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Dr. Mathias (Mat) Disney UCL Geography Office: 113, Pearson Building

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Presentation on theme: "Dr. Mathias (Mat) Disney UCL Geography Office: 113, Pearson Building"— Presentation transcript:

1 CEGEG046 / GEOG3051 Principles & Practice of Remote Sensing (PPRS) 1: Introduction to Remote Sensing
Dr. Mathias (Mat) Disney UCL Geography Office: 113, Pearson Building Tel:

2 Format of the course Term 1
Radiometric principles and data collection (Disney) Mapping science (Dowman, Iliffe, Haklay, Backes, Smith, Cross) Computing for image analysis (Lewis) Analytical methods (Ziebart, Iliffe) Image processing & GIS (Liu) Organisations (Harris) Global Monitoring of Environment & Security (Muller, Disney,Laxon etc.) Seminars (Thurs afternoons, 5-6 pm dates TBC, room 304 3rd floor Pearson BUT north entrance!)

3 Format of the course Term 2 Term 3 Advanced Modules Research project
Geomatics for coastal zone/Geomatics for ocean management (Oceans 2) (Simons, Morley, Iliffe) Topographic mapping/Terrestrial laser scanning(Backes, Robson) Airborne laser scanning/Digital mapping (Backes, Lewis) Renewable natural resources (Lewis, Wooster) Term 3 Research project

4 Miscellaneous Remote Sensing and Photogrammetry Society
£19 for students + get 1 yr RSE for €83 student meeting Mar 2008, New Forest, organised by Tina Thomson from GE travel bursaries NERC National Centre for Earth Observation (NCEO) involvment in several themes at UCL Solid Earth (Centre for the Observation and Modelling of Earthquakes & GE NERC National Centre for Earth Observation (NCEO Cryosphere (Centre for Polar Observation and Earth Sciences: Carbon Theme (formerly Carbon Centre for Terrestrial Carbon Geography

5 Reading and browsing Remote sensing
Campbell, J. B. (2006) Introduction to Remote Sensing (4th ed), London:Taylor and Francis. Harris, R. (1987) "Satellite Remote Sensing, An Introduction", Routledge & Kegan Paul. Jensen, J. R. (2006, 2nd ed) Remote Sensing of the Environment: An Earth Resource Perspective, Prentice Hall, New Jersey. (Excellent on RS but no image processing). Jensen, J. R. (2005, 3rd ed.) Introductory Digital Image Processing, Prentice Hall, New Jersey. (Companion to above) BUT some available online at Jones, H. and Vaughan, R. (2010, paperback) Remote Sensing of Vegetation: Principles, Techniques, and Applications, OUP, Oxford. Excellent. Lillesand, T. M., Kiefer, R. W. and Chipman, J. W. (2004, 5th ed.) Remote Sensing and Image Interpretation, John Wiley, New York. Mather, P. M. (2004) Computer Processing of Remotely‑sensed Images, 3rdEdition. John Wiley and Sons, Chichester. Rees, W. G. (2001, 2nd ed.). Physical Principles of Remote Sensing, Cambridge Univ. Press. Warner, T. A., Nellis, M. D. and Foody, G. M. eds. (2009) The SAGE Handbook of Remote Sensing (Hardcover). Limited depth, but very wide-ranging – excellent reference book. General Monteith, J. L. and Unsworth, M. H. (1990) ”Principles of Environmental Physics”, 2nd ed. Edward Arnold, London. Hilborn, R. and Mangel, M. (1997) “The Ecological Detective: Confronting models with data”, Monographs in population biology 28, Princeton University Press, New Jersey, USA.

6 Reading and browsing Moodle & www.geog.ucl.ac.uk/~mdisney/pprs.html
Web Tutorials Glossary of alphabet soup acronyms! Other resources NASA NASAs Visible Earth (source of data): European Space Agency earth.esa.int NOAA Remote sensing and Photogrammetry Society UK IKONOS: QuickBird:

7 Lecture outline General introduction to remote sensing (RS), Earth Observation (EO) definitions of RS Why do we do it? Applications and issues Who and where? Concepts and terms remote sensing process, end-to-end

8 What is remote sensing? The Experts say "Remote Sensing is...”
...techniques for collecting image or other forms of data about an object from measurements made at a distance from the object, and the processing and analysis of the data (RESORS, CCRS). ”...the science (and to some extent, art) 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.”

9 What is remote sensing (II)?
The not so experts say "Remote Sensing is...” Advanced colouring-in. Seeing what can't be seen, then convincing someone that you're right. Being as far away from your object of study as possible and getting the computer to handle the numbers. Legitimised voyeurism (more of the same from

10 Remote Sensing Examples
First aerial photo credited to Frenchman Felix Tournachon in Bievre Valley, 1858. Boston from balloon (oldest preserved aerial photo), 1860, by James Wallace Black.

11 Remote Sensing Examples
Kites (still used!) Panorama of San Francisco, 1906. Up to 9 large kites used to carry camera weighing 23kg.

12 Remote Sensing Examples

13 Remote Sensing: scales and platforms
Not always big/expensive equipment Individual/small groups Calibration/validation campaigns

14 Remote Sensing: scales and platforms
Both taken via kite aerial photography

15 Remote Sensing: scales and platforms
upscale upscale Platform depends on application What information do we want? How much detail? What type of detail?

16 Remote Sensing: scales and platforms
E.g. aerial photography From multimap.com Most of UK Cost? Time?

17 Remote Sensing: scales and platforms
upscale Many types of satellite Different orbits, instruments, applications

18 Remote Sensing Examples
Global maps of vegetation from MODIS instrument

19 Remote Sensing Examples
Global maps of sea surface temperature and land surface reflectance from MODIS instrument

20 Remote sensing applications
Environmental: climate, ecosystem, hazard mapping and monitoring, vegetation, carbon cycle, oceans, ice Commercial: telecomms, agriculture, geology and petroleum, mapping Military: reconnaissance, mapping, navigation (GPS) Weather monitoring and prediction Many, many more

21 EO process in summary..... Collection of data
Some type of remotely measured signal Electromagnetic radiation of some form Transformation of signal into something useful Information extraction Use of information to answer a question or confirm/contradict a hypothesis

22 Remote sensing process: I
Statement of problem What information do we want? Appropriate problem-solving approach? In situ: field, lab, ancillary data (Meteorology? Historical? Other?) EO data: Type? Resolution? Cost? Availability? Pre/post processing? Data collection Analog: visual, expert interp. Digital: spatial, photogrammetric, spectral etc. Modelling: prediction & understanding Information extraction Data analysis Products: images, maps, thematic maps, databases etc. Models: parameters and predictions Quantify: error & uncertainty analysis Graphs and statistics Presentation of information Formulate hypothesis Hypothesis testing

23 The Remote Sensing Process: II
Collection of information about an object without coming into physical contact with that object Passive: solar reflected/emitted Active:RADAR (backscattered); LiDAR (reflected)

24 The Remote Sensing Process: III
What are we collecting? Electromagnetic radiation (EMR) What is the source? Solar radiation passive – reflected (vis/NIR), emitted (thermal) OR artificial source active - RADAR, LiDAR

25 Electromagnetic radiation?
Electric field (E) Magnetic field (M) Perpendicular and travel at velocity, c (3x108 ms-1)

26 Energy radiated from sun (or active sensor)
Energy  1/wavelength (1/) shorter  (higher f) == higher energy longer  (lower f) == lower energy from

27 Information What type of information are we trying to get at?
What information is available from RS? Spatial, spectral, temporal, angular, polarization, etc.

28 Spectral information: vegetation
Wavelength, nm 400 600 800 1000 1200 reflectance(%) 0.0 0.1 0.2 0.3 0.4 0.5 very high leaf area very low leaf area sunlit soil NIR, high reflectance Visible green, higher than red Visible red, low reflectance

29 Spectral information: vegetation

30 Colour Composites: spectral
‘Real Colour’ composite Green band on green Red band on red Blue band on blue Approximates “real” colour (RGB colour composite) Landsat TM image of Swanley, 1988

31 Colour Composites: spectral
‘False Colour’ composite (FCC) NIR band on red red band on green green band on blue

32 Colour Composites: spectral
‘False Colour’ composite NIR band on red red band on green green band on blue

33 Colour Composites: temporal
‘False Colour’ composite many channel data, much not comparable to RGB (visible) e.g. Multi-temporal data but display as spectral AVHRR MVC 1995 April August September

34 Temporal information Change detection Rondonia 1975 Rondonia 1986

35 Colour Composites: angular
‘False Colour’ composite many channel data, much not comparable to RGB (visible) e.g. MISR -Multi-angular data (August 2000) 0o; +45o; -45o Real colour composite (RCC) Northeast Botswana

36 Always bear in mind..... when we view an RS image, we see a 'picture’ BUT need to be aware of the 'image formation process' to: understand and use the information content of the image and factors operating on it spatially reference the data

37 Why do we use remote sensing?
Many monitoring issues global or regional Drawbacks of in situ measurement ….. Remote sensing can provide (not always!) Global coverage Range of spatial resolutions Temporal coverage (repeat viewing) Spectral information (wavelength) Angular information (different view angles)

38 Why do we study/use remote sensing?
source of spatial and temporal information (land surface, oceans, atmosphere, ice) monitor and develop understanding of environment (measurement and modelling) information can be accurate, timely, consistent remote access some historical data (1960s/70s+) move to quantitative RS e.g. data for climate some commercial applications (growing?) e.g. weather typically (geo)'physical' information but information widely used (surrogate - tsetse fly mapping) derive data (raster) for input to GIS (land cover, temperature etc.)

39 Caveats! Remote sensing has many problems Can be expensive
Technically difficult NOT direct measure surrogate variables e.g. reflectance (%), brightness temperature (Wm-2  oK), backscatter (dB) RELATE to other, more direct properties.

40 Colour Composites: polarisation
‘False Colour’ composite many channel data, much not comparable to RGB (visible) e.g. Multi-polarisation SAR HH: Horizontal transmitted polarization and Horizontal received polarization VV: Vertical transmitted polarization and Vertical received polarization HV: Horizontal transmitted polarization and Vertical received polarization

41 What sort of parameters are of interest?
Back to the process.... What sort of parameters are of interest? Variables describing Earth system....

42 Information extraction process
Analogue image processing Multi: spectral, spatial, temporal, angular, scale, disciplinary Visualisation Ancillary info.: field and lab measurements, literature etc. Image interpretation Tone, colour, stereo parallax Size, shape, texture, pattern, fractal dimension Height/shadow Site, association Primary elements Spatial arrangements Secondary elements Context Presentation of information Multi: spectral, spatial, temporal, angular, scale, disciplinary Statistical/rule-based patterns Hyperspectral Modelling and simulation After Jensen, p. 22

43 Example: Vegetation canopy modelling
Develop detailed 3D models Simulate canopy scattering behaviour Compare with observations

44 Output: above/below canopy signal
Light environment below a deciduous (birch) canopy 44

45 LIDAR signal: single birch tree
Higher density Allows interpretation of signal, development of new methods 45

46 EO and the Earth “System”
Atmosphere EO and the Earth “System” External forcing Cryosphere Geosphere Biosphere Hydrosphere From Ruddiman, W. F., Earth's Climate: past and future.

47 Example biophysical variables
After Jensen, p. 9

48 Example biophysical variables
Good discussion of spectral information extraction: After Jensen, p. 9

49 Remote Sensing Examples
Ice sheet dynamics Wingham et al. Science, 282 (5388): 456.

50 Electromagnetic spectrum
Zoom in on visible part of the EM spectrum very small part from visible blue (shorter ) to visible red (longer ) ~0.4 to ~0.7m (10-6 m)

51 Electromagnetic spectrum
Interaction with the atmosphere transmission NOT even across the spectrum need to choose bands carefully!

52 Interesting stuff….. ceimaging.com/gallery/zoomify/london_08_08_03/&zoomifyX=0&zoomifyY=0&zoomifyZoo m=10&zoomifyToolbar=1&zoomifyNavWin=1&location=London,%20England


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