Title: Remote%20Sensing%20
1Remote Sensing Geodesy
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3What is Remote Sensing?
the science of deriving information about
Earth's land and water areas from images acquired
at a distance
4- Starting in 1946, captured V-2 rockets were
launched to gt 100 km by the U.S. Army - Launch 13 in the V-2 series contained a motion
picture camera in its nose cone, which acquired a
series of views of the Earth's surface as it
proceeded to a 134 km altitude.
http//rst.gsfc.nasa.gov/
5The Soviet Union surprised the world when it
launched Sputnik, the world's first satellite, on
October 4, 1957. The U.S. quickly followed suit
Explorer I, was launched into Earth orbit on Jan.
31, 1958 and discovered the Van Allen radiation
belts (above, right). In the 1960s spy planes
and satellites were common (e.g., right Cuban
missile crisis) .
6Landsat
S.F. Bay Area
http//geo.arc.nasa.gov/sge/landsat/
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8Satellite Orbits
Geostationary
- Communications satellites use a geostationary
orbit, in which the satellite is always in the
same position (above the equator) with respect to
the rotating Earth. - Geostationary orbits are high altitude (35700
km)
9Satellite Orbits
Polar
- Many remote-sensing satellites use a polar orbit
to provide a more global view of Earth - These satellites operate in a sun-synchronous
orbit at an altitude of 700 to 800 km - .
10Multispectral Imaging Systems
- MSI systems are passive devices that measure
electromagnetic waves (e.g. light, infrared) at
different wavelengths, then combine the results - Example Landsat Thematic Mapper (TM) images are
produced using 7 different spectral bands
http//www.classzone.com/books/earth_science/terc/
content/investigations/esu101/esu101page07.cfm
11Multispectral Imaging Systems
http//www.classzone.com/books/earth_science/terc/
content/investigations/esu101/esu101page07.cfm
12Global Positioning System
- The Global Positioning System is a network of 24
satellites placed into orbit by the U.S.
Department of Defense. - The satellites circle the earth twice a day in a
very precise orbit and transmit information to
earth.
13Global Positioning System
- A GPS location is pinpointed using triangulation
from 3 or more satellites. - Today, GPS is used extensively for navigation
and geodetic studies.
http//pasadena.wr.usgs.gov/office/hudnut/scec/97_
SCEC_E_summary.html
14Satellite Radar Systems
- Radar satellites (e.g., ERS2, Radarsat) are
active systems that reflect radar beams from
Earths surface. - Radar waves can pass through clouds and so
provide more continuous coverage of the surface
15Satellite Radar Systems
- Since the satellite orbits approximately repeat,
radar images of the same region can be compared
(radar interferometry) - Interferometric synthetic aperture radar (InSAR)
techniques are used to study dynamic systems
(e.g., Indian earthquake on right)
http//www.gfz-potsdam.de/ pb1/pg5/research/method
s/insar/insar_uk.html
16Satellite Gravity Systems
- CHAMP (CHAllenging Minisatellite Payload),
launched July 15, 2000, is a German small
satellite mission that measures Earths gravity
using precise GPS orbital data
17Satellite Gravity Systems
- The Gravity Recovery and Climate Experiment
(GRACE) March 2002 mission detects changes in
Earths gravity field by monitoring the distance
between the two satellites - The trailing spacecraft is actually about 220
kilometers behind the lead spacecraft.
18Satellite Gravity Data
- New data from satellite gravity missions is
being used for plate tectonic research - Note improvement in the resolution of gravity
anomalies in Tonga trench region
http//www.csr.utexas.edu/grace/gravity/solid_eart
h.html
19http//www.gfz-potsdam.de/pb1/op/champ/
20Geodesy Study of Earths shape
- The Earth is not quite a perfect sphere
- This shape is called the reference ellipsoid
(RE) - RE has the shape of a drop of ideal fluid
rotating at same velocity as Earth!
http//earth.leeds.ac.uk/dynamicearth/internal/sha
pe.htm
21Geodesy Study of Earths shape
- Geoid The hypothetical Earth surface that
coincides with sea level everywhere. - Usually, the Reference Ellipsoid is used for a
datum. - Large-scale Geoid anomalies reflect the mass
distribution in Earths mantle.
22Geoid