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Sensor Types
two basic types, both detect electromagnetic radiation
passive sensors absorb radiation coming from earth, no emission
multispectral and hyperspectral imaging
active sensors emit electromagnetic radiation
RADAR and LiDAR imaging
Passive Sensors
‘optical’ passive satellites capture spectral bands on the visible spectrum, with some capabilities at wavelengths just shorter and longer than visible
typical satellite image (e.g. google maps) is a combo of red, green and blue bands
many optical satellites in orbit
can also use band ratios to figure out things
vegetation (NDVI), snow (NDSI), water (NDWI), sediment, urban areas, etc.
Spectral Band
dataset consisting of one wavelength on the EMS
Optical Satellites
Sentinel deployed by European Space Agency
Landsat deployed by NASA
NDVI
Normalised Difference Vegetation Index (NDVI)
tells you about the density of plants
= (NIR - RED) / (NIR + RED)
NIR = near infrared band, RED = red band
trees absorb visible red light spectrums, increased NDVI means denser vegetation
Active Sensors
RADAR
LiDAR
RADAR
can see through clouds (X-Band, C-Band), also trees depending on wavelength (L-Band)
used for biomass, water, interferometry
Radar Interferometry
radar interferometry combines multiple images to map topography and surface shifts, useful for volcanoes
can measure centimetre scale changes from orbit
LiDAR
Light Detection and Ranging
shoots a laser that bounces back, calculate distance based on speed of light
can shoot many, many points to get a dense ‘point cloud’
used for biomass and topography
can see through trees
Digital Surface Model includes trees, buildings, etc. but Digital Terrain Model only shows earth surface
Research based on global satellite data
Global GHG emissions from biomass estimates, Harris et al 2021
Tidal wetlands mapping,
Changes in live terrestrial biomass
Mass balance of Greenland Ice Sheet