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GIS 104
Microwave introduction
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Microwave sensing
Encompasses both
active
and
passive
forms of remote sensing
Microwave
portion of the spectrum
Covers the range from approximately
1cm
to
1m
in wavelength
Longer wavelength microwave radiation can penetrate through
cloud
cover, haze, dust, and all but the heaviest
rainfall
Longer
wavelengths are not susceptible to atmospheric scattering which affects
shorter
optical wavelengths
Passive
microwave
sensing
Similar in concept to thermal remote sensing
All objects emit microwave energy of some magnitude, but the amounts are generally very small
A
passive microwave sensor
detects the naturally emitted microwave energy within its field of view
Emitted energy is related to the
temperature
and
moisture
properties of the emitting object or surface
Passive microwave sensor
1.
Antenna
is used to detect and record the microwave energy
2.
Microwave
energy can be emitted by the atmosphere
3. Reflected from the surface
4. Emitted from the surface
5. Transmitted from the subsurface
Passive microwave sensors
Characterized by
low spatial resolution
Applications of passive microwave remote sensing
Meteorology
Hydrology
Oceanography
Active microwave sensors
Provide their own source of
microwave radiation
to illuminate the target
Generally divided into two distinct categories:
imaging
and
non-imaging
RADAR
RAdio
Detection
And
Ranging
Sensor transmits a microwave (
radio
) signal towards the target and detects the
backscattered
portion of the signal
Strength of the backscattered signal is measured to
discriminate
between different targets
Time
delay between the transmitted and reflected signals determines the
distance
(or range) to the target
Non-imaging microwave sensors
Include
altimeters
and
scatterometers
Profiling devices which take measurements in one
linear
dimension, as opposed to the
two-dimensional
representation of imaging sensors
Radar altimetry
Transmit
short microwave pulses
and measure the round trip time delay to targets to determine their
distance
from the sensor
Generally altimeters look straight down at nadir below the
platform
and thus measure
height
or elevation
Scatterometers
Used to make precise
quantitative
measurements of the amount of
energy backscattered
from targets
Amount of energy backscattered is dependent on the surface
properties
(roughness) and the
angle
at which the microwave energy strikes the target
Advantages of radar
Capability of the radiation to penetrate through
cloud cover
and most
weather conditions
Can be used to image the
surface
at any time, day or
night
Radar image is quite different from and has special
properties
unlike images acquired in the visible and
infrared
portions of the spectrum
First demonstration of the transmission of radio microwaves and
reflection
from various objects achieved by
Hertz
1886
First
rudimentary radar
developed for
ship detection
Early
1900s
Experimental ground-based pulsed radars developed for detecting objects at a distance
1920s
and
1930s
First imaging radars used with rotating sweep displays for detection and positioning of aircrafts and ships
World War
II
Side-looking airborne radar (SLAR) developed for
military terrain reconnaissance
and
surveillance
After World War
II
Advances in SLAR and development of higher resolution synthetic aperture radar (SAR) for military purposes
1950s
Radars
declassified
and began to be used for
civilian mapping
applications
1960s
Canada became involved in radar remote sensing
Mid-1970s
Canada's
SURSAT
(Surveillance Satellite) project
1977
to
1979
Launch of ESA's
ERS-1
satellite
1991
Launch of Japan's
J-ERS
satellite
1992
Launch of
ERS-2
and Canada's
RADARSAT
satellite
1995