Topic 9 Flashcards

(47 cards)

1
Q

how do you determine what is the best coordinate system

A

depends on what you are doing/mapping

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2
Q

describe the projection process

A

choose how to model the earth
principale scale = scale reduction
reduced to the globe

global = sphere
small = ellipsoid

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3
Q

what does GCS do

A

tell me where on the earth the data should draw

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4
Q

what does the PCS do

A

tell me how to draw on the earth on a flat surface

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5
Q

GCS

A

latitude and longitude
3d reference type on a spherical surface

angular measures (degrees, minutes, seconds)

N,E are +
S,W are -

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6
Q

the geoid

A

equipotential surface
surface rises under continents and lowers under oceans - generally
variations in gravitational force due to irregular distribution of rocks

earth shaped

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7
Q

the ellipsoid

A

a regular geometric surface used to approximate the geoid

oblate or “flattened”

has easily defined axes

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8
Q

how to choose ellipsoid?

A

before 1980s different ellipsoids used for different areas.

satellite data allowed to choose a best fitting ellipsoid for the whole earth
(WGS84)

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9
Q

datums and characteristics

A

shape of ellipsoid

orientation of ellipsoid

size, position, orientation (3 key points)

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10
Q

what are the two types of datums

A

ECEF ( earth fixed) global
WGS84

Not ECEF (not earth fixed) local
NAD27
NAD83

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11
Q

prominent horizontal datums

A

NAD27

NAD83

WGS84

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12
Q

NAD27

A

north american datum 1927

based on clarke 1866 ellipsoid

NOT ECEF

basis for horizontal datum

developed to map North America

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13
Q

NAD83

A

north american datum 1983

based on GRS1980 ellipsoid

less flattened than NAD27

PLATE FIXED

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14
Q

WGS84

A

world geodetic system

slight change from the NAD 83 (2m + difference only)

slight orientation change

based on GRS1980

ECEF

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15
Q

ECEF vs. plate fixed

A

ECEF = earth centered, earth fixed
location is same, but earth might have moved

plate fixed = move lat and long locally according to earth movement

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16
Q

what is an epoch

A

mathchig timeframe of measurements to our maps
timeframe when the snapshot was taken

epoch = realization

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17
Q

what is the ITRS

A

international terrestrial reference system

describes procedures for creating reference frames

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18
Q

what is the ITRF

A

international terrestrial reference frames

realization of the ITRS
new reference frame solutions produced
snapshot of coordinates
lat/long elevation at point in time

updated every few years

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19
Q

what does a G730 realization mean

A

= # of weeks since Jan 1st 1980

G=GPS

so 730 weeks since Jan 1st 1980

20
Q

What is a GCS?

A

main components
sperhical coordinate system
mathmatical model (datum)

21
Q

what is EPSG

A

european petroleum survey group

stnadards for projections and coordinates

22
Q

vertical datums

A

defines 0 altitude, so references sea level
before 1980s based on measurments of ‘mean sea level”

NAVD88

CGVD2013

GNSS (based on ellipsoid not sea level measurments)!!

23
Q

what do vertical datums show

A

shows difference in height between ellipsoid and geoid

H = orthometric height
N = geoid height
h = ellipsoid height

H = h - N

if this equals -# that means ellipsoid is above the geoid

24
Q

what is CSRS

A

canadian spatial reference system

collection of standards, models, data products and infrastructure supportin geospatial positioning

coordinate base is also a reference frame like ITRF (canadian is plate fixed)

25
if your map is off mostly likely someone has incorrectly defined the reference system T/F?
true 70m is a small error for canada as a whole erros are inherently built inot the NAD27
26
what reference system is used for Canada
NTv2 NADCOW for USA very small difference between the NAD83 and the updated 2010 Alberta model of NAD83
27
reference difference in alberta
last arc second = aprx. 30 meters long arc second = depends what lat at north pole + = so tiny much larger at equator
28
PCS
cartesian how ti should be drawn on a flat surface drawing a 3d volume on a flat surface distortions will happen (golden triangle problem) choice of projection depends on what you are doing descringly important as cartogprahy scale increases (zoom in) bigger area = projection more important converting to x,y point positions
29
what are map projections families based on
developable surfaces ("the paper") plane, cone, cyclinder
30
Azimuthal projections
gnomic projection source at centre of earth used for navigation charts orthographic infinite light source looks like earth from space stereographic light from back or side of globe common historically mapping polar regions lambert conformal basemap for BC (used heaviley in Canada)
31
what is the basemap for alberta
tranverse mercator canada = lambert conformal conic
32
what are the 2 common cylindrical projections
mercator :wrapped around equator transverse mercator : wrapped around poles
33
4 key properties for projection distortion
shape area distance direction each projection is designed to achieve one or two of these
34
what is tissot's indicatrix
unit circle on globe visual help in understanding distortions preserve shape = conformal angles are the same size will vary preserve area = equal area area preserved angles compromised
35
shape : conformal projections
scale is the same in every direction around any given point (isotropic) scale changes between areas of the map shapes for small regions are portrayed accurately cant compare sizes lambert conformal conic
36
area: equal are projection
scale in small area changes depending on direction (anisotropic) shapes in small areas are distorted cant compare shape bonne projection albers equal area vs lambert conformal
37
distance: equidistant projections
true distances distance between any point and the north pole is true doesnt work for any two random points tho usualyl azimuthal no map can be conformal and equal area at the same time azimuthal equidistant projection conic equidistant projection
38
direction
direction measurements on the map same as those on the ground can be conformal, mercator can be maintained simultaneously with one or two of the other 3 properties
39
projection surface: tangent
stretching: where paper is above the globe c is not distorted a and e are stretched a lot b and d are stretched a little 1 standard line
40
projection surface: secant
shrinking: there paper is "inside" the globe b and d are not distorted a and e stretched (paper is above the globe) c is shrunken 2 standard lines
41
patterns of distortion (aimuthal)
tangent = 1 standard line secant = 2 standard lines
42
how does projection and concept of PCS work
plotting cartesian points on a x,y graph
43
universal transverse mercator (UTM)
basis of many topographic maps globe is divided into 60, 6 degree longitudinal strips each strip is "numbered zone" subdivided into latititude strips
44
transverse mercator characteristics
cyclindrical conformal projection secant pick meridian 6 degrees of longitude or strips, or zones maps are windows in the zones doesnt go all the way to the polar regions but only 84 degrees north and 80 degrees south central meridian moves with the projection UTM is only unique to a geographic coordinate system standard lines are not actually defined center of meridian = 500,000 m E so that we are always using positive numbers
45
is NAD83 CSRS a GCS?
yes
46
definition of a map projection
orderly system of parallels and meridians used to draw a map on a flat surface distortion must occur when transforming information from 3d to a flat surface choice of projection is dependent on the purpose of the map decreasingly important as cartographic scale increases
47
choice of map description
go by desired properties basic guidelines there is no right answer only good and bad choices trying to match the projection with the shape of the mapped earth plate fixed or ECEF