INTRODUCTORY REMOTE SENSING
INTRODUCTORY REMOTE SENSING
Landsat 7 15 m image highlighting the geology of Oman
http://www.satimagingcorp.com/gallery/landsat-geology-lg.htmlhttp://www.satimagingcorp.com/gallery/landsat-geology-lg.html
ASTER 15 m SWIR image, Geology, Yemen
http://www.satimagingcorp.com/satellite-sensors/aster.htmlhttp://www.satimagingcorp.com/satellite-sensors/aster.html
ASTER 15 m SWIR image, Mexicali
ASTER 15 m image, Las Vegas
MODIS 500 m hyperspectral image, Alaska
https://airbornescience.nasa.gov/instrument/MAShttps://airbornescience.nasa.gov/instrument/MAS
GOALS OF THE COURSE
• Overview of basics of remote sensing: • Electromagnetic spectrum, spectral responses of objects
(e.g., trees, houses, crops) • Platforms/Sensors: where / how they capture energy • How this energy gets converted into images (A2D)• Development of technical / theoretical skills for reading,
enhancing and processing remotely sensed data (DIP)• Use of remotely sensed imagery in environmental change
detection, urbanization, desertification, deforestation, forest fire monitoring, natural hazards monitoring, etc.
WHAT IS REMOTE SENSING?
• Remote sensing is the art and science of acquiring information about the Earth's surface without actually being in contact with it. This is done by sensing and recording reflected or emitted energy and processing, analyzing, and applying that information.
WHAT IS REMOTE SENSING?
• Platforms (C/B/D/A/S)• Data types
• Aerial photographs (analog / digital)• Satellite images (digital)
• Science: Physics• Scattering, etc.• RADAR
• Art: Subjective interpretation
SPECTRAL SIGNATURES AND SENSORS
http://www.tankonyvtar.hu/en/tartalom/tamop425/0032_terinformatika/ch05.htmlhttp://www.tankonyvtar.hu/en/tartalom/tamop425/0032_terinformatika/ch05.htmlhttp://www.tankonyvtar.hu/en/tartalom/tamop425/0032_terinformatika/ch05.htmlhttp://www.tankonyvtar.hu/en/tartalom/tamop425/0032_terinformatika/ch05.html
CHARACTERISTICS OF REMOTELY SENSED IMAGERY
• Data resolutions• Spatial (pixels)• Spectral (bands)• Temporal (orbits)• Radiometric (DNs)
• Data sources: Visible light, near (reflected) to far (heat) IR, microwaves (radar)
• and much more.
False colour
AERIAL PHOTOGRAPHY
• Stereo-effect: pairs of images that are displaced produce a 3-D effect
• Allows for measuring elevation
INFRARED IMAGERY
Airborne thermal IR (25 cm resolution) of homes highlighting energy loss
http://www.imagingnotes.com/go/article_free.php?mp_id=181http://www.imagingnotes.com/go/article_free.php?mp_id=181
SATELLITE IMAGERY: OCEAN MONITORING
Eddies off of Haida Gwaii
SeaWiFS (1 km)June 13, 2002.
http://earthobservatory.nasa.gov/IOTD/view.php?id=2536http://earthobservatory.nasa.gov/IOTD/view.php?id=2536
DROUGHT MONITORING
JULY 2001 JULY 2002
LANDSAT THEMATIC MAPPER (30 m) (SOURCE: CCRS 2002)
(Healthy vegetation is bright red)
MODIS imagery (200 m) showing Myanmar before and after being hit by a cyclone.
DISASTER MONITORING
http://movingimages.wordpress.com/2008/05/
LIGHT DETECTION AND RANGING
Forest canopy (1st return)
Using many rapid small bursts of laser light, a record of the terrain is produced from
the reflections obtained from multiple sources.
Ground surface (last return)
LIDAR
Archaeology
Oceanography
Forest inventory
RADAR – MONITORING SEA ICE
(30 m)
RADAR -- INTERFEROMETRY
THE ‘SYSTEM’
• A: Source of EMR• B: Electromagnetic radiation (EMR)• C: Object of interest• D: Sensor• E: Transmission to receiver• F: Data products (DIP)• G: Results of analyses
A
DIGITAL IMAGE PROCESSING
1. Pre-processing: Radiometric Correction and Georeferencing
2. Classification:1. Unsupervised Classification2. Supervised Classification3. Object-based Classification
3. Change Detection & Data Integration (GIS)
http://www.clarklabs.org/products/Object-Oriented-Image-Segmentation-and-Classification.cfmhttp://www.clarklabs.org/products/Object-Oriented-Image-Segmentation-and-Classification.cfm
DIGITAL IMAGE PROCESSING: CLASSIFICATION
• A wide variety of methods can be used, each of which may produce a different result. No one method is necessarily the ‘best’.
• Accuracy assessment is a necessary component in any classification.• Methods can produce a soft (fuzzy classes) or a hard classification.
Named classes
Training sites
Classified image
Pixels DN-based classesAssign
names to classes
Image segmented into blocks
Objects identified
Blocks assigned to
classes
• Non-uniform• Varies according to
• Wavelength• Time
• Active sensors are less variable
• Uniform emissions
EMR: SOURCE
IDEAL Reality
• Interfering• Varies according to
• Wavelength• Windows
• Atmospheric conditions
• Time and place• Source’s position
• Blue sky• Red sunsets
• Non-interfering
EMR: ATMOSPHERE
IDEAL REALITY
• Common responses from dissimilar objects
• Responses vary even for a known target• Time (e.g., seasons)• Angle of source-target-
sensor• Much remains to be
documented
• Unique• Known
OBJECT REFLECTANCE
IDEAL REALITY
• Sensors have variable sensitivities (and the sensitivity can vary the need for frequent calibration)
• Spatial and spectral resolution varies
• Highly and equally sensitive to all wavelengths
• Consistent spatial and spectral resolutions
SENSORS
IDEAL REALITY
• Processing is not always timely
• Interpretation is fraught with complications
• Results are software- and user-dependent
• Real-time processing and consistent interpretation
• Software is easy to use• Data is easy to obtain
DIGITAL IMAGE PROCESSING
IDEAL REALITY
• Limited or unrealistic impressions of RS
• Lacking in domain-specific knowledge
• Transformation of data to knowledge is complex
• In-depth knowledge of remote sensing and GIS
• Domain-specific knowledge (e.g., forest ecology, oceanography)
USERS
IDEAL REALITY
FINAL EXAM
• Three components:• Definitions (point form okay, use diagrams if helpful)• Short answers (point form okay, use diagrams if helpful)• Essay questions (proper grammar) (50%)
• Exam will cover:• Lectures• Labs• Chapters from text• Entire term
WHAT NEXT?
• Other Geospatial courses in the Department• Advanced GIS: Geob 370• Cartography: Geob 372• Statistics: Geog 374• Advanced Cartography: Geob 472• GIScience in Research: Geob 479
• BCIT• Graduate School• Employment
ALL THE BEST!
Final exam: APR 9 08:30 AM in MCLD 292
http://imgs.xkcd.com/comics/correlation.png
http://maps.ubc.ca/PROD/index_detail.php?show=y,n,n,n,n,y&bldg2Search=n&locat1=312&locat2=#showMapCampushttp://maps.ubc.ca/PROD/index_detail.php?show=y,n,n,n,n,y&bldg2Search=n&locat1=312&locat2=#showMapCampus
Introductory Remote SensingSlide Number 2Slide Number 3Slide Number 4Slide Number 5Slide Number 6Goals of the course What is remote sensing?What is remote sensing?spectral signatures and sensorsCharacteristics of remotely sensed ImageryAerial photographyInfrared ImagerySatellite imagery: Ocean monitoringDrought monitoringDisaster monitoringLight Detection and Ranging LIDARRADAR – Monitoring Sea IceRADAR -- InterferometryThe ‘system’Digital Image ProcessingDigital Image Processing: ClassificationEMR: SourceEMR: AtmosphereObject ReflectanceSensorsDIGITAL IMAGE PROCESSINGUsersSlide Number 30Final examWhat Next?All the best!Slide Number 34