Lecture 1: Overview of Satellite Geodesy
Geodesy
The discipline that deals with the measurement and representation (geometry, physics, and temporal variations) of the Earth and other celestial bodies (International Association of Geodesy)
Satellite
A celestial body orbiting the Earth or another planet
Artificial Satellite
An artificial body placed in orbit round the Earth or another planet in order to collect information or for communication
Satellite Geodesy
Science of measuring Earth’s geometric shape, orientation in space, and gravitational field using artificial satellites.
Applications of Satellite Geodesy
Global Geodesy
General shape of the Earth’s figure and gravity field
Dimensions of a mean earth ellipsoid
Establishment of a global terrestrial reference frame
Detailed geoid as a reference surface on land and at sea
Connection between different geodetic datums
Connection of national datums with a global datum
Geodetic Control
Establishment of geodetic control for national networks
Installation of 3D homogenous networks
Analysis and improvements of existing terrestrial networks
Establishment of geodetic connections between islands or with the mainland
Densification of existing networks up to short interstation distances
Geodynamics
Control points for crustal motion
Polar motion, earth rotation
Solid earth tides
Applied and Plane Geodesy
Detailed plane surveying (cadastral, engineering, GIS, mapping, etc.)
Installation of special networks and control for engineering tasks
Terrestrial control points in Photogrammetric cameras
Control points for Cartography during expedition
Navigation and Marine Geodesy
Precise navigation of land, sea, and air vehicles
Precise positioning for marine mapping exploration, hydrography, oceanography, marine geology, and geophysics
Connections of tide gauges (unification of height systems)
Related Fields
Position and velocity determination of geophysical observations (gravimetric, magnetic, seismic survey) also at sea and in the air
Determination of ice motion in glaciology
Global
GPS — USA
Official name of GPS is Navigational Satellite Timing and Ranging Global Positioning System (NAVSTAR GPS)
The Global Positioning System (GPS) was designed for military applications
Its primary purpose was to allow soldiers to keep track of their position and to assist in guiding weapons to their targets
The satellites were built by Rockwell International and were launched by the US Air Force
The entire system is funded by the US government and controlled by the US Department of Defense
The total cost for implementing the system was over $12 billion
It costs about $750 million to manage and maintain the system per year
GLONASS: The “other” GPS — Russia
Global Navigation Satellite System
Two modes:
Standard Precision (SP)
High Precision (HP)
By April 2002, only 8 in operation
3 more launched in 2006, 18 more by 2007-end
Aim: to make GLONASS performance comparable by 2010 with GPS and Galileo
Fully restored: 2011, 24 satellites
Strong at high altitudes
Galileo GPS (ESA) — EU
Constellation of 30 satellites in 3 orbital planes inclined at 54° and at an altitude of around 23,000 km
Full civilian control, high accuracy
Private-public partnerships (PPP)
28 satellites
Excellent signal design for geodesy
BeiDou — China
35 satellites
Strong Asia-Pacific geometry
Now fully interoperable with GPS/Galileo
Regional NSSs
Quasi-Zenith Satellite System — Japan
Regional focus: Japan / East Asia
4-7 satellites (highly inclined orbits)
Always near zenith over Japan
Improves urban canyon and mountainous performance
Fully interoperable with GPS
NavIC (IRNSS) — India
Regional focus: India + ~1500 km
7 satellites (GEO + IGSO)
Dual-frequency modernization underway
Strategic independence for India
Applications of GNSS
PNT - Position, Navigation, Timing
GNSS surveying
International Terrestrial Reference Frame (ITRF) Realization
Geodetic Network Establishment
Atmospheric studies
Tropospheric and ionospheric applications
Sea level and Ocean
Sea Surface Height
Co-location studies
Non-GNSS Satellites used for Geodesy
Satellite Radar Altimetry
Send radar or laser pulses straight down
They provide:
Global mean sea level rise
Marine geoid validation
Ice sheet elevation change
Vertical datum realization
Coastal sea-level monitoring
Altimetry + gravimetry = modern height systems
Satellite Gravity Missions
Detect tiny changes in gravity, which correspond to mass movement
Satellite Laser Ranging (SLR)
Used for defining the geocenter (Earth’s center of mass)
Absolute scale of the terrestrial reference frame
Earth rotation parameters (ERP)
Low-degree geavity field
Tests of general relativity
Synthetic Aperture Radar (SAR)
Earthquake deformation
Volcanic inflation / deflation
Land subsidence (groundwater extraction)
Landslides
InSAR gives dense spatial coverage where GNSS is sparse
Doppler and Radio Tracking Missions
Precise orbit determination
Plate motion studies
Earth rotation
Gravity field support
Still part of the International Earth Rotation and Reference Systems Service (IERS) geodetic observing system
Very Long Baseline Satellites (Indirect, but critical)
Earth rotation and reference frames
No dedicated satellites — but quasars act as fixed reference points
VLBI + SLR + GNSS = global reference frame backbone