lecture 2 Flashcards

1
Q

why is it complicated to define coordinates

A
  1. flat 2D maps are distorted
  2. earth is not a perfect sphere
  3. all measures contain some error
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2
Q

what is the earths shape

A

an oblate spheriod ellipsoid

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3
Q

earth –> ellipsoid

A

mathmatical representation

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4
Q

ellipsoid

A

used as a reference surface for horizontal coordinates
3D reference shape based on ellipse
- polar flattening and eccentricity
- around 30 ellipsoids used

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5
Q

geoid

A

earth shaped

  • made from precise measurements of gravity
  • vertical reference surface
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6
Q

relationship of ellipsoid vs geoid

A

earths surface bulges above or depressed below ellipsoid
ellipsoid replicates approximate shape of earth (horizontal)
- geod replicates vertical structure

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7
Q

ellipsoid/ geod –> datum (reference surface)

A

mathmatical empirical definition

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8
Q

datum

A

use info about the size and shape of the earth (ellipsoids and geoids) with a reference point to describe the location of other points on the earth
horizontal –> ellipsoid
vertical (elevation) –> geoid

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9
Q

horizontal datums

A

local - north american datum NAD

global - world geodetic system of 1984 WGS84

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10
Q

vertical datums

A

origin or zero point based on geoid
mean sea level to approximate height
- global: global sea level observing system (GSLOS)
- local: US national geodetic vertical datum (NAVD88)

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11
Q

datum (reference surface) –> globe

A

physical measurements

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12
Q

what is a coordinate system

A

system used to register and measure horizontal and vertical locations on the Earth
- movement over x and y axis

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13
Q

lat/long

A

latitude- angular distance from the equator
- going up the ladder
longitude- angular distance from prime meridian
- lengthwise

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14
Q

parallels & meridians

A

parallels: lines of latitude are the same distance apart
0-90
meridians: lines of longitude are varying distances
0-180

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15
Q

formats of geographic coordinates

A

decimal degrees:
ddd degree mm’ss”
minutes seconds :
123.3656

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16
Q

what is a map projection

A

arrangement of the coordinates of a 3D earth onto a 2D plane
- planar, cylinder, conic

17
Q

projection properties

A

line or point on a map has to be the same scale as the reference globe

  • aim to preserve geographic properties
    ex. area, angles, distances, directions, compromise
18
Q

exmaples of projections

A

albers equal area conic- maintains size
lambert conformal conic- maintain angles
lambert azimuthal equal area- maintain area
azimuthal equidistant- maintain distances
mollweide equal area- maintain area
goodes homolosine interrupted- methods of area and shape

19
Q

scale factor

A

map scale is an average scale
if no distortion: SF 1.0
if stretched: SF > 1
if compressed: SF < 1

20
Q

UTM (universal transverse mercator)

A

projected coordinate system

- easting and northing

21
Q

what do GPS coordinates depend on

A
  1. how to take points on a 3D surface and translate onto 2D
  2. the models we use to describe the earth (ellipsoid and geoid)
  3. measurements we reference our coordinates to (datum)