Geodesy and Datums

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Geodesy and Datums

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In areas far away from the shore, mean sea level is determined by the shape of the geoid. ... Difference between Elipsoid, Geoid and Topgrapahic Surfaces ... – PowerPoint PPT presentation

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Title: Geodesy and Datums


1
Geodesy and Datums
  • Michael A. McAdamsGeography Dept.Fatih
    UniversityIstanbul, Turkey

2
Is the earth round?
  • Well...all the globes are round..so it must be...
  • It must be flat because..I have never seen the
    earth curve
  • It is not flat, but more like an elispse
  • It depends on what you mean by round. It is a
    sphere, but not a perfect one.

3
A View from Space (Google Earth)
4
Another view of the earth
Türkiye
5
Istanbul from Space(looks flat, but is it??)
You are here
6
Fatih University
You are here
7
Another image of Istanbul (infra-red)
8
Some questions?
  • Geodesy is the science of measuring and
    monitoring the size and shape of the Earth and
    the location of points on its surface. (NOAA
    website http//www.oceanservice.noaa.gov/educati
    on/kits/geodesy/welcome.html )
  • Why is it used?
  • To obtain accurate measures on the surface of
    the earth
  • Who uses it?
  • Surveyers, remote sensing specialists, GIS
    technicians, geographers, archeologists, anyone
    concerned with spatial analysis
  • What is the difference between a geod and a
    datum?
  • A datum is the specifications to construct a
    geod or at least a part of one

9
The Elements of Geodesy The Figure of the Earth
  • The Earth's shape is nearly spherical, with a
    radius of about 3,963 miles (6,378 km), and its
    surface is very irregular.
  • Mountains and valleys make actually measuring
    this surface impossible because an infinite
    amount of data would be needed.
  • It would take you many lifetimes to measure every
    crevice, valley, and rise. You could never
    complete the project because it would take too
    long.
  • http//www.oceanservice.noaa.gov/education/kits/ge
    odesy/geo03_figure.html

10
A Round Earth...not a new idea
  • In 6th Century B.C.E. Pythagoras stated that
    people must live on a body of perfect shape
  • Aristotle (4th Century B.C.E.) noted that sailing
    ships disappear from view hull first and then
    mast instead of getting smaller and smaller
  • Astronomical observation also evident of the
    circular appearence of the earth
  • Eratosthenes (librarian at the library at
    Alexandria) calculated a slightly larger
    circumference of the earth in 250 B.C.E.see
    Figure 4.1 in textbook

11
Members of a 1922 geodetic survey expedition.
Until recent advances in satellite technology,
namely the creation of the Global Positioning
System (GPS), geodetic surveying was an arduous
task best suited to individuals with strong
constitutions, and a sense of adventure.
12
Elipsoid and Geod
  • An elipsoid is probably the most similar to the
    earths surface..but not exactly
  • Various types of official elipsoids (see Table
    4.2)most widely used is the WGS84
  • A geod is the three-dimenisonal shape that would
    be approximated by mean sea level in the oceans
    and the surface of a series of hypothetical
    sea-level canals crisscrossing the continents.
    (Robinson, 44)

13
Different Abstractions of the Earth
  • http//www.oceanservice.noaa.gov/education/kits/ge
    odesy/media/supp_geo03a.html

14
Simple Explainations of the Abstractions of the
Earths surface
  • Flat Earth (planar)A flat earth without
    accounting for the curvature of the earth. This
    is used for surveying and small areas.
  • SphereSimular to a ball or what we think of as a
    globe. It discounts the irregularities in the
    earths surface such as mountaing ranges and
    canyons
  • ElipsoidLooks like an egg. The earth is more
    like an elipsoid than a sphere so it is more
    accurate than a sphere.
  • GeodBased on the elevation and earths
    gravatational pull. It is the most accurate
    description of the surface of the earth.

15
What is a datum?
  • A datum is as a set of spatial information that
    acts as a foundation for other data, just like
    concrete acts as a foundation for the structure
    of a building, including all the furnishings and
    decorations inside.
  • In other words, it is the necessary information
    (data or datum) that can re-create a plane,
    sphere, elipsoid or geod.
  • Without a datum there would be nothing to
    securely support other spatial information, such
    as digital elevations, land use, or population.
  • There are two types of datums, horizontal and
    vertical
  • More on datums at http//www.colorado.edu/geograp
    hy/gcraft/notes/datum/datum_f.html

16
Horizonal and Vertical datums
  • the horizontal datum is a collection of specific
    points on the Earth that have been identified
    according to their precise northerly or southerly
    location (latitude) and easterly or westerly
    location (longitude).
  • The vertical datum is a collection of specific
    points on the Earth with known heights either
    above or below mean sea level. Near coastal
    areas, mean sea level is determined with a tide
    gauge. In areas far away from the shore, mean sea
    level is determined by the shape of the geoid.

http//www.oceanservice.noaa.gov/education/kits/ge
odesy/
17
Difference between Elipsoid, Geoid and
Topgrapahic Surfaces
18
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19
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20
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21
Global Positioning System (GPS)
  • Using the Global Positioning System (GPS), every
    point on Earth can be given its own unique
    address -- its latitude, longitude, and height.
    The U.S. Department of Defense developed GPS
    satellites as a strategic system in 1978. But
    now, anyone can gather data from them.
  • GPS is a constellation of satellites that orbit
    approximately 11,000 miles above the Earth and
    transmit radio wave signals to receivers across
    the planet. By determining the time that it takes
    for a GPS satellite signal to reach your
    receiver, you can calculate your distance to the
    satellite and figure out your exact location on
    the Earth. Sound easy? In fact it is a very
    complicated process. For the GPS system to work,
    you need to have incredibly precise clocks on the
    satellites and receivers, and you must be able to
    access and interpret the signals from several
    orbiting satellites simultaneously. Fortunately,
    the receivers take care of all the calculations.
  • http//www.oceanservice.noaa.gov/education/kits/ge
    odesy/geo09_gps.html

22
Conclusion
  • Geodesy is an important for accurate measurements
    of the earth
  • Geods, elipsoids and spheres are abstractions of
    the earth
  • Datums are the measurements or data that directs
    the contruction of an elipzoid, sphere or geod
  • If accuracy is important (i.e., GPS)
  • The mixing or non-transformation of datums can be
    perhaps the difference between life or death if
    using it for navigation purposes.
  • If you hire a surveyor to survey a property you
    have just bought and he does not know what datum
    is being used..it is time for another surveyor.
  • Datums, projections and coordinate systems are
    related issues, as will be discussed in the next
    lecture

23
Some Other References
  • Datums, who needs em anyway?http//www.esri.com/
    news/arcuser/0401/datum.html
  • Geodesy Overview by Peter Danahttp//www.colorad
    o.edu/geography/gcraft/notes/datum/datum_f.htmlG
    eodesy Tutorial by NOAAhttp//www.oceanservice.n
    oaa.gov/education/kits/geodesy/welcome.html
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