Technology
Applications
- Maritime Weather Monitoring and Prediction
- Navigational Improvements
- Hydrography
- Fisheries -- Food from the Sea
- Coastal Engineering
- Coastal Hydrology
- Sea Ice Prediction and Tracking
- Data Transmission
Devices
The two most efficient types of underwater remote sensing are categorized as platforms and sensors.
I. Platforms
- Fixed Platforms
- Consist of towers and platforms fixed on the ocean floor
- Used to acquire long-term measurements in locations where mobile platforms would be impractical
- Floating Platforms
- First method used to apply remote sensing to oceanography
- Consists of ships and buoys with cameras and IR radiation thermometers to study surface characteristics.
- Early data collected consisted of the air-sea exchange across the surface.
- Balloons
- Used in most ocean operations.
- Cheap, compact, reliable way allowing measuring from above the ocean surface.
- Responsible for finding archaeological sites shallow waters. How? By observing anomalous patterns against the sea floor from balloons towed by research vessels.
- Moored balloons are often used to provide measurements over periods.
- Airships (blimps)
- As a measurement device, when useful for low speed, endurance, and good payload capability are wanted.
- Few are used due to low quantity in existence.
- Aircraft
- Most common device used to apply remote sensing to measurement of oceanographic aspects.
- Used for aerial survey, sensors test for spacecraft platforms.
- Spacecraft
- Provide rapid coverage of an area on a real-time basis.
- During the 1960's, unmanned weather satellites were not specifically used to produce oceanographic data but much of the data collected has been used in studies of the oceans.
- During the 1970's, manned and unmanned earth-orbiting satellites collected data concerning overall pollution of the plant.
- The future includes specific ocean-oriented sensors in orbit.
II. Sensors
- Passive Sensors
- Ultraviolet Band
- Not commonly used.
- Usually combined with UV (ultraviolet) with visual and IR (infrared) bands.
- Visible Band
- Largest class of imagery.
- Primarily used by cameras and photographic emulsions.
- Infrared Spectrum
- Measures heat fluxes above, at, and beneath the sea-air surface.
- Used by imager (produces imagery mapping of the ocean surface with thermal contours) and radiometer-spectrometers (provides values of apparent temperature of the surface at points across the ocean).
- Microwave Spectrum
- Used to measures temperature, surface brightness (index to wind and wave action), and salinity (relationship of salt-to-water content) of the ocean,
- Not affected by high altitudes or poor weather.
- Active Sensors
- Lasers
- Can collect accurate altitude information for geophysical measurements such as the slope of the ocean surface, and wave height measurements.
- Also, can be used to identify materials, such as oils and sediments, at the sea surface.
- Radars
- Used to measure phenomena, such as coastal features, river outflows, surface boundaries, fish schooling, and waves.
- Can be used during all types of weather (at which passive sensors would be rendered ineffective).
Adapted from Lintz, Joseph, Remote Sensing of Environment, Addison-Wesley, Reading, MA, 1976.