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<metadata><idinfo><citation><citeinfo><title>EAARL Coastal Topography - Northern Gulf of Mexico, 2007: Bare Earth</title><geoform>XYZ</geoform><pubdate>2008</pubdate><serinfo><sername>Data Series</sername><issue>400</issue></serinfo><pubinfo><pubplace>Saint Petersburg</pubplace><publish>U.S. Geological Survey</publish></pubinfo><origin>U.S. Geological Survey</origin><ftname Sync="TRUE"/><pubtime>Unknown</pubtime><edition>first</edition></citeinfo></citation><descript><abstract>A bare earth elevation map (also known as a Digital Elevation Model, or DEM) of the northern Gulf of Mexico barrier islands and Naval Live Oaks was produced from remotely sensed, geographically referenced elevation measurements cooperatively by the U.S. Geological Survey (USGS), the National Park Service (NPS), and the National Aeronautics and Space Administration (NASA). Elevation measurements were collected over the area using the NASA Experimental Advanced Airborne Research Lidar (EAARL), a pulsed-laser ranging system mounted onboard an aircraft to measure ground elevation, vegetation canopy, and coastal topography. The system uses high-frequency laser beams 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 plane travels over the target area at approximately 50 meters per second at an elevation of approximately 300 meters. The EAARL, developed by NASA at Wallops Flight Facility in Virginia, measures ground elevation with a vertical resolution of 15 centimeters. A sampling rate of 3 kilohertz or higher results in an extremely dense spatial elevation dataset. Over 100 kilometers of coastline can be surveyed easily within a 3- to 4-hour mission. When subsequent elevation maps for an area are analyzed, they provide managers with a useful tool to make management decisions regarding land development.</abstract><purpose>The purpose of this project was to produce a highly detailed and accurate bare earth digital elevation map of the northern Gulf of Mexico barrier islands for use as a management tool and to make these data available to natural resource managers and research scientists.</purpose><supplinf>Unprocessed Lidar data are not in a format that is generally usable by resource managers and scientists. Converting dense Lidar elevation data into a readily usable format without loss of essential information requires specialized processing. The U.S. Geological Survey's Coastal and Marine Geology (CMG) Program has developed custom software to convert unprocessed Lidar data into a GIS-compatible map product to be provided to GIS specialists, managers, and scientists. The primary tool used in the conversion process is Advanced Lidar Processing System (ALPS), a multi-tiered processing system developed by a USGS-NASA collaborative project. Specialized processing algorithms are used to convert unprocessed waveform Lidar data acquired by the EAARL to georeferenced spot (x,y,z) returns for "bare earth" topography. These data are then converted to the North American Datum of 1983 and the North American Vertical Datum of 1988 (using the GEOID 03 model).  The files are in the Quarter-Quad tiling format and are named after the U.S. Geological Survey Alpha Quarter-Quad naming convention ('QQ_naming_convention.doc'). The development of custom software for creating these data products has been supported by the U.S. Geological Survey CMG Program's Decision Support for Coastal Parks, Sanctuaries, and Preserves project. Processed data products are used by the U.S. Geological Survey CMG Program's National Assessments of Coastal Change Hazards project to quantify the vulnerability of shorelines to coastal change hazards such as severe storms, sea-level rise, and shoreline erosion and retreat.</supplinf><langdata Sync="TRUE">en</langdata></descript><timeperd><timeinfo><rngdates><begdate>20070627</begdate><enddate>20070630</enddate></rngdates></timeinfo><current>ground condition</current></timeperd><status><progress>Complete</progress><update>None planned</update></status><spdom><bounding><westbc>421832.119252527</westbc><eastbc>415765.741460796</eastbc><northbc>3346811.74239591</northbc><southbc>3339841.04619841</southbc></bounding><lboundng><leftbc Sync="TRUE">421832.119252527</leftbc><rightbc Sync="TRUE">415765.741460796</rightbc><bottombc Sync="TRUE">3339841.04619841</bottombc><topbc Sync="TRUE">3346811.74239591</topbc></lboundng></spdom><keywords><theme><themekey>Lidar</themekey><themekey>Experimental Advanced Airborne Research Lidar</themekey><themekey>EAARL</themekey><themekey>Digital Elevation Model</themekey><themekey>elevation change</themekey><themekey>laser altimetry</themekey><themekey>derived surface</themekey><themekey>resource management</themekey><themekey>ALPS</themekey><themekey>Advanced Lidar Processing System</themekey><themekey>Hurricanes</themekey><themekt>http://remotesensing.usgs.gov/</themekt></theme><place><placekey>Florida</placekey><placekey>Mississippi</placekey><placekey>Alabama</placekey><placekt>http://nationalmap.gov/</placekt><placekey>Gulf of Mexico</placekey><placekey>Cat Island</placekey><placekey>Petit Bois Island</placekey><placekey>Dauphin Island</placekey><placekey>Chandeleur Islands</placekey><placekey>Horn Island</placekey><placekey>Ship Island</placekey><placekey>Santa Rosa Island</placekey><placekey>Perdido Key</placekey><placekey>Naval Live Oaks</placekey></place><stratum><stratkey>Bare earth</stratkey><stratkt>http://lidar.cr.usgs.gov/</stratkt></stratum><temporal><tempkey>2007</tempkey><tempkt>http://www.esri.com/news/arcuser/1104/temporal.html</tempkt></temporal></keywords><useconst>Although the U.S. Geological Survey is making these datasets available to others who may find the data of value, the The U.S. Geological Survey, National Park Service, and National Aeronautical and Space Administration request the be acknowledged as originators of this data in future products or derivative research.</useconst><ptcontac><cntinfo><cntorgp><cntorg>Jacobs Technology, contracted to USGS</cntorg><cntper>Amar Nayegandhi  or  John Brock at USGS</cntper></cntorgp><cntpos>Computer Scientist</cntpos><cntaddr><addrtype>mailing and physical address</addrtype><address>600 4th Street South</address><city>Saint Petersburg</city><state>FL</state><postal>33701</postal><country>USA</country></cntaddr><cntvoice>727-803-8747 x3026</cntvoice><cntemail>anayegandhi@usgs.gov</cntemail><hours>M-F 8:30-5:00 EST</hours><cntemail>jbrock@usgs.gov</cntemail></cntinfo></ptcontac><datacred>Acknowledgement of the U.S. Geological Survey, Florida Integrated Science Center, as a data source would be appreciated in products developed from these data, and such acknowledgement as is standard 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 the U.S. Geological Survey staff. Users should be aware that comparisons with other datasets for the same area from other time periods may be inaccurate due to inconsistencies resulting from changes in photointerpretation, mapping conventions, and digital processes over time. These data are not legal documents and are not to be used as such.</datacred><native>Microsoft Windows XP Version 5.1 (Build 2600) Service Pack 2; ESRI ArcMap 9.2.2.1350</native><crossref><citeinfo><pubdate>In Press</pubdate><title>Small footprint, waveform-resolving lidar estimation of submerged and subcanopy topography in coastal environments</title><serinfo><sername>International Journal of Remote Sensing</sername></serinfo><origin>Nayegandhi, A., Brock, J.C., Wright, C.W</origin><pubinfo><publish>Taylor and Francis</publish><pubplace>London</pubplace></pubinfo></citeinfo></crossref><crossref><citeinfo><pubdate>2002</pubdate><title>Basis and methods of NASA Airborne Topographic Mapper lidar surveys for coastal studies</title><edition>18(1), p. 1-13</edition><serinfo><sername>Journal of Coastal Research</sername><issue>18(1), p. 1-13</issue></serinfo><origin>Brock, J.C., Wright, C.W., Sallenger, A.H., Krabill, W.B., and Swift, R.N.</origin><pubinfo><publish>Coastal Research and Education Foundation, Inc.</publish></pubinfo></citeinfo></crossref><crossref><citeinfo><origin>Sallenger, A.H., Wright, C.W., and Lillycrop, J.</origin><pubdate>2005</pubdate><title>Coastal impacts of the 2004 hurricanes measured with airborne lidar; initial results</title><edition>73(2-3), p. 10-14</edition><serinfo><sername>Shore and Beach</sername><issue>73(2-3), p. 10-14</issue></serinfo></citeinfo></crossref><natvform>XYZ</natvform><secinfo><secclass>Unclassified</secclass><secsys>unclassified</secsys><sechandl>none</sechandl></secinfo></idinfo><dataqual><attracc><attraccr>The expected accuracy of the measured variables are as follows: attitude within 0.07 degree, 3 cm nominal laser ranging accuracy, and vertical elevation accuracy of +/-15 cm for the topographic surface. Quality checks are built into the data-processing software.</attraccr></attracc><posacc><horizpa><horizpar>Unprocessed elevation measurements have been determined to be within 1 meter horizontal accuracy.</horizpar></horizpa><vertacc><vertaccr>Elevations of the DEM are vertically consistent with the point elevation data, +/-15 cm.</vertaccr></vertacc></posacc><lineage><srcinfo><srctime><timeinfo><rngdates><begdate>20070627</begdate><enddate>20070630</enddate></rngdates></timeinfo><srccurr>ground condition</srccurr></srctime><srccite><citeinfo><origin>U.S. Geoloigcal Survey</origin><pubdate>2008</pubdate><serinfo><sername>Data Series</sername><issue>400</issue></serinfo><pubinfo><pubplace>FISC St. Petersburg</pubplace><publish>U.S. Geological Survey</publish></pubinfo><title>EAARL Coastal Topography-Northern Gulf of Mexico, 2007: Bare Earth</title><geoform>remote-sensing image</geoform><pubtime>Unknown</pubtime><edition>first</edition></citeinfo></srccite><typesrc>Point elevation measurements collected by the EAARL sensor.</typesrc><srcscale>1</srcscale><srccitea>none</srccitea><srccontr>unknown</srccontr></srcinfo><procstep><procdesc>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 (532 nm) 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 U.S. Geological Survey office in St. Petersburg and the NASA office at Wallops Flight Facility. The navigational data are processed at Wallops Flight Facility. The navigational and unprocessed data are then downloaded into the Advanced 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).</procdesc><procdate>20070627 - 20080805</procdate><proccont><cntinfo><cntaddr><addrtype>mailing and physical address</addrtype><address>600 4th Street South</address><city>Saint Petersburg</city><state>FL</state><postal>33703</postal><country>USA</country></cntaddr><cntvoice>727-803-8747 x3026</cntvoice><hours>M-F, 8:00-5:00 EST</hours><cntemail>anayegandhi@usgs.gov</cntemail><cntorgp><cntorg>Jacobs Technology, U. S. Geological Survey, FISC St. Petersburg</cntorg><cntper>Amar Nayegandhi</cntper></cntorgp><cntpos>Computer Scientist</cntpos></cntinfo></proccont></procstep></lineage><complete>Several regions of the dataset are labeled as "No Data", which corresponds to a cell value of -32767 m  in the XYZ 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.</complete><logic>Each file contains data located in USGS 24K Quarter Quadrangle tile and are named after the USGS Alpha Quarter Quad naming convention. AAOOOaoq, where AA is the positive whole number component of the  latitude. OOO is the positive whole number component of the longitude (zero-padded to a width of 3); a is an alpha character a-h designating which quad in the degree of latitude; where a is closest to 0 minutes and h is closest to the next full degree. Each represents 1/8 of a degree; o is a numeral 1-8 designating which quad in the degree of longitude, where 1 is closest to 0 minutes and 8 is closest to the next full degree. Each represents 1/8 of a degree; q is an alpha character a-d designating which quarter in the quad, where a is SE, b is NE, c is NW, and d is SW. Each quarter-quad is 1/16 of a degree in latitude and 1/16 of a degree in longitude.</logic></dataqual><spdoinfo><direct>Point</direct></spdoinfo><spref><horizsys><planar><planci><plance>row and column</plance><coordrep><absres>2.000000</absres><ordres>2.000000</ordres></coordrep><plandu>meters</plandu></planci><gridsys><gridsysn Sync="TRUE">Universal Transverse Mercator</gridsysn><utm><utmzone Sync="TRUE">16</utmzone><transmer><sfctrmer Sync="TRUE">0.999600</sfctrmer><longcm Sync="TRUE">-87.000000</longcm><latprjo Sync="TRUE">0.000000</latprjo><feast Sync="TRUE">500000.000000</feast><fnorth Sync="TRUE">0.000000</fnorth></transmer></utm></gridsys></planar><geodetic><horizdn>North American Datum of 1983</horizdn><ellips>Geodetic Reference System 80</ellips><semiaxis>6378137.000000</semiaxis><denflat>298.257222</denflat></geodetic><cordsysn><geogcsn>GCS_North_American_1983</geogcsn><projcsn>NAD_1983_UTM_Zone_16N</projcsn></cordsysn></horizsys><vertdef><altsys><altdatum>North American Vertical Datum of 1988</altdatum><altres>0.15 m</altres><altunits>meters</altunits><altenc>Explicit elevation coordinate included with horizontal coordinates</altenc></altsys></vertdef></spref><eainfo><overview><eadetcit>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). Z value is referenced to orthometric elevations derived from National Geodetic Survey Geoid Model, GEOID03.</eadetcit><dsoverv>This raster represents Lidar-derived elevations.</dsoverv><eaover>The XYZ ascii data is encoded with a 1-meter resolution.</eaover></overview></eainfo><distinfo><distrib><cntinfo><cntpos>Project Manager</cntpos><cntaddr><addrtype>mailing address</addrtype><address>600 4th Street South</address><city>Saint Petersburg</city><state>FL</state><postal>33701</postal><country>USA</country></cntaddr><cntvoice>727 803-8747</cntvoice><hours>M-F 8:30-5:00 EST</hours><cntorgp><cntorg>U.S. Geological Survey</cntorg><cntper>Project Manager</cntper></cntorgp></cntinfo></distrib><resdesc>DS 400</resdesc><distliab>This DVD publication was prepared by an agency of the United States Government. Although these data have been processed successfully on a computer system at the U.S. Geological Survey, no warranty expressed or implied is made regarding the display or utility of the data on any other system, nor shall the act of distribution imply any such warranty. The U.S. Geological Survey shall not be held liable for improper or incorrect use of the data described and (or) contained herein. Reference herin to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof.</distliab><stdorder><fees>vary</fees><ordering>contact U.S. Geological Survey</ordering><turnarnd>vary</turnarnd><digform><digtinfo><formname>XYZ</formname><formspec>XYZ</formspec><formvern>1.1</formvern></digtinfo><digtopt><offoptn><offmedia>DVD</offmedia><recfmt>DVD</recfmt></offoptn></digtopt></digform></stdorder><custom>Contact U.S. Geological Survey for Details</custom><availabl><timeinfo><sngdate><caldate>2008</caldate></sngdate></timeinfo></availabl></distinfo><metainfo><metd>20080307</metd><metc><cntinfo><cntorgp><cntorg>U. S. 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