satellite altimetry - possibilities and limitations by per knudsen kort & matrikelstyrelsen...
TRANSCRIPT
Satellite Altimetry- possibilities and limitations
by
Per KnudsenKort & MatrikelstyrelsenGeodetic DepartmentRentemestervej 8DK-2400 Copenhagen September 2001
Contents:• The system:
• Principle of altimetry• Sampling characteristics
• Applications:• Mean sea surface• Sea level variability• Sea level changes
• Operational issues• Data services• In Europe
The System:Principle of altimetry
– A space borne tide
gauge:
S: The distance is measured by the onboard altimeter,
H: The position and height of the satellite is computed,
SSH = H – S: The sea surface height above a reference ellipsoid is obtained.
Altimeter Satellites:Satellites: Launch:Skylab 1973
GEOS 3 1974
SeaSat 1978
GEOSAT 1984
ERS-1 1991
TOPEX/POSEIDON 1992ERS-2 1995GFO 1998JASON 2001ENVISAT 2001
The Altimeter:The pulse and its
return:The pulse is generated
by a 13.5 GigaHz oscillator, transmitted at 1000 Hz, and averaged at 1 sec.s
The return of the pulse depends on
• Distance• Surface roughness• Significant wave
height
The Altimeter:
The waveform:
The waveform depends on
• Travel time: Distance / height
• Surface roughness sigma_0 - Windspeed
• The slope - Significant waveheight
Sampling of the Sea Surface
Altimeter data are collected along the satellites ground track with a spacing of 7 km – 1 sec averages.
Sampling of the Sea Surface
One revolution of the satellites orbit takes about 100 - 115 min.s depending on the altitude of the satellite (800 – 1350 km).
Hence, the satellite completes 13–14 revolutions per day.
Sampling of the Sea Surface
The number of tracks, i.e. the track density, depends on the repeat period, e.g. 3 days.
The coverage depends on the inclination of the orbit plane.
Orbit Parameters
Satellite
Repeat Period
Track spacing
Inclination
Geosat 17 days 163 km 108°
ERS 35 days 80 km 98°
T/P 10 days 315 km 66.5°
The actual coverage of the sea surface depends on the orbit parameters such as the inclination of the orbit plane and repeat preiod.
Applications 1
Mean sea surface: • Reference surface• Geo-centric• Consistent with GPS / GNSS
Example: Mean sea surface from a merge of about 10 years of altimetric sea surface heights.
Mean Sea Surface from multi-mission altimetry
Applications 2
Sea surface variability: • Statistics of variability• Sea level anomalies
Periodic signals Non-periodic signals
Examples:1. Variability (RMS) of sea surface w/o
tides2. Daily signals: Ocean tides3. Meso-scale: El niño 1997 event4. Seasonal: Annual cycle
Sea level variability
M2 ocean tides model
M2 loop
Seasonal Cycle
El Niño - 1997
El Niño - 1997
Applications 3
Sea level changes: • Global coverage – open ocean• Uniform Geocentric reference
• About 10 years of data Spatial characteristics
• Calibration needed at tide gauges
ERS
Altimeter data services
Satellite altimetry is made available through the space agencies:• ESA• NASA, CNES, • US-navy
Upgraded / value added products are available through• Space agencies ( NASA/JPL,
CNES/CLS )• Research institutions ( CSR, DEOS,
KMS, GFZ )
Operational issues
Satellite altimetry is becoming available in near-real time to contribute to the monitoring of present changes in sea level to contribute to programmes such as• GOOS, and• El Niño forecasting
Problems:• Not real-time (4-6 hours)• Insufficient sampling locally – more
satellites
Operational issues
Potential data products:• Mean sea surface• Statistics of variability, extreme
sea level• Ocean tides• Seasonal cycles• Sea level anomalies• Sea level trends – decadal
variations
ConclusionsSatellite altimetry has proven its value in studies
of• Mean sea surface• Ocean dynamics
Satellite altimetry has shown its potential in studies of• Sea level changes
Satellite altimetry has, furthermore, a potential in• Hydrography / surveying – Bathymetry - GPS• Operational sea level services