Topic 02 pt 2 Flashcards
(31 cards)
geoid
equipotential surface
gravity measurements
variations in mean sea level
rises under continents and lowers under oceans generally
trying to model mathematically
constantly changing
ellipsoid
regualr geometric shape used to approximate the geoid
semi - minor axis (Y)
semi-major axis (X)
NAD27
describes Clark 1866 ellipsoid
was latered to maximize NA
based entirely on ground surveys
lots of distortions built into it
local datum
NAd 83, WGS84
almost identical, growing further apart
both shared GRS80 ellipsoid, but origin differs by about 2,=m
what is the best fitting ellipsoid
WGS84
datums
not just the ellipsoid (is geometric shape)
size of ellipsoid
position of ellipsoid relative to earth
two types
ECEF
Not ECEF
ECEF
global datum (doesnt move)
Not ECEF
local datums for specific regions
moves
plate-fixed
horizontal datums
NAD 27
clark 1866
Not ECEF
NAD83
GRS80
plate-fixed
almost ECEF
WGS84
World geodetic model
ECEF
slight change from NAd 83
ECEF vs plate fixed
ECEF
location of permanent flag would change locations
plate fixed
changes alongside with the flag location so coordinates don’t change
ITRS
international terrestrial reference system
procedures and standards
ITRF
international terrestrial reference frames
reference frames
realization of the procedures
describes regulations for measuring the earth
realizations of WGS84 since original data
in weeks EPOCH
EPSG
european petroleum survey group
codes on realizations
GCS
combinations of datum and how we put lat/long on that datum
arbitrary starting starting point at the equator
vertical datums
NAVD88
CGUD2013
GNSS
NAVD88
supplement for the NAVD29
vertical datum
CGUD2013
used in canada
provides the separation between NAD83 (CSRS)
GNSS
based on ellipsoid, not sea level measurements
calculating heights
getting elevation above ellipsoid not the sea level
H = orthometric height
h = ellipsoid height
N = geoid height
(changes, correction factor)
H = h - N
CSRS
collection of standards, protocols, models etc
all the things that go into geospatial positioning
NAD83 (original)
pretty much the same as the NAD27
ground based
static