Topic 02 pt 2 Flashcards

(31 cards)

1
Q

geoid

A

equipotential surface
gravity measurements
variations in mean sea level
rises under continents and lowers under oceans generally

trying to model mathematically

constantly changing

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2
Q

ellipsoid

A

regualr geometric shape used to approximate the geoid

semi - minor axis (Y)

semi-major axis (X)

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3
Q

NAD27

A

describes Clark 1866 ellipsoid
was latered to maximize NA
based entirely on ground surveys
lots of distortions built into it

local datum

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4
Q

NAd 83, WGS84

A

almost identical, growing further apart

both shared GRS80 ellipsoid, but origin differs by about 2,=m

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5
Q

what is the best fitting ellipsoid

A

WGS84

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6
Q

datums

A

not just the ellipsoid (is geometric shape)

size of ellipsoid

position of ellipsoid relative to earth

two types

ECEF
Not ECEF

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7
Q

ECEF

A

global datum (doesnt move)

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8
Q

Not ECEF

A

local datums for specific regions

moves

plate-fixed

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9
Q

horizontal datums

A

NAD 27

clark 1866

Not ECEF

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10
Q

NAD83

A

GRS80

plate-fixed
almost ECEF

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11
Q

WGS84

A

World geodetic model
ECEF
slight change from NAd 83

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12
Q

ECEF vs plate fixed

A

ECEF
location of permanent flag would change locations

plate fixed
changes alongside with the flag location so coordinates don’t change

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13
Q

ITRS

A

international terrestrial reference system
procedures and standards

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14
Q

ITRF

A

international terrestrial reference frames

reference frames
realization of the procedures
describes regulations for measuring the earth

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15
Q

realizations of WGS84 since original data

A

in weeks EPOCH

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16
Q

EPSG

A

european petroleum survey group

codes on realizations

17
Q

GCS

A

combinations of datum and how we put lat/long on that datum
arbitrary starting starting point at the equator

18
Q

vertical datums

A

NAVD88

CGUD2013

GNSS

19
Q

NAVD88

A

supplement for the NAVD29
vertical datum

20
Q

CGUD2013

A

used in canada
provides the separation between NAD83 (CSRS)

21
Q

GNSS

A

based on ellipsoid, not sea level measurements

22
Q

calculating heights

A

getting elevation above ellipsoid not the sea level

H = orthometric height
h = ellipsoid height
N = geoid height
(changes, correction factor)

H = h - N

23
Q

CSRS

A

collection of standards, protocols, models etc

all the things that go into geospatial positioning

24
Q

NAD83 (original)

A

pretty much the same as the NAD27

ground based

static

25
NAD83 (CSRS)
based on satellite 3d dynamic realization `
26
NAD83 coordinate transformations
transformations between NAD83 (CSRS) to ITRF NTV2
27
grid shift lines
grid cells where distortions are similar and has a distinct correction factor density grid in urban areas to be more precise
28
NTV2 (NAD27 - NAD83 original)
6.1m Lat distortion 70m Long in calgary
29
NTV2 (NAD83 original - NAD83 (CSRS 2010 Alberta)
4cm lat 6cm long
30
GPS -H
vertical datums convert between ellipsoid height to height of geoid based on gravitational model CGVD2013 (difference of 16m)
31
Choice of a map projection
based on type of distortions that are acceptable go by desired properties how much error exists within each projection (IE scale factor)