Positioning Flashcards
the map of 1482 drawn by Ptolemy was important
because it was the first map to use cordinate system
it was the first map to use latitude and longitude
latitude
angle that describes the north-south position
parallel
circle connecting all locations with a given latitude
ex tropical of capicorn,tropical of cancer
pole
points where the earth’s axis of rotation meets its surface
smallest parallel
Equator
intersection of the earth’s surface with the plane perpendicular to the axis of rotation and midway betwen the poles
the equator is the biggest parallel
0 degree latitude
artic circle
southernmost latitude in the northen hemisphere where the sun can remain constinously above or below the horizon for 24 hours
66.5 degress north
Antartic circle
norternmost latitude in the south hemisphere where the sun can remain constinously above or below the horizon for 24 hours
66.5 degress south
tropic of cancer
northernmost circle of latitude where the sun can be directly overhead
northern hemesphere
23.5 degrees north
tropic of capricorn
southernmost circle of latitude where the sun can be directly overhead
south hemesphere
23.5 degrees south
Earth’s axil tilt
the eraths spins at 23.44 degrees tilt
how we define/get the information above
when the top of the earth is tilted towards the sun,it is summer in the northern hemisphere.since the southerer hemesphire is tilted away from the sun,it’s winter there
Longitude
angle that describes the east-west position
Meridian
half of an imagenery great circle,terminating at the north pole and the south poles,connecting points of equal longitude
orange slices
Prime Meridian
origin of the measures of longitude
pass through Greenwich, England
0 degrees of longitude
defines what is west and what is east
the shapes of the earth
- Earth:reality more complex and more accurate)
- Geoid
- Ellipsoid
- sphere(simplier and less accurate)
as it goes down: it gets simplier and less acurate
Geoid
- physical approximation of the figure of the earth
- shape of the surface of calmed oceans,in the absence of other influences such as winds and tides
- computed using complex physical models and gravity readings of eath’s surface
- used to measure surface elevations with a high degree of acurracy
- uses most often for earthquack but not normaly used in our day to day lives