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Geographic information systems
computer based function used to capture, store, analyze, and display spatial or geographic data (uses layers of data, each layer has a different theme)
5 Components of a GIS
hardware, software, data, workflow, people
Uses for GIA
-cartography
-data management
-spatial analysis
Vector
crisp, realistic model not as good for data analysis
Raster
each cell has a single value for attributes you are collecting
High resolution
cells are smaller (more cells)
Low resolution
cells are larger (less cells)
Pros of raster data
some functions only run in raster, raster data is continuous
Cons of raster data
large data size = slow processing, resolution can reduce detail
Pros of vector data
small data sizes= fast loading, points are an accurate foundation of data
Cons of vector data
sharp boundaries between features, can be misleading for natural features
Where can you obtain GIS data?
digitizing, GPS, field survey, remote sensing
GPS applications
querying
analyzing
displaying
outputting
Querying data
searching and filtering, uses SQL (structured query language)
Buffers
-euclidean
-network
Euclidean buffers
creates a uniform buffer around a feature
Network buffers
applied through a medium (road, river, rail line), not in a straight line ex. Google maps
GPS
location finding and data network that bases data on a satellite, receiver measures distance from satellite to your location, the satellite broadcasts signals with accurate time information
Examples of GPS applications
military, space travel, agriculture, construction, mapping, public safety, utilities, transportation
3 parts of a GPS
-satellite (space segment)
-ground control (control segment)
-receivers (user segment)
Satellite
signals are captured by any ground receiver, composed of a computer, atomic clock, and a transmitter (GPS has 24 satellites and orbits 2x a day)
Ground control
made to communicate with the satellite (can be spoofed by the DOD)
Receivers
made to communicate with satellite
C/A Code
initial signal that a GPS receiver reads, long term orbitals, approximates location (ex. almanac)
P Code
more precise and complex, somewhat restricted use, short term orbital data critical for real-time data (ex. ephemeris)
Two way
uses two delays that naturally occur in signal transmission to determine the range between two stations (ex. speed radar)
One way
measurement of the travel time of a signal from transmitter to receiver w/ separate clocks (ex. counting time between lightning and thunder)
Trilateration
similar to triangulation, need 4 satellites for accurate ground location
Timing error
satellite clock drift (atomic clock can experience noise and drift), receiver clock offset (value used to adjust clock is wrong
Ephemeris
actual orbit is off predicted orbit (can’t fix)
Atmospheric delay
signal refraction; signals have light and can bend
Receiver circuit noise
some level of noise always contaminates observations as static or hissing
Multipath error
signals bounce off objects before they are captured by receivers (most common source of error, can be fixed by using a directional antenna)
Satellite geometry
arrangement of SV in relation to the receiver, the further apart they are, the higher the position accuracy (DOP and PDOP)
Differential correction
improves location accuracy, electronically moves points after the survey is taken