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Laser mapping uses a pulsed laser ranging system mounted onboard an aircraft to measure ground
elevation and topography. The laser emits laser beams at high frequency and is directed downward at the
earth's surface through a port 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 aircraft travels over the beach at approximately 60 meters per second while surveying from
the low water line to the landward base of the sand dunes.

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            <gco:CharacterString>Use Constraints: This data was collected for the purposes of research. Any conclusions drawn from analysis of this information
are not the responsibility of NOAA or the Office for Coastal Management. This data is likely to contain returns
from the water surface and vegetation. No processing has been done to remove returns from water or vegetation.
Users should be aware that temporal changes may have occurred since this data set was collected and some parts
of this data may no longer represent actual surface conditions. Users should not use this data for critical
applications without a full awareness of its limitations.</gco:CharacterString>
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            <gco:CharacterString>Distribution Liability: This data was collected for the purposes of research. Any conclusions drawn from analysis of this information are not the responsibility
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                    <gmd:CI_Contact>
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                        <gmd:CI_OnlineResource>
                          <gmd:linkage>
                            <gmd:URL>https://www.fisheries.noaa.gov/inportserve/waf/noaa/nos/ocm/dmp/pdf/48149.pdf</gmd:URL>
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              <gmd:westBoundLongitude>
                <gco:Decimal>-121.688571</gco:Decimal>
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                <gco:Decimal>-121.014281</gco:Decimal>
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                <gml:TimePeriod gml:id="boundingTemporalExtent-1-1">
                  <gml:description>| Currentness: Ground Condition</gml:description>
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                </gml:TimePeriod>
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Sciences Branch (OSB) of NASA at the Wallops Flight Facility in Virginia. The instrument, originally designed for mapping ice sheets
in Greenland, is called the Airborne Topographic Mapper or ATM. The ATM II (the latest version), operates with a Spectra Physics
laser transmitter, which provides a 7 nanoseconds long, 250 microjoules pulse at a frequency-doubled wavelength of 523 nanometers
in the blue-green spectral region. The laser transmitter can function  at pulse rates from 2 to 10 kilohertz (kHz). The laser system
with a separate cooling unit weighs approximately 45 kilograms (kg) and requires approximately 15 amperes of power at 115 volts.
The transmitted laser pulse is reflected to the surface of the earth with the aid of a small folding mirror mounted on the back of a
secondary mirror of a rotating scan mirror assembly mounted directly in front of the telescope. The scan mirror, which is rotated at 20
hertz, is comprised of a section of round aluminum stock, machined to a specific off-nadir angle. A scan mirror with the off-nadir
angle of 15 degrees was utilized, producing an elliptical scan pattern with a swath width equal to 50 percent of the approximately
700-meter aircraft altitude. The reflected laser pulse is transmitted to a photo-multiplier assembly that consists of a lens, a
narrow bandpass filter, and a single photomultiplier tube.
Note:  The Spatial Reference section of this document may lack fully FGDC-compliant information regarding projection parameters
(i.e., Central meridian, false Northing, etc.). The State Plane or UTM Zone will be supplied, and the corresponding parameters can be
found in Appendix C of: Snyder, John, 1987, Map Projections, a Working Manual (U.S. Geological Survey Professional Paper 1395):
Washington, U.S. Government Printing Office.</gco:CharacterString>
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            <gco:CharacterString>The ATM LIDAR elevation measurements have been found to be within +/- 15 centimeters of each other in successive and overlapping
passes of the same area. In comparisons of LIDAR data for a small geographic region with various ground surveys the differences
are between +/- 15 to 20 centimeters. The accuracy of the majority of the data is estimated to be consistent with the above
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                <gco:CharacterString>The vertical values in this data set have been filtered through visual inspection to find abnormally high and abnormally low values.
In addition, this data was processed using a spatial filtering program that identifies and discards outlier elevation measurements.
This program reads each elevation measurement within a file and identifies "spatially close" points (i.e. those neighboring points
within a fixed radius of the point). The mean and standard deviation is calculated using the elevations of these points. If the
elevation difference from the mean of the point under consideration is more than 2 standard deviations and greater than a defined
distance the point is discarded.</gco:CharacterString>
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          <gmd:source>
            <gmd:LI_Source>
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                <gmd:CI_Citation>
                  <gmd:title>
                    <gco:CharacterString>Qfit lidar data</gco:CharacterString>
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    </gmd:DQ_DataQuality>
  </gmd:dataQualityInfo>
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