Remote sensing is the acquisition of information about an object without physical contact.
This term is mostly in contrast to on-site observation.
Categories
Source of radiation:
- Passive remote sensing: record emitted or reflected radiation, typically sunlight.
- Active remote sensing: emit signal from aircraft or satellites and measure reflected radiation
Type of radiation:
- visible light: CCD (Charge-coupled device, 感光耦合组件)
- Infrared
- Sonar: (passive) vessel, animal; (active) underwater objects
- Ultrasound sensor: (active) sea level, tide
radiometer
radar altimeter: seafloor, ocean wave height and wavelength
Photogrammetry
Photogrammetry (摄影测量法) is a traditional and less sophisticated method of remote sensing, compared to satellite imagery.
Private vendors: Pictometry (Southwest US, ~95 aircrafts)
Drones have been used for photogrammetry in recent years.
Types and uses:
- Orthophoto: for measurement and map making;
- Oblique image: for (human) validation.
- Stereophotogrammetry: topographic maps (地形图), rapid 3D mapping (Saab Group)
Earth Observation Satellite
Earth observation (EO) is the acquisition of satellite imagery of Earth.
Instrumentation technology and applications:
-
Radar (radio detection and ranging, 雷达):
- aerial traffic control (speed limit enforcement),
- large scale meteorological data (precipitation, wind velocity)
-
LiDAR (light detection and ranging, 光学雷达):
- weapon ranging (测距), laser-homing projectiles (激光自动寻的导弹),
- vegetation, chemical concentration in the atmosphere
-
InSAR (interferometric synthetic aperture radar, 干涉合成孔径雷达):
- precise, large-scale digital elevation model, land cover and land use
Data processing
Data resolutions:
- Single band
- spatial: meter per pixel, 1 ~ 1000;
- radiometric: bit, 8 ~ 14; [256 ~ 16384 levels]
- Spectral: μm per band, 0.10 ~ 2.1; [visible spectrum 0.39 ~ 0.70 μm]
- Temporal: for time-series studies, cloud-averaged image for deforestation and mapping.
Corrections:
- Georeference: matching points on image to established benchmark
- Radiometric correction: convert monochromatic scale to radiance values
- Topographic correction: recover reflectivity in horizontal conditions from terrain-affected radiance values
- Atmospheric correction: transform gray-scale value to eliminate atmospheric haze
Data processing levels†:
- Level 0: Raw data
- Level 1: Reconstructed data
- (1a): Unprocessed data at full instrument resolution, time-referenced and annotated with ancillary information, including radiometric and geometric calibration coefficients and georeferencing parameters
- (1b): Level 1a data processed to sensor units
- Level 2: Derived geophysical variables, at full instrument resolution.
- Level 3: Variables mapped on uniform space-time grid scales.
Level 1 data is the most fundamental record with significant scientific utility.
Level 2 data is the first directly usable data for most scientific applications, variables including ocean wave height, soil moisture, ice concentration, etc.
Level 3 data is smaller and have regular spatial and temporal organization.
† As defined by NASA and EUMETSAT
Earth Observation Data Products
See the main article about Earth Observation Data Products.
Elevation Models:
- Digital elevation model (DEM)
- Digital surface model (DSM)
- Orthorectified radar intensity images (ORI)
🏷 Category=Geographic Information System