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Reference Guide to Emerging
Technologies to Implement NEPA
Geographic Information
Systems and the
Global Positioning System FAQ
1.
What are geographic information systems (GIS)?
Geographic information systems (GIS) are defined as:
"computer systems capable of assembling, storing,
manipulating, and displaying geographically referenced
information." (ESRI). GIS store information about
the world as a collection of thematic layers that can
be linked together by geography.
Defining features of
GIS

For a complete introduction to GIS, please visit ESRI's
GIS Tutorial Web site, http://www.gis.com.
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2. What are the key features
of geographic information systems?
There are two defining features of GIS: the ability
to overlay spatial data and the ability to be changed
as new data becomes available.
The first key feature of GIS programs is the
capability to overlay multiple sets of databases into
a final map that graphically explains the relationships
between the data. Spatial data - points, boundaries,
and lines - comprise the base of the map and can be
supplemented with tabular data - tables linked to
the maps with further information - and image data,
such as that from satellites. This powerful and versatile
concept has proven invaluable for solving many real-world
problems, from recording details of planning applications
to modeling global atmospheric circulation.
The second key feature of GIS is that they
can be thought of as "dynamic maps" which
can be updated and altered as needed. These maps may
also be manipulated for scientific analyses and to
create models of different environments.
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3. What is the relationship between
remotely sensed data and geographic information systems
(GIS)?
Remote sensing data applications and geographic information
systems (GIS) have an established history of interdependency.
GIS provides a format to distribute of remote sensing
data and to create valuable information from the data.
Remotely sensed data is also a critical means to create
base GIS maps and updating many data layers in a GIS.
The integration of remotely sensed data and GIS is particularly
attractive because 1) the conversion of remotely sensed
raster-format data to GIS vector-format data is inexpensive
and 2) remote sensing data offers a cost-effective way
to visualize large geographic areas in a digital format.
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4. What is the Global Positioning
System (GPS)?
The United States' Global Positioning System (GPS)
is "an all weather, worldwide, continuous coverage,
satellite-based, radio navigation system." The
GPS can be described as operating in three segments:
Space, Ground Control, and Users.
Space Segment: The Space segment consists
of 24 satellites, uniformly distributed in orbit around
the Earth. The satellites are divided into 6 orbital
planes, and a user located anywhere on the globe has
access to at least four satellites all the time, which
is the number needed for accurate positioning.
Ground Control Segment: The ground control
segment is comprised of one master control station,
six monitoring stations, and four ground antennas.
The stations determine the orbital mode and clock
correction parameters for each satellite and relay
this information to the ground antennas for transmission
to the satellites for broadcast to the users in real-time
or store the information to be entered as a data layer
into a GIS.
Users Segment: The users are antennas and receivers
that measure and decode the satellite transmission
to provide positioning, velocity, and precise timing
in real-time. The receivers can be handheld, personal
data devices. Many receivers are capable of data collection
and maintenance, and in the field, would be supported
by a GPS antennae carried in a backpack. Data collected
with machines such as this one can be easily transferred
into a GIS for further data processing.
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5. How does the GPS collect information?
GPS receivers work via a process called "triangulation."
Triangulation involves a receiver computing distances
by measuring the travel time of signals from multiple
satellites. The satellites are very carefully timed
using atomic clocks timed to thousandths of a second,
because a timing error of one-thousandth of a second
would set the measurement off by nearly 200 miles. Three
satellites are used to accurately triangulate the distance,
and a fourth satellite is in orbit to correct for the
timing inaccuracy of the receivers.
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6. How accurate is GPS information?
GIS data that is collected and referenced using a GPS
receiver is subject to the error of the GPS satellites.
Currently, an average GPS receiver has an "autonomous
accuracy" range of +/- 5-10 meters depending on
the sensor quality, the environment in which the recording
was taken, and the latitude at which the recording was
taken. The errors affecting a receiver with autonomous
accuracy are: distortions of the signal by the atmosphere,
distortions of the signal by ground interference, error
caused by gravitational pull, timing errors from the
atomic clocks aboard the satellites, and basic geometric
error stemming from the receiver. Scientists using a
receiver with Differential GPS (DGPS) capabilities can
have real-time accuracies in the +/- 1-5 meter range,
and even in the sub-meter and sub-centimeter accuracy
range depending on the quality of the receiver.
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The
materials on this Web site were developed by Ken Markowitz
as part of a presentation at the ALI-ABA
Course of Study: Environmental Impact Assessment: NEPA
(National Environmental Policy Act) and Related Requirements,
December, 2001, Washington, DC.
© 2002 Earthpace
LLC and ELIS. All rights reserved. Not for reproduction
without the express written approval from Earthpace, LLC
and ELIS. |