introduction to remote sensing fundamentals of …timor.dhigroup.com/descriptions/2_fundamentals...
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Introduction to Remote Sensing –
Fundamentals of Satellite Remote Sensing
Mads Olander Rasmussen ([email protected])
• “the art, science, and technology of obtaining reliable information about
physical objects and the environment, through the process of recording,
measuring and interpreting imagery and digital representations of energy
patterns derived from noncontact sensor systems”. (Cowell 1997)
• “Satellite remote sensing refers to the reception, preprocessing and later
analyses of data obtained from Earth orbiting satellites” (Campbell, J.B.,
2001)
• Other terms: Earth Observation
What is remote sensing?
Components of a remote sensing system
PRE-PROCESSING
Remote Sensing
Platform
IMAGE ANALYSIS END USER INFORMATION
1858 1900 1950 19901970
Balloon
Plane
Space
Program
Landsat-4
SpaceShuttle
Landsat-1
Sputnik
Meteorological
Satellites
Space Station
2010
ERS-1UnitedSsatte
Commercial
Satellites
Pigeon camera
Historical development of remote sensing systems
2014
• Airborne (lidar, hyperspectral, thermal etc.).
• Unmanned (UAV)
• Ground sensors
Other sources of Remote Sensing data
• Satellite and Sensor types
• Satellite orbit
− Spatial resolution
− Temporal resolution
− Spectral resolution
• From reflected ’light’ to a satellite image
− The electromagnetic spectre
− Spectral signatures
• Digital image processing
Key parameters
Satellite orbits
• Polar-orbiting satellites (200-1000km)
Most satellites are polar orbiting. They
circle the Earth in a certain track that
allows them to monitor all areas within a
certain time interval (e.g. Landsat, SPOT,
WorldView, Sentinel)
• Geo-stationary satellites (36000 km)
Geo-stationary satellites orbit Earth in
app. 36.000 km altitude. Monitors the
same area of the Earth at all times (e.g.
Meteosat, NOAA GOES)
• Passive
− Sun’s energy which is reflected (visible) or
− Absorbed and re Absorbed and re-emitted as
emitted as thermal infrared wavelengths
− Landsat, SPOT, WorldView, Pleiades
• Active
− Emit radiation
− Radiation reflected is detected and measured
− SAR, LIDAR, and SONAR
− SRTM (Shuttle Radar Topography Mission)
Types of Satellite Sensors
© DHI
There is no such thing as bad weather…
Active/
SAR data
Passive/
Optical data
An image type for all weather conditions:
• Ikonos (1 / 4 m) - 1999
• QuickBird (0,6 / 2.4 m) - 2001
• WorldView-1 (0,5 m) – 2007
• GeoEye-1 (0,5 / 2 m) - 2008
• WorldView-2 (0,5/2 m) – 2009
• Pleiades (0,5/2 m) – 2011/2012
• SkyBox
• …etc!
Very High Resolution
• Landsat (15 - 90 m) - 1973
• SPOT (2.5-20 m) - 1981
• IRS (5 – 23 m) - 1988
• Aster (15-90 m) – 1999
• RapidEye (5 m) – 2009
• DMC2 (22m) - 2009
• SPOT 6-7 (1.5m) – 2012/2014
• Sentinel 2 (10/20/60m) - 2015
• PlanetLabs (5-8m) - 2015…
• …
High/Medium Resolution
• NOAA AVHRR (1 km) - 1998
• MODIS (250 – 1000 m) - 1999
• MERIS (300 – 1000 m) – 2002
• NPP VIIRS (750m) - 2011
• Geostationary (Meteosat/MSG/GOES,MTSAT etc) (3km – 8 km)
• …
Low Resolution
© DHI
A. Archive imagery
− On/offline archives
− What has been imaged in the past
B. New acqusition
− Possibility of controlling the time and area to be imaged
− Area of 2400 sqkm can be collected in a few minutes!
Getting access to imagery with high resolution
• Spatial …is defined as the area of
ground represented by one
pixel in the image
Key parameter: RESOLUTION
• Spectral …is a measure of the number
(and width) of bands in which a
given sensor records
information
…is defined as the frequency at
which images are recorded in a
specific place on the earth
• Temporal
• Spatial …is defined as the area of
ground represented by one
pixel in the image
Key parameter: RESOLUTION
• Spectral …is a measure of the number
(and width) of bands in which a
given sensor records
information
…is defined as the frequency at
which images are recorded in a
specific place on the earth
• Temporal
• The registered energy for every band is written to an image file; everyobservation becomes a pixel value.
• Each value represents the average brightness for a portion of the surface,
represented by the square unit areas in the image. In computer terms the
grid is commonly known as a raster, and the square units
are cells or pixels
• Satellite Images are typically stored as GeoTiff images (.tif)
Digital Image
• Very High Resolution
0.5 - 1 m
• High/Medium Resolution
2.5 - 90 m
• Low Resolution
250 m – 8 km
Spatial Resolution
Spatial resolution is controlled by the specifications of the radiometer, view
angle geometry and the orbit altitude
Spatial Resolution
• Spatial …is defined as the area of
ground represented by one
pixel in the image
Key parameter: RESOLUTION
• Spectral …is a measure of the number
(and width) of bands in which a
given sensor records
information
…is defined as the frequency at
which images are recorded in a
specific place on the earth
• Temporal
• Temporal resolution is important when choosing imagery
− If the goal is to monitor a process that changes rapidly (e.g. floods, fires), several images may be needed per day
− If the goal is to document a slow process (e.g. Vegetation trends, Glacier movement or urban growth) then one image per year would suffice
Temporal Resolution
• Use time series of satellite data to include seasonal variations of
wetness/flooding
Importance of time series
• Spatial …is defined as the area of
ground represented by one
pixel in the image
Key parameter: RESOLUTION
• Spectral …is a measure of the number
(and width) of bands in which a
given sensor records
information
…is defined as the frequency at
which images are recorded in a
specific place on the earth
• Temporal
• 2 relevant parts of the electromagnetic spectrum:
− Visible-IR (Optical)
− Microwave (SAR)
• Not all parts of the spectrum are ’transparent’
• Electromagnetic radiation blocked primarily by: water vapour, Ozone, CO2
and aerosols (dust etc.)
The electromagnetic spectre
Pan-c
rom
atisk
bill
ede
Fals
e-c
olo
r im
age
Spectral resolution
400 500 600 700 800 900 1000 1100
MS
WV2 Pan
WV1 Pan
MS
QB Pan
Wavelength (nm)
400 500 600 700 800 900 1000 1100
MS
WV2 Pan
WV1 Pan
MS
QB Pan
Wavelength (nm)
Blue Green Red Near-Infrared
• Optical remote sensing is based on the detection of reflected and emitted
energy at different wavelenghts
Different materials will have varying reflective/emmissive proportions at
different wavelengths.
Radiation principles
Landsat 8 - Band Combinations
Natural Color 4 3 2
False Color (urban) 7 6 4
Color Infrared (vegetation) 5 4 3
Agriculture 6 5 2
Atmospheric Penetration 7 6 5
Healthy Vegetation 5 6 2
Land/Water 5 6 4
Natural With Atmospheric
Removal
7 5 3
Shortwave Infrared 7 5 4
Vegetation Analysis 6 5 4
Spectral signatures
0.4 0.5 0.6 0.7 0.9 1.6
Vegetation
Soil
Wavelength (µm)
Ref
lect
an
ce (
%)
50
Blu
e
Gre
en
Red
Nea
r-in
fra
red
Mid
-in
fra
red
• Spatial …is defined as the area of
ground represented by one
pixel in the image
Key parameter: RESOLUTION
• Spectral …is a measure of the number
(and width) of bands in which a
given sensor records
information
…is defined as the frequency at
which images are recorded in a
specific place on the earth
• Temporal
• Radiometric …refers to the effective bit-
depth of the sensor (number of
grayscale levels)
Key parameter: RESOLUTION
…what is the cost?• Economic