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INTRODUCTORY REMOTE SENSING
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INTRODUCTORY REMOTE SENSING€¦ · • Overview of basics of remote sensing: • Electromagnetic spectrum, spectral responses of objects (e.g., trees, houses, crops) • Platforms/Sensors:

Jan 25, 2021

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  • 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