This document provides an overview of synthetic aperture radar (SAR) basics and theory. It discusses key aspects of SAR including how it works, imaging geometry, spatial resolution, backscatter coefficients, common frequency bands, and advanced modes. SAR uses microwave radiation and can image the Earth's surface in all weather and light conditions, providing complementary data to optical remote sensing. It discusses concepts such as range and azimuth resolution, factors that influence backscatter, and challenges like speckle that SAR addresses through techniques like multi-look processing.
This content presents for basic of Synthetic Aperture Radar (SAR) including its geometry, how the image is created, essential parameters, interpretation, SAR sensor specification, and advantages and disadvantages.
How to better understand SAR, interpret SAR products and realize the limitationsNopphawanTamkuan
This content shows how to better understand SAR (how to interpret SAR images and read SAR interferogram ). Moreover, capacities and limitations of SAR are discussed for each disaster emergency mapping (Flood, Landslide and Earthquake).
SAR is a type of radar which works with antenna and receiver using radio waves which can create two dimension or three dimension of the objects . A synthetic-aperture radar is an imaging radar mounted on a moving platform. SAR gives high resolution data and works 24*7.
This content presents for basic of Synthetic Aperture Radar (SAR) including its geometry, how the image is created, essential parameters, interpretation, SAR sensor specification, and advantages and disadvantages.
How to better understand SAR, interpret SAR products and realize the limitationsNopphawanTamkuan
This content shows how to better understand SAR (how to interpret SAR images and read SAR interferogram ). Moreover, capacities and limitations of SAR are discussed for each disaster emergency mapping (Flood, Landslide and Earthquake).
SAR is a type of radar which works with antenna and receiver using radio waves which can create two dimension or three dimension of the objects . A synthetic-aperture radar is an imaging radar mounted on a moving platform. SAR gives high resolution data and works 24*7.
RADAR - RAdio Detection And Ranging
This is the Part 1 of 2 of RADAR Introduction.
For comments please contact me at solo.hermelin@gmail.com.
For more presentation on different subjects visit my website at http://www.solohermelin.com.
Part of the Figures were not properly downloaded. I recommend viewing the presentation on my website under RADAR Folder.
This course gives keys to understand the SAR image and specificities: geometry, speckle, penetration capabilities, layovers, multipath, dielectric properties.
Advanced modes: polarimetry, interferomety and POLINSAR are also presented.
A ~25 slide presentation that explains the underlying principles and some applications of InSAR, with a particular focus on the measurement of deformation due to earthquakes. The presentation could be used in a lecture or lab setting, or provided to students for review out of class. The slides are annotated with additional background information designed to assist instructors.
SBAS-DInSAR processing on the ESA Geohazards Exploitation PlatformEmmanuel Mathot
In the context of space-borne geodetic techniques, Differential Synthetic Aperture Radar Interferometry (DInSAR) has demonstrated its high performance in measuring surface displacements in different conditions and scenarios, both natural and anthropic. In particular, the advanced DInSAR time series processing method referred to as Small BAseline Subset (SBAS), that allows studying both the spatial and temporal variability of the surface displacements, has proven to be particularly suitable in different contexts, as for natural hazards (volcanoes, earthquakes and landslides) and human-induced deformation (subsidence due to aquifer exploitation, mining operations, and building of large infrastructures). Recently, an efficient implementation of this algorithm (referred to as P-SBAS approach) has been fully integrated within the ESA’s Grid Processing on Demand (G-POD) environment, which is part of the [Geohazards Thematic Exploitation Platform (GEP)](https://geohazards-tep.eo.esa.int/#!) of ESA. The GEP is devoted to the exploitation of EO data resources in the context of the Geohazard Supersites & Natural Laboratories as well as on the CEOS Pilots on Seismic Hazards and Volcanoes. The GEP is sourced with elements, data and processing, including P-SBAS, relevant to the geohazards theme. The integration of the P-SBAS algorithm within GEP resulted in a web-based tool freely available to the scientific community. This tool allows users to process, from their own laptops, the European SAR data archives (ERS, ENVISAT and Sentinel-1) for obtaining surface displacement maps and time series in a completely unsupervised way, without caring about data download and processing facility procurements. The workshop is organized in four parts. First, a short overview on the DInSAR processing methods allowing retrieving mean surface deformation maps and displacement time series will be provided, with a specific focus on the SBAS-DInSAR technique. Secondly, the GEP and G-POD environments will be introduced and the P-SBAS web tool will be presented. The third and the fourth parts are dedicated to the advanced features and to case studies and results achieved via the web tool, respectively.
RADAR - RAdio Detection And Ranging
This is the Part 1 of 2 of RADAR Introduction.
For comments please contact me at solo.hermelin@gmail.com.
For more presentation on different subjects visit my website at http://www.solohermelin.com.
Part of the Figures were not properly downloaded. I recommend viewing the presentation on my website under RADAR Folder.
This course gives keys to understand the SAR image and specificities: geometry, speckle, penetration capabilities, layovers, multipath, dielectric properties.
Advanced modes: polarimetry, interferomety and POLINSAR are also presented.
A ~25 slide presentation that explains the underlying principles and some applications of InSAR, with a particular focus on the measurement of deformation due to earthquakes. The presentation could be used in a lecture or lab setting, or provided to students for review out of class. The slides are annotated with additional background information designed to assist instructors.
SBAS-DInSAR processing on the ESA Geohazards Exploitation PlatformEmmanuel Mathot
In the context of space-borne geodetic techniques, Differential Synthetic Aperture Radar Interferometry (DInSAR) has demonstrated its high performance in measuring surface displacements in different conditions and scenarios, both natural and anthropic. In particular, the advanced DInSAR time series processing method referred to as Small BAseline Subset (SBAS), that allows studying both the spatial and temporal variability of the surface displacements, has proven to be particularly suitable in different contexts, as for natural hazards (volcanoes, earthquakes and landslides) and human-induced deformation (subsidence due to aquifer exploitation, mining operations, and building of large infrastructures). Recently, an efficient implementation of this algorithm (referred to as P-SBAS approach) has been fully integrated within the ESA’s Grid Processing on Demand (G-POD) environment, which is part of the [Geohazards Thematic Exploitation Platform (GEP)](https://geohazards-tep.eo.esa.int/#!) of ESA. The GEP is devoted to the exploitation of EO data resources in the context of the Geohazard Supersites & Natural Laboratories as well as on the CEOS Pilots on Seismic Hazards and Volcanoes. The GEP is sourced with elements, data and processing, including P-SBAS, relevant to the geohazards theme. The integration of the P-SBAS algorithm within GEP resulted in a web-based tool freely available to the scientific community. This tool allows users to process, from their own laptops, the European SAR data archives (ERS, ENVISAT and Sentinel-1) for obtaining surface displacement maps and time series in a completely unsupervised way, without caring about data download and processing facility procurements. The workshop is organized in four parts. First, a short overview on the DInSAR processing methods allowing retrieving mean surface deformation maps and displacement time series will be provided, with a specific focus on the SBAS-DInSAR technique. Secondly, the GEP and G-POD environments will be introduced and the P-SBAS web tool will be presented. The third and the fourth parts are dedicated to the advanced features and to case studies and results achieved via the web tool, respectively.
This presentation is all about the wireless sensor networks, how they collect data using aggregation, and how they evaluate or calculate the parameters
Standard radar detection process requires that the sensor output is compared to a predetermined threshold. The
threshold is selected based on a-priori knowledge available and/or certain assumptions. However, any
knowledge and/or assumptions become in adequate due to the presence of multiple targets with varying signal
return and usually non stationary background. Thus, any predetermined threshold may result in either increased
false alarm rate or increased track loss. Even approaches where the threshold is adaptively varied will not
perform well in situations when the signal return from the target of interest is too low compared to the average
level of the background .Track-before-detect techniques eliminate the need for a detection threshold and provide
detecting and tracking targets with lower signal-to-noise ratios than standard methods. However, although trackbefore-
detect techniques eliminate
the need for detection threshold at sensor's signal processing stage, they often use tuning thresholds at the output
of the filtering stage .This paper presents a computerized simulation model for target detection process.
Moreover, the proposed model method is based on the target motion models, the output of the detection
process can easily be employed for maneuvering target tracking.
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Synthetic aperture radar (sar) 20150930
1. 10/12/2015
1
Synthetic Aperture Radar (SAR)
Basics and Theory
Dr. M Jahanzeb Malik
B.E. (Civil Engg.), NED University, Pakistan
M.Sc (Geo information science and Earth Observation), ITC-UT, The Netherlands
PhD (Remote Sensing and Land Surface Modeling), ITC-UT, The Netherlands
Remote Sensing (RS)
Electromagnetic
spectrum: Wave and
frequencies used in RS
Why microwave RS…?
Independence of the Sun as a
source of illumination:all-hour
Ability to penetrate clouds, haze,
dust (and to some extent rain):
all-weather
Ability to penetrate more
deeply into vegetation, snow,
soils then optical waves
Microwave RS complements
Optical RS
MODIS
Aqua
5-Aug, 10
R,G,B
5(NIR),1(R),4(G)
PALSAR
ALOS
L-Band
5-Aug, 10
2. 10/12/2015
2
Microwave RS complements Optical RS
ALOS: PALSAR, HH
ALOS:AVNIR, (R,G,B): (NIR,R,G)
Nawabshah/ Dadu,Sindh, Pakistan
Microwave RS complements Optical RS
Envisat,ASAR,WSM, C-Band,VV
01-Mar,2006
Tibet, China
Basic operation of RADAR
RADAR: RAdio Detection And Ranging
Spaceborne radar RS
Radar Altimeters: measure the round trip time delay to
targets to determine their distance from the sensor (e.g.,
SIRAL on CryoSat-2)
Radar Scattromters: make measurements of the amount of
energy backscattered from targets (e.g., Seawinds on
QuikSCAT)
Synthetic Aperture Radars (SAR): measure the round trip
time and amount of energy backscattered from targets (e.g.,
TerraSAR-X,COSMO-SkyMed,RADARSAT)
3. 10/12/2015
3
Imaging geometry of Side Looking RADAR
or pulse width
Bandwidth (B) = 1/τ
Common angles in radar imaging
slant range: the range along the radar line of sight, and
ground range: range from the nadir track along a smooth surface (the ground) to the
scatterer.
The incidence angle is the angle between the radar beam and ground surface
The look angle is the angle at which the radar looks at the surface
What does RADAR measure? Backscattering coefficient
units of m²
4. 10/12/2015
4
Spatial resolution
What is spatial resolution…?
the size of the smallest possible feature that can be
detected
RS in visible region:
For a homogeneous feature to be detected, its size
generally has to be equal to or larger than the IFOV.
If the feature is smaller than this, it cannot be detectable
as the average brightness of all features in that IFOV will
be recorded
Road
IFOVIFOV
Spatial resolution
SLAR Case:
Slant range resolution
Ground range resolution
Along-track (or azimuth)
resolution
=pulse duration
Range resolution
In designing the signal pattern for a radar sensor, there is
usually a strong requirement to have as much energy as
possible in each pulse in order to enhance the signal-to-
noise ratio (SNR)
This can be done by increasing the transmitted peak
power or by using a longer pulse
peak power is usually strongly limited by the available
power sources
an increased pulse length, which leads to a worse range
resolution
Spatial resolution vs range
5. 10/12/2015
5
Example: SLAR
X-band radar: 9.65 GHz (0.03 m); bandwidth: 150MHz
(pulse duration: 6.67 ns); speed of light: 2.9x108 m/s;
Antenna length: 9 m; height: 3000 m; incidence angle: 20
deg
Slant range resolution: 1 m
Ground range resolution: 3 m
Azimuth resolution: 11 m
Height: 500 km;Azimuth resolution: around 2 km
For this reason,SLAR are not commonly used in spaceborne remote sensing
SAR
The main difference between
SLAR and SAR is the way in
which the azimuth resolution is
achieved.
The longer synthetic array
allows a larger Doppler
bandwidth and, hence, a finer
surface resolution.
The range resolution derived for
a real aperture radar is still valid
here.
SAR: azimuth resolution
The achievable azimuth resolution of a SAR is
approximately equal to one-half the length of the actual
(real) antenna and does not depend on
platform altitude (distance or range)
Wavelength
It shows that a smaller antenna gives better resolution
Power of the antenna is proportional to the square of its
aperture
So, Penalty in SNR must be paid to push antenna aperture
to very small dimension
SAR basic principle
Shorter pulse duration (Te ) higher bandwidth (Be) higher range resolution
Now, SAR bandwidth is selectable, e.g., PALSAR 2 (14/28/42/84 MHz), RADARSAT2 (11.6-
100 MHz),TerraSAR-X (150/300 MHz)
6. 10/12/2015
6
Spatial resolutions
ALOS PALSAR
(L-Band; ~23 cm)
TerraSAR-X
(X-Band; ~3 cm)
Spatial resolutions
ALOS PALSAR
(L-Band; ~23 cm)
TerraSAR-X
(X-Band; ~3 cm)
Topographic effects on reflectivity and map
geometry
For slopes facing the radar, the ground
range resolution will be poorer than that for slopes facing away
from the radar.
Geometric issues
7. 10/12/2015
7
Geometric issues Geometric issues
Envisat,ASAR,
WSM, C-Band,VV
13-Feb, 2006
Tibet, China
Backscattering coefficients
𝜎 𝑂=
𝜎
𝐴 𝐿
𝛽 𝑂=
𝜎
𝐴 𝛽
Backscattering coefficient
Example: for an object with an RCS of 10m2, and an image
pixel size of 10mx10m, = -10dB.
8. 10/12/2015
8
Backscattering coefficient
The value depends on:
Physical and electrical properties of the material
Shape, size, orientation, arrangement
Dielectric constant
Sensor parameters
Wavelength
Polarization
Incidence angle
Site parameters
Surface roughness
Topographic relief
Backscattering coefficient
Airborne SAR systems Spaceborne SAR systems
The Envisat mission ended on Apr 2012, following the unexpected loss of contact with the satellite,
and RADARSAT-1 in Mar, 2013.
2014ALOS-2/PalSAR-2 8 – 70 deg.
9. 10/12/2015
9
Surface Interaction with the Radar Beam
Surface Scattering
Specular Scattering
Bragg Scattering
Volume Scattering
Main scattering mechanism
Main scattering mechanism How trees are seen by RADARS
10. 10/12/2015
10
Surface scattering
surfaces appear “rougher” at larger angles
Surface Roughness
Roughness is a relative concept depending upon
wavelength and incidence angle.
According to the Rayleigh criterion, a surface is
considered smooth if:
and considered rough if:
Commonly used frequency bands Advanced SAR modes
Stripmap:The classic mode for side looking SAR
instruments
ScanSAR (Wide Swath Mode): Increased swath width
with loss in azimuth resolution
Spotlight Mode: Improved azimuth resolution; no
continious imaging can be achieved
11. 10/12/2015
11
Spackles
Inherent to coherent systems (i.e., phase information is
preserved)
Spackles make interpretation more difficult
Spackles : salt and paper effect
Speckle reduction
Multi-look processing
By averaging the looks incoherently
pixel by pixel the speckle reduced
image is obtained.
The speckle reduced image has an
improved radiometric resolution, but
the geometric resolution will be
worse.
Adaptive and non-adaptive filters
A moving window filter changes the
intensity of the central pixel
depending on the intensities of all
the pixels within the window