Remote sensing is a technique used to collect data about the earth without taking a physical sample of the earth's surface. A sensor is used to measure the energy reflected from the earth. This information can be displayed as a digital image or as a photograph. Sensors can be mounted on a satellite orbiting the earth, or on a plane or other airborne structure.
| There are two basic types of sensors: passive and active sensors. Passive sensors
record
radiation reflected from, or emitted by, the earth's surface.
The source of this radiation must come from
| ![]() Example of a Passive Sensor |
![]() Example of an Active Sensor |
Active sensors, unlike passive sensors,
require the energy source to come from within the sensor. For example, a
laser remote sensing system is an
active sensor that sends out a beam of light with a known wavelength and frequency. This
beam of
light hits the earth and is reflected back to the sensor, which records the
time it took for the beam of light to return.
For more detailed information on how remote sensing works, proceed to Remote Sensing Fundamentals. |
![]() South Carolina Shoreline Delineated from Aerial Photography |
Coastal Applications |
![]() Sea Surface Temperatures for the Carolina Coast |
Oceanic Applications |
![]() LIDAR Data Used to Map Beachfront Property |
Hazard Assessment |
![]() North Inlet National Estuarine Research Reserve Boundary Overlaid on Satellite Imagery |
Natural Resource Management |