer. Ensure all portions of metadata are read and clearly understood before using these data in order to protect both user and USGS interests. See section 6.3 Distribution Liability. Although the USGS is making these data sets available to others who may find the data of value, USGS does not warrant, endorse, or recommend the use of thes data for any given purpose. The user assumes the entire risk related to the use of these data. These data sets are not for navigational purposes. USGS is providing these data "as is", and USGS disclaims any and all warranties, whether expressed or implied, including (without limitation) any implied warranties of merchantability or fitness for a particular purpose. In no event will USGS be liable to you or to any third party for any direct, indirect, incidental, consequential, special, or exemplary damages or lost profits resulting from any use or misuse of these data. Acknowledgement of the U.S. Geological Survey Center for Coastal and Watershed Studies as a data source would be appreciated in products developed from these data, and such acknowledgement as is standad for citation and legal practices for data source is expected by users of this data. Sharing new data layers developed directly from these data would also be appreciated by USGS staff. Users should be aware that comparisons with other data sets for the same area from other time periods may be inaccurate due to inconsistencies resulting from changes in photo interpretation, mapping conventions, and digital processes over time. These data are not legal documents and are not to be used as such. United States Geological Survey, Center for Coastal and Watershed Studies Dr. John C. Brock Research Oceanographer mailing and physical address

600 4th Street South

St. Petersburg Florida 33701- USA 727 803-8747 ext3088 727 803-2031 jbrock@usgs.gov Monday-Friday, 8-5, EST e298n2722.tif gridplot tiff image TIFF The USGS Center for Coastal and Watershed Studies would like to acknowledge NASA Goddard Space Flight Center for their cooperation and assistance in the development of the data. The USGS would also like to acknowledge Park Management and personnel at Dry Tortugas National Park. The National Park Service also contributed by editing the lidar tiles to remove processing artifacts. Microsoft Windows 2000 Version 5.0 (Build 2195) Service Pack 4; ESRI ArcCatalog 8.3.0.800 Brock, J.C.; Wright, C.W.; Sallenger, A.H; Krabill, W.B., and Swift, R.N 2003 journal article West Palm Beach, FL Journal of Coastal Research Wright, C.W. and J. Brock 2002 20-22, May 2002 proceedings article Miami Proceedings of the Seventh International Conterence on Remote Sensing for Marine and Coastal Environments John Brock and Asbury Sallenger, US Geological Survey 2001 USGS Open File Report St. Petersburg, FL US Geological Survey Raster Dataset The expected accuracy of the measured variables are as follows: attitude within 0.07 degree, 3-cm nominal ranging accuracy, and vertical elevation accuracy of +/-20 cm for the "first return" surface. Quality checks are built into the data-processing software. Raw elevation measurements have been determined to be within 1 meter horizontal accuracy. Processing steps (grid interpolation) may introduce additional error which has not been tested at the time of this publication. 1 Elevations of the DEM are vertically consistent with the point elevation data, +/-20 cm. .20 NASA Collected the EAARL Lidar data and distributed to USGS for processing raster digital data Point elevation measurements collected by the EAARL sensor. 073104,080104,080304,080404,080504,080804,080904 ground condition The data are collected using a Cessna 310 aircraft. The NASA Experimental Advanced Airborne Research Lidar (EAARL) laser scanner collects the data using a green (532nm) raster scanning laser, while a digital camera acquires a visual record of the flight. The data are stored on hard drives and archived at the USGS office in St. Petersburg and the NASA office at Wallops Flight Facility. The navigational data are processed at Wallops Flight Facility. The navigational and raw data are then downloaded into the Airborne Lidar Processing System (ALPS). Data are converted from units of time to x,y,z points for elevation. The derived surface data can then be converted into raster data (geotiffs).United States Geological Survey Center for Coastal and Watershed StudiesAmar NayegandhiComputer Scientistmailing and physical address

600 4th Street South

St. PetersburgFlorida33701USA727-803-87478:00am to 5:00pm Monday thru Friday, ESTCall Survey for Details2004

18001 Old Cutler Road

mailing and physical address

Suite 419

MiamiFlorida33157National Park Service South Florida / Caribbean Network Inventory and Monitoring ProgramJudd PattersonResearch Assistant(305) 252-0347(305) 253-0463The raster dataset was opened in ERDAS IMAGINE for editing. An Area of Interest (AOI) polygon was drawn around regions of poor data quality. Poor data quality was determined visually by locating gaps in the data as well as artifacts of the lidar processing. Pixels within the AOI polygons were given a raster value of -100 to correspond with other areas of No Data.January - March 2006ESRI ArcGIS 8.3Metadata imported.C:\LIDAR\DRTO\LIDAR\e298n2722\e298n2722edit.tif.xml2006031515300600 Several regions of the dataset are labeled as "No Data", which corresponds to a cell value of -100 m in the GeoTiff file. These "No Data" areas are a result of the survey not covering a particular region, optical water depth of greater than 1.5 Secchi disc depths, or the manual removal of lidar processing artifacts. Raster Pixel 2000 2000 1 1.0000001.00000032Upper LeftFALSENone1pixel RGBTRUETIFFmetermeterlidar dem row and column 1.000000 1.000000 meters Universal Transverse Mercator170.999600-81.0000000.000000500000.0000000.000000 North American Datum of 1983 Geodetic Reference System 80 6378137.000000 298.257222 GCS_North_American_1983NAD_1983_UTM_Zone_17N North American Vertical Datum of 1988 .01 meters Explicit elevation coordinate included with horizontal coordinates North American Vertical Datum of 1988 .01 meters Explicit elevation coordinate included with horizontal coordinates This Digital Elevation Model is an Geotiff derived from point data. It is raster data consisting of cells. Each cell has an elevation value associated with it. Cell size is 1 meter by 1 meter. This Digital Elevation Model is an Geotiff derived from point data referenced to WGS84, NAD83 UTM eastings and northings (m). The variables measured by EAARL are: distance between aircraft and GPS satellites (m), attitude information (roll, pitch, heading in degrees), scan angle (degrees), second of the epoch (sec), and 1-ns time-resolved return intensity waveform (digital counts). It is raster data consisting of cells. Each cell has an elevation value associated with it. Cell size is 1 meter by 1 meter. This raster represents lidar-derived elevations. United States Geological Survey Jerry Butcher Windows System Administrator mailing address

600 4th Street South

St. Petersburg FL 33701 USA 727-803-8747 ext3049 Lidar DEM (date - identifier) The United States Geological Survey shall not be held liable for improper or incorrect use of the data described and/or contained herein. These data and related graphics are not legal documents and are not intended to be used as such. The information contained in these data is dynamic and may change over time. The data are not better than the original sources from which they were derived. It is the responsibility of the data user to use the data appropriately and consistent within the limitations of geospatial data in general and these data in particular. The related graphics are intended to aid the data user in acquiring relevant data; it is not appropriate to use the related graphics as data. The United States Geological Survey gives no warranty, expressed or implied, as to the accuracy, reliability, or completeness of these data. It is strongly recommended that these data are directly acquired from an USGS server and not indirectly through other sources which may have changed the data in some way. Although these data have been processed successfully on a computer system at the United States Geological Survey, no warranty expressed or implied is made regarding the utility of the data on another system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty. This disclaimer applies both to individual use of the data and aggregate use with other data. TIFF15.29115.291DVD-ROMCall USGS for Details Call USGS for Details 20060315 United States Geological Survey mailing and physical address

600 4th Street South

St. Petersburg Floirda 33704 USA 727-803-8747 Call Survey for Details FGDC Content Standards for Digital Geospatial Metadata FGDC-STD-001-1998 local time enhttp://www.esri.com/metadata/esriprof80.htmlESRI Metadata Profile 2006031515300600FALSE20060315153007002006031515300700FALSE{68E1206F-648C-4BFC-92CB-705D5C050143}Microsoft Windows 2000 Version 5.0 (Build 2195) Service Pack 4; ESRI ArcCatalog 8.3.0.800e304n2722edit.tif304001306001272200027200001-82.935852-82.91583224.59992624.581621ISO 19115 Geographic Information - MetadataDIS_ESRI1.0dataset002file://\\BISC77823-HQ-SP\LIDAR\DRTO\LIDAR\e304n2722\e304n2722edit.tifLocal Area Network15.291Raster DatasetNAD_1983_UTM_Zone_17N22000120001120060315