remote sensing

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Remote sensing what is it? Observation from a distance Aerial photographs- very detailed Satellite images – global view

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Basic introduction to remote sensing

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Page 1: Remote sensing

Remote sensing what is it?

• Observation from a distance– Aerial photographs- very detailed– Satellite images – global view

Page 2: Remote sensing

Oblique aerial photograph

• Viewed from an oblique angle: looking sideways

• Looks natural, easy to understand, useless for measurement purposes

Page 3: Remote sensing

Vertical aerial photograph

• Viewed straight down giving a “map view”• Difficult to understand at first. Can be used

as a basis of mapping, after image has been rectified

Page 4: Remote sensing

Aerial photographs: 1995 and 1972

Page 5: Remote sensing

Map derived form aerial photographs

• Visible features are “digitised” by tracing around them on a computer screen.

• This creates the points lines and polygon symbols which build up into the map

Page 6: Remote sensing

Stereo-photography 3-d visualisation

overlap

Photo 1 Photo 2Plane travels at constant altitude above sea level. Height above ground varies with topography

60% of image

• Overlapping aerial photographs can be used to build 3-d stereoscopic visual models. These can be used to map out contours and heights of features

Page 7: Remote sensing

Stereoscopic reconstruction of overlapping areas

overlap

Photo 1 Photo 2

Right eye Left eye

• A stereoscope is used to view the overlapping areas simultaneously and the brain builds a 3-d model of the landscape where the images overlap.

Page 8: Remote sensing

Digital manipulation of aerial photographs

• 3-d models can also be built by “digitally draping” photographs over a digital elevation model of the landscape.

Page 9: Remote sensing

Satellite Remote Sensing

• Satellites give a higher viewpoint and give unrestricted coverage of the whole globe

Link to Gateway Remote sensing videohttp://gateway.rac.ac.uk/mod/resource/view.php?id=3937

Page 10: Remote sensing

Satellite orbits

• Geostationary orbit: above the equator, 35,000 km height, orbital period 24 hours. Satellites appear fixed in sky

• Low Earth orbit, usually polar, orbital period can be less than 1 hour. Satellites seen to move across sky

Page 11: Remote sensing

Geo-stationary meteorological satellite: Meteosat

Infra-red image from 0600March 8, 2000

“Ground” position of satellite

• Geostationary orbits, approx 33,000 km elevation over the equator. Satellite takes 24hours for one orbit, the earth rotates once in that time, so the satellite appears stationary in the sky

Page 12: Remote sensing

Polar orbiting meteorological satellites

• Polar orbiting satellites cover the whole globe, but move, so there are long time intervals between one image and the satellites next return

Page 13: Remote sensing

Earth observation satellites: Landsat 7 image (30m resolution)

• Earth observation satellites are designed to view the surface of the globe. Some are designed for view the oceans, others, like the Landsat series, observe the land

Page 14: Remote sensing

2004 tsunami: Aceh province, Sumatra

Page 15: Remote sensing
Page 16: Remote sensing

Land classification; spectral signatures: Using SPOT images

• Simultaneous Multi-spectral images can be used to classify landcover.

• The reflectance of certain landcover types are measured on each image to build up a signature of that type of cover. This is then searched for over the whole image

Page 17: Remote sensing

Land classification; spectral signatures: Using SPOT images

• Simultaneous Multi-spectral images can be used to classify landcover.

• The reflectance of certain landcover types are measured on each image to build up a signature of that type of cover. This is then searched for over the whole image

Page 18: Remote sensing

Land classification; spectral signatures: Using SPOT images

• Simultaneous Multi-spectral images can be used to classify landcover.

• The reflectance of certain landcover types are measured on each image to build up a signature of that type of cover. This is then searched for over the whole image

Page 19: Remote sensing

Land classification; spectral signatures: Using SPOT images

• Simultaneous Multi-spectral images can be used to classify landcover.

• The reflectance of certain landcover types are measured on each image to build up a signature of that type of cover. This is then searched for over the whole image

Page 20: Remote sensing

Remote sensing images:

Harnhill farm

Page 21: Remote sensing

Aerial photograph, 2011 Spatial resolution approx. 0.2m

Page 22: Remote sensing

GoogleMaps aerial photo, Spatial resolution approx. 1.5m

Page 23: Remote sensing

Scanned Aerial photograph, 1995 Spatial resolution approx. 2.0m

Page 24: Remote sensing

Landsat 5 image, circa 2001 Spatial resolution approx. 30m

Page 25: Remote sensing

LIDAR image, 2011 Spatial resolution approx. 1.0mVertical resolution approx. 0.001m

Page 26: Remote sensing

Landsat 5: 30m resolution

• Landsat 5 image of Gloucestershire (Landsat 6 crashed on take off. Landsat 7 is current satellite, Landsat 8 has just been launched)

Harnhill

Gloucester

Swindon

Cheltenham

Page 27: Remote sensing

Ikonos: 1m resolution

• Commercial panchromatic image at 1m resolution. On the original image people can be seen walking in Horse Guards Parade and the spokes of the London Eye are visible

Page 28: Remote sensing

Ikonos agricultural image 1m resolution

• Another Ikonos image showing the detail available in an agricultural image, here form Montana

• How useful is this for farmers?

Page 29: Remote sensing

RADARSAT classified image of Flevoland, NL

• Radar, “active remote sensing”, sees through clouds and in the dark. This addresses some of the major problems with “Passive remote sensing” which measures reflected sunlight.

• The images are very difficult to interpret

Page 30: Remote sensing

RADARSAT-Mozambique floods

• Shuttle borne radar image of the Mozambique floods• Radar is good at detecting the edge of water bodies,

which it can “see” through cloud cover

Page 31: Remote sensing

Remote sensing summary

• Aerial photography gives us a controllable, highly detailed view of the Earth

• Satellite imagery gives global, unrestricted views which are repeated a frequent intervals

• The references to actions such as “interpretation” and “classification” lead on to things we can do with a geographic information system (GIS) using remote sensing as a source of data