chapter 4: Meteorological Satellite Instumentation Flashcards
define passive radiometers
- The instruments flown on-board the satellites measure electromagnetic energy that is either reflected or emitted by our planet
- An instrument that quantitatively measures the intensity of electromagnetic radiation in some bands (wavelength regions) within the spectrum.
basic elements of a radiometer
The optics, detectors, and electronics
Optics:
collect the radiation, separate or disperse the spectral components, and focus the radiation to a field stop.
Detectors:
located behind the field stop, respond to the photons with a voltage signal.
electronics
That voltage signal is amplified by the electronics and converted into digital counts.
Usually, a radiometer is further identified by
the portion of the spectrum it covers
Usually, a radiometer is further identified by the portion of the spectrum it
covers; for example:
- visible (0.4 – 0.7 um),
- infrared (0.7 to 3.0 um – reflected IR and 3.0 to 100um – thermal IR), or
- microwave (1 mm to 1 m).
Earth emitted radiation is detected in
several spectral regions by radiometers where the spectral separation through one of the following approaches.
Earth emitted radiation is detected in several spectral regions by radiometers
where the spectral separation through one of the following approaches.
- Prisms separate the incoming radiation as refraction changes with wavelength (bending angle depends on index of refraction that is a function of wavelength; longer wavelengths are deflected less)
- Band pass filters, using internal reflections within the filter, can separate the infrared spectrum into roughly 20 cm-1 segments.
- Grating spectrometers and interferometers which are capable of spectral resolutions (λ/Δλ) of about 1/1000 also have been used for remote sensing of the earth.
There are two common types of radiometers:
imagers and sounders
Imagers:
A radiometer that has a scanning capability to provide a twodimensional array of pixels from which an image may be produced.
The imagers are utilized in satellite meteorology in two ways:
- To measure the amount of visible light from the sun reflected back to space by the earth’s surface or by clouds, to produce visible imagery.
- Visible images are the same thing we would see with our naked eye and require daylight.
- To measure the amount of infrared radiation emitted by the earth’s surface or by clouds, to produce ir imagery
- Infrared images depend on the amount of radiation an object emits. The obvious advantage to having infrared capability is that weather systems can be monitored both day and night.
Sounders:
measure the infrared radiation, emitted by:
- the earth’s surface or
- by clouds,
provide:
- vertical profiles of temperature,
- pressure,
- water vapor and
- critical trace gases in the earth’s atmosphere
The detail visible in an image is dependent on
- the spatial resolution of the sensor and
- refers to the size of the smallest possible feature that can be detected.
Spatial resolution of passive sensors (we will look at the special case of
active microwave sensors later)
Spatial resolution of passive sensors (we will look at the special case of active microwave sensors later) depends primarily on their
Instantaneous Field of View (IFOV)
The IFOV is
the angular cone
- (A) of visibility of the sensor and determines the area
- (B) on the Earth’s surface which is “seen” from a given altitude at one particular moment in time.
- The size of the area viewed is determined by multiplying the IFOV by the distance (C) from the ground to the sensor.
resolution cell
This area on the ground is called the resolution cell and determines a sensor’s maximum spatial resolution.
For a homogeneous feature to be detected
its size generally has to be equal to or larger than the resolution cell.
For a homogeneous feature to be detected, its size generally has to be equal to or larger than the resolution cell.
If the feature is smaller than this
it may not be detectable as the average brightness of all features in that resolution cell will be recorded.
Spectral resolution describes
the ability of a sensor to define fine wavelength intervals
The finer the spectral resolution, the
narrower the wavelength range for a particular channel or band
multi-spectral sensors
Many remote sensing systems record energy over several separate wavelength ranges at various spectral resolutions
hyperspectral sensors
Advanced multi-spectral sensors that detect hundreds of very narrow spectral bands throughout the visible, near-infrared, and midinfrared portions of the electromagnetic spectrum.
Advanced multi-spectral sensors called hyperspectral sensors, detect hundreds of very narrow spectral bands throughout the visible, near-infrared, and midinfrared portions of the electromagnetic spectrum.
Their very high spectral resolution facilitates
fine discrimination between different targets based on their spectral response in each of the narrow bands.
The radiometric resolution of an imaging system describes
its ability to discriminate very slight differences in energy.
The finer the radiometric resolution of a sensor, the
more sensitive it is to detecting small differences in reflected or emitted energy.
Imagery data are represented by
positive digital numbers which vary from 0 to a selected power of 2
Imagery data are represented by positive digital numbers which vary from 0 to a selected power of 2. This range corresponds to
the number of bits used for coding numbers in binary format.
Each bit records
an exponent of power 2 (e.g. 1bit=21=2)
Each bit records an exponent of power 2 (e.g. 1bit=21 =2). The maximum number of brightness levels available depends on
the number of bits used in representing the energy recorded.
Thus, if a sensor used 8 bits to record the data, there would be
28 =256 digital values available, ranging from 0 to 255. However, if only 4 bits were used, then only 24=16 values ranging from 0 to 15 would be available. Thus, the radiometric resolution would be much less.
Thus, the difference in the level of detail discernible (visible) depends on
the radiometric resolution
Many electronic remote sensors acquire data using scanning systems, which
employ a sensor with a narrow field of view (i.e. IFOV) that sweeps over the terrain to build up and produce a two-dimensional image of the surface.
multispectral scanner (MSS)
A scanning system used to collect data over a variety of different wavelength ranges
There are two main modes of scanning:
across-track and along-track scanning.
Across-track scanners
scan the Earth in a series of lines. The lines are oriented perpendicular to the direction of motion of the sensor platform (i.e. across the swath).