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Merge branch 'SatDump:master' into master
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25
resources/descriptions/124.md
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resources/descriptions/124.md
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# 124
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124, also known as *Cloud RGB*, is an enhancement designed to make clouds stand out more compared to surface features, while keeping the color scheme close to nature and easy to understand even for the general public.
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The name 124 comes from the usage of AVHRR channel 1 (0.862 µm) in the red position, channel 2 (0.63 µm) in the green position, and infrared channel 4 (10.8 µm) in the blue position.
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### Appearance
|
||||
|
||||
Land appears green-bluish tinge (vegetated areas) or green-yellowish tinge (deserts), while sea appears dark purple black.
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||||
Snow and ice appear pale yellow, with melting snow having a more reddish tone
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||||
Mid and low level clouds appear yellow. Thick high level clouds appear white. Thin high-level clouds appear bluish.
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||||
### Intended usage
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||||
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||||
Meteorology (cloud detection and characterization at daytime).
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||||
|
||||
### Limitations
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||||
|
||||
Low level clouds, medium level clouds and snow have similar colors.
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||||
Low contrast between vegetated and desert areas.
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Vegetation information is dependent on temperature.
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### References
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* [EUMETSAT Training Module - Cloud RGB](https://resources.eumetrain.org/data/4/461/navmenu.php?tab=5&page=1.0.0)
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@ -2,6 +2,8 @@
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3b45, also known as *Alternate false color infrared*, is a basic infrared enhancement for night time use. Compared to 543b, it swaps the 12 µm and 3.75 µm channels, providing a different appearance.
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On METEOR-M, the enhancement is called 456 due to the different channel numbering.
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### Appearance
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||||
Land appears in various shades of orange-gray, where more orange tinged colors indicate lower surface temperature.
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resources/descriptions/4221merge.md
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resources/descriptions/4221merge.md
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# 4/221 Merge
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4/221 Merge merges the 10.4 µm infrared channel (Channel 4 on AVHRR) with the regular 221 enhancement.
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It provides increased contrast when compared to the regular 221 enhancement.
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||||
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||||
### Appearance
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||||
|
||||
Land appears yellow (vegetated areas) or gray (deserts), while sea appears deep blue or black.
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Snow and ice appear white, including sea ice.
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Clouds appear white.
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Fog appears violet-white, but is hard to see.
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||||
|
||||
### Intended usage
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||||
|
||||
General purpose imagery at daytime.
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||||
|
||||
### Limitations
|
||||
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||||
Hard to determine the cloud nature.
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||||
Hard to discriminate between cirrus clouds and fog.
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||||
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@ -2,6 +2,8 @@
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|
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543b, also known as *False color infrared*, is a basic infrared enhancement for night time use.
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|
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On METEOR-M, the enhancement is called 654 due to the different channel numbering.
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|
||||
### Appearance
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||||
|
||||
Land appears in various shades of bluish-gray, where darker colors indicate lower surface temperature.
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||||
|
|
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|||
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resources/descriptions/BD.md
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resources/descriptions/BD.md
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# BD
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This enhancement, also called *Hurricane enhancement*, uses a look-up table to highlight certain temperatures in the eye and eye wall of the storm that are known to be related to the intensity of the storm.
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|
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Dvorak (1984) developed a technique for measuring the intensity of these tropical cyclones by comparing the warmest spot within the eye and the warmest cloud top temperature within the cold cloud ring surrounding the eye. The greater that difference, the more intense the tropical cyclone.
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|
||||

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|
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This curve facilitates those estimating tropical cyclone intensity by highlighting the differences between the eye temperature and that of the cold cloud ring by performing severe contrast stretches in both warm and cold portions of the enhancement curve.
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### Appearance
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||||
|
||||
Gray scale.
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||||
|
||||
### Intended usage
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||||
|
||||
Hurricane analysis.
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||||
|
||||
### Limitations
|
||||
|
||||
Unsuitable for smaller tropical storms.
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||||
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resources/descriptions/CC.md
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resources/descriptions/CC.md
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# CC
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This enhancement, also called *Cold climate MB* uses a look-up table to highlight specific cloud top temperatures in thunderstorm systems where there is the highest likelyhood of the strongest precipitations to be occurring. It is similar to the MB enhancement, but is modified for use over colder northern latitudes in winter.
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||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
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||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (thunderstorm analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
Unsuitable for warm climates (use the MD enhancement) or medium latitude climates (use the MB enhancement)
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resources/descriptions/CloudUnderlay.md
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resources/descriptions/CloudUnderlay.md
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# Cloud Underlay
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This enhancement strips only the clouds from the satellite image, and applies them as a layer over a predefined map. This can help to differentiate some cloud types from land in single-band infrared imagery.
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This can be used to provide daytime-like imagery even at night.
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### Appearance
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||||
Clouds appear white.
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Land and sea appear as specified by the map used (by default, a physical map).
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||||
|
||||
### Intended usage
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||||
|
||||
Aesthetical reasons, cloud analysis
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||||
|
||||
### Limitations
|
||||
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||||
Limited scientific value
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||||
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resources/descriptions/ColorGeneralIR.md
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resources/descriptions/ColorGeneralIR.md
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# Color general cloud IR
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This enhancement, uses a look-up table to highlight certain temperatures in the clouds.
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It greatly enhances the contrast in the land/sea regions with respect to the clouds, which are usually hard to see on pure infrared imagery.
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||||
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||||
### Appearance
|
||||
|
||||
Progressively thicker clouds appear in shades of yellow, then orange, and then red.
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||||
Land and sea appear in shades of blue, gray and white.
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||||
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||||
### Intended usage
|
||||
|
||||
Meteorology.
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||||
|
||||
### Limitations
|
||||
|
||||
Not suitable for colder climates.
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||||
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resources/descriptions/DayMicro.md
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resources/descriptions/DayMicro.md
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# Day Microphysics
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The Day Microphysics enhancement makes use of various shades of colors and three spectral bands in the visible and infrared ranges to enable cloud identification and analysis.
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### Appearance
|
||||
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||||

|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (in-depth cloud analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
The large number of colors it can produce make its interpretation hard, especially for inexperienced users.
|
||||
Lower clouds could be obstructed by level clouds.
|
||||
|
||||
### References
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||||
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* [EUMETSAT Training Module - Day Microphysics](https://resources.eumetrain.org/data/4/461/print_3.htm)
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resources/descriptions/EC.md
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resources/descriptions/EC.md
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# EC
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This enhancement, also called *Cool season precipitation* uses a look-up table to highlight specific cloud top temperatures where there is the highest likelyhood of the strongest precipitations, usually snow, to be occurring.
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||||
|
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### Appearance
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||||
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Gray scale.
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||||
|
||||
### Intended usage
|
||||
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||||
Meteorology (precipitation analysis).
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||||
|
||||
### Limitations
|
||||
|
||||
Unsuitable for warm climates.
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||||
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resources/descriptions/HE.md
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resources/descriptions/HE.md
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# HE
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||||
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This enhancement, also called *Western US*, is used principally by weather offices in the western United States.
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It provides good enhancement of a wide variety of cloud types, but is somewhat complex, and may be difficult to use at first.
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|
||||
It enhances low and middle level clouds common along the Pacific Coast of North America in two separate gray shaderanges. The freezing level is easily determined, an advantage for aviation users concerned with icing. Step wedge regions display very cold infrared cloud top temperatures associated with thunderstorms and frontal systems in 5 degree increments down to -60 °C. Two additional "repeat gray" segments define cloud top temperatures colder than -60 °C.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
Hard to use. The HF enhancement is easier to use.
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||||
17
resources/descriptions/HF.md
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resources/descriptions/HF.md
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# HF
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||||
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This enhancement, also called *New western US* is used principally by weather offices in the western United States and is essentially an updated version of the HE enhancement.
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|
||||
It enhances low and middle level clouds common along the Pacific Coast of North America. Step wedge regions display very cold infrared cloud top temperatures associated with thunderstorms and frontal systems in 5 °C increments down to -60 °C. Two additional "repeat gray" segments define cloud top temperatures colder than -60 °C.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
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||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
No specific limitations.
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||||
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resources/descriptions/JF.md
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resources/descriptions/JF.md
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# JF
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This enhancement, also called *simple sea surface/cold cloud*, is a hybrid enhancement scheme used to highlight both sea surface temperatures, and cold cloud tops associated with thunderstorms and other weather systems. It is somewhat simpler to interpret than the later JJ enhancement. The coldest portion of the enhancement (less than -33 °C) is nearly identical to the general use MB enhancement. The maximum enhancement is provided at the warm end (25 to 10 °C) to depict sea surface temperatures and warm low cloudsin tropical and sub-tropical areas.
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||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
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||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
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||||
|
||||
### Limitations
|
||||
|
||||
No specific limitations.
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||||
18
resources/descriptions/JJ.md
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resources/descriptions/JJ.md
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# JJ
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||||
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||||
This enhancement, also called *Sea surface/cold cloud*, is used to highlight both sea surface temperatures, and cold
|
||||
cloud tops associated with thunderstorms and other weather systems. Maximum enhancement is provided at the warm end (23 to 0C) to depict sea surface temperatures and low clouds. The presence of a freezing level break point is important for aviation
|
||||
users interested in icing conditions. Multiple, steep, ramp enhancement ranges provide considerable detail within cold cloud tops such as thunderstorms.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
It is difficult to determine the actual temperatures with any accuracy.
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||||
Hard to use for inexperienced users (use JF instead).
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15
resources/descriptions/MB.md
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resources/descriptions/MB.md
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# MB
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||||
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This enhancement, also called *Thunderstorm*, uses a look-up table to highlight specific cloud top temperatures in thunderstorm systems where there is the highest likelyhood of the strongest precipitations to be occurring.
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||||
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||||
### Appearance
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||||
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||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (thunderstorm analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
Unsuitable for hotter climates (use the MD enhancement) or cold, northern latitude climates (use the CC enhancement)
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||||
18
resources/descriptions/MCIR.md
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resources/descriptions/MCIR.md
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# MCIR
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This enhancement strips only the clouds from the satellite image, and applies them as a layer over a predefined map. This can help to differentiate some cloud types from land in single-band infrared imagery, typical of APT transmissions.
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||||
Compared to the Cloud Underlay, it tries to preserve more cloud data.
|
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|
||||
### Appearance
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||||
Clouds appear white, progressively less transparent as the cloud thickens.
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||||
Land and sea appear as specified by the map used (by default, a physical map).
|
||||
|
||||
### Intended usage
|
||||
|
||||
Cloud analysis on APT.
|
||||
|
||||
### Limitations
|
||||
|
||||
No cloud top temperatures.
|
||||
21
resources/descriptions/MCIR_precip.md
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resources/descriptions/MCIR_precip.md
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# MCIR Rain
|
||||
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||||
This enhancement strips only the clouds from the satellite image, and applies them as a layer over a predefined map. This can help to differentiate some cloud types from land in single-band infrared imagery, typical of APT transmissions.
|
||||
|
||||
After that, it applies the NO enhancement on top.
|
||||
|
||||
### Appearance
|
||||
|
||||
Clouds with progressively higher likelyhood of precipitation, including areas that are already receiving precipitation, appear green, then yellow, then red, and finally black.
|
||||
|
||||
Clouds with no precipitation likelyhood are white or grayish.
|
||||
|
||||
Land and sea appear as specified by the map used (by default, a physical map).
|
||||
|
||||
### Intended usage
|
||||
|
||||
Cloud analysis on APT.
|
||||
|
||||
### Limitations
|
||||
|
||||
No specific limitations.
|
||||
17
resources/descriptions/MD.md
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resources/descriptions/MD.md
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# MD
|
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|
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This enhancement, also called *Warm season MB* or *Warm season thunderstorm*, enhancement is a modification of the MB enhancement scheme. It is intended for warm season use, and provides improved enhancement within the gray "step wedges" that depict "warm top" convection. An additional improvement is better delineation of warm low clouds (30 °C to 7 °C). The middle cloud range is somewhat broader than with MB, and enhancement of details is minimised.
|
||||
|
||||
Otherwise, it is the same as the MB enhancement.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (thunderstorm analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
Unsuitable for colder climates or seasons (use the MB enhancement) or cold, northern latitude climates (use the CC enhancement)
|
||||
21
resources/descriptions/MSA.md
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resources/descriptions/MSA.md
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|
|||
# Cloud Underlay
|
||||
|
||||
This enhancement strips only the clouds from the satellite image, and applies them as a layer over a predefined map. This can help to differentiate some cloud types from land in single-band visible imagery, typical of APT transmissions.
|
||||
|
||||
Compared to the Cloud Underlay, it tries to preserve more cloud data.
|
||||
|
||||
Compared to MCIR, it uses a visible channel (channels 1 or 2 on AVHRR).
|
||||
|
||||
### Appearance
|
||||
|
||||
Clouds appear white, progressively less transparent as the cloud thickens.
|
||||
Land and sea appear as specified by the map used (by default, a physical map).
|
||||
|
||||
### Intended usage
|
||||
|
||||
Aesthetical reasons, cloud analysis on APT at daytime.
|
||||
|
||||
### Limitations
|
||||
|
||||
No cloud top temperatures.
|
||||
Not usable at night.
|
||||
19
resources/descriptions/NDVI.md
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19
resources/descriptions/NDVI.md
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|
|||
# NDVI
|
||||
|
||||
NDVI (Normalized Difference Vegetation Index) is a simple enhancement that enables detection of living vegetation in a particular area.
|
||||
|
||||
The difference of the two channels used by this enhancement (0.62 and 0.863 µm) permits the detection of the Photosynthetically Active Radiation (PAR) band, which is the radiation absorbed by the plants to perform chlorophyllian photosynthesys.
|
||||
|
||||
### Appearance
|
||||
|
||||
Water appears blue.
|
||||
Land with living vegetation appears in progressively darker shades of yellow-green and then green.
|
||||
Deserts appear yellow.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Vegetation analysis, deforestation and desertification monitoring.
|
||||
|
||||
### Limitations
|
||||
|
||||
Cloud dependent.
|
||||
19
resources/descriptions/NO.md
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19
resources/descriptions/NO.md
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|
|||
# NO
|
||||
|
||||
This enhancement, also (improperly) called *Rain* or *Precipitation*, uses a look-up table to highlight certain temperatures in the cloud top that correspond to a higher likelyhood of precipitations.
|
||||
|
||||
It also greatly enhances the contrast in the land/sea regions with respect to the clouds, which are usually hard to see on pure infrared imagery.
|
||||
|
||||
### Appearance
|
||||
|
||||
Clouds with progressively higher likelyhood of precipitation, including areas that are already receiving precipitation, appear green, then yellow, then red, and finally black.
|
||||
|
||||
Land and sea appear in shades of gray.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
No specific limitations.
|
||||
18
resources/descriptions/NOAANatColor.md
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18
resources/descriptions/NOAANatColor.md
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|
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|
|||
# NOAA Natural color
|
||||
|
||||
NOAA Natural Color attempts to provide more lifelike imagery on NOAA satellites that typically do not transmit the 1.62 µm short wave infrared channel used by the *Natural Color* enhancement.
|
||||
|
||||
### Appearance
|
||||
|
||||
Land appears green (vegetated areas) or gray (deserts), while sea appears blue.
|
||||
Clouds appear white.
|
||||
Fog appears whitish-gray.
|
||||
|
||||
### Intended usage
|
||||
|
||||
General purpose imagery at daytime.
|
||||
|
||||
### Limitations
|
||||
|
||||
Hard to determine the cloud nature.
|
||||
Cannot discriminate between cirrus clouds and fog.
|
||||
24
resources/descriptions/NightMicro.md
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24
resources/descriptions/NightMicro.md
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|
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|
|||
# Night Microphysics
|
||||
|
||||
The Night Microphysics enhancement makes use of various shades of colors and three spectral bands in the short wave and long wave infrared to enable night time cloud identification and analysis, including fog discrimination.
|
||||
|
||||
### Appearance
|
||||
|
||||

|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (In-depth cloud and fog analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
The large number of colors it can produce make its interpretation hard, especially for inexperienced users.
|
||||
Can be contaminated by solar light, for example at the terminator.
|
||||
Thin radiation fog is semi-transparent, which can alter pixel colors.
|
||||
The color of cloud free regions varies depending on their temperature, surface type, and the column moisture.
|
||||
Seasonal and diurnal variations.
|
||||
Very cold clouds show yellow noise.
|
||||
|
||||
### References
|
||||
|
||||
* [EUMETSAT Training Module - Night Microphysics](https://resources.eumetrain.org/data/4/461/navmenu.php?tab=2&page=1.0.0)
|
||||
15
resources/descriptions/SST.md
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15
resources/descriptions/SST.md
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|
@ -0,0 +1,15 @@
|
|||
# Sea surface temperatures
|
||||
|
||||
This enhancement uses a land mask to remove ground, two long wave infrared channels (10.8 and 12.4 µm) and an emissivity correction factor to provide a calibrated temperature of the sea surface.
|
||||
|
||||
### Appearance
|
||||
|
||||
Colder temperatures appear violet while warmer temperatures appear orange or red.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Sea surface temperature measurements, sea water currents analysis
|
||||
|
||||
### Limitations
|
||||
|
||||
Cloud dependent.
|
||||
16
resources/descriptions/Snow.md
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16
resources/descriptions/Snow.md
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|
@ -0,0 +1,16 @@
|
|||
# Snow enhancement
|
||||
|
||||
This enhancement emphasizes the presence of snow.
|
||||
|
||||
### Appearance
|
||||
|
||||
Treeless land (grassland, farmland, desert) is rendered tan, snow on treeless land is white, forests without snow are light green, forests with snow are dark green with a greyish white "frosty" tinge, water is grayish blue with warmer water tending toward purple and ice cover showing up as white, low clouds are yellow, and higher clouds range from yellow through green to light blue as cloud height increases (i.e., as cloud temperature decreases).
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology (snowfall, sea ice and glaciers analysis).
|
||||
|
||||
### Limitations
|
||||
|
||||
Cloud dependent.
|
||||
Does not usually work on NOAA POES satellites.
|
||||
19
resources/descriptions/TA.md
Normal file
19
resources/descriptions/TA.md
Normal file
|
|
@ -0,0 +1,19 @@
|
|||
# TA
|
||||
|
||||
The TA curve is a combination of the CA curve (warm portion) and the HD curve (colder portion).
|
||||
|
||||
The linear part of the curve is to improve land/water/low cloud contrast. The coldest part
|
||||
of the curve is in the same temperature ranges that are used for precipitation estimates and
|
||||
tropical storm classifications.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
Not suitable for cold climates.
|
||||
19
resources/descriptions/ThermalCal.md
Normal file
19
resources/descriptions/ThermalCal.md
Normal file
|
|
@ -0,0 +1,19 @@
|
|||
# Thermal Channel
|
||||
|
||||
Automatically selects the thermal infrared (10.8 µm) channel, and applies a color look-up table to make its interpretation easier.
|
||||
|
||||
This enhancement is calibrated in temperature.
|
||||
|
||||
### Appearance
|
||||
|
||||
Colder temperatures appear violet while warmer temperatures appear orange or red.
|
||||
|
||||

|
||||
|
||||
### Intended usage
|
||||
|
||||
General temperature analysis
|
||||
|
||||
### Limitations
|
||||
|
||||
No emissivity compensation.
|
||||
15
resources/descriptions/ZA.md
Normal file
15
resources/descriptions/ZA.md
Normal file
|
|
@ -0,0 +1,15 @@
|
|||
# ZA
|
||||
|
||||
This enhancement, also called *General IR enhancement*, uses a look-up table to increase contrast by saturating the low and high temperature regions where is typically very little information.
|
||||
|
||||
### Appearance
|
||||
|
||||
Gray scale.
|
||||
|
||||
### Intended usage
|
||||
|
||||
Meteorology.
|
||||
|
||||
### Limitations
|
||||
|
||||
No specific limitatiton.
|
||||
BIN
resources/descriptions/img/AVHRRtempscale.png
Normal file
BIN
resources/descriptions/img/AVHRRtempscale.png
Normal file
Binary file not shown.
|
After Width: | Height: | Size: 5 KiB |
BIN
resources/descriptions/img/DayMicro.png
Normal file
BIN
resources/descriptions/img/DayMicro.png
Normal file
Binary file not shown.
|
After Width: | Height: | Size: 77 KiB |
BIN
resources/descriptions/img/Dvorak.png
Normal file
BIN
resources/descriptions/img/Dvorak.png
Normal file
Binary file not shown.
|
After Width: | Height: | Size: 351 KiB |
BIN
resources/descriptions/img/NightMicro.png
Normal file
BIN
resources/descriptions/img/NightMicro.png
Normal file
Binary file not shown.
|
After Width: | Height: | Size: 46 KiB |
BIN
resources/lut/NDVI.png
Normal file
BIN
resources/lut/NDVI.png
Normal file
Binary file not shown.
|
After Width: | Height: | Size: 29 KiB |
28
resources/scripted_compos/amsu_tpw.lua
Normal file
28
resources/scripted_compos/amsu_tpw.lua
Normal file
|
|
@ -0,0 +1,28 @@
|
|||
|
||||
|
||||
function init()
|
||||
return 1 -- Number of channels to output
|
||||
end
|
||||
|
||||
function process()
|
||||
local d1 = 0.754
|
||||
local d2 = -2.265
|
||||
local adj = 0.003
|
||||
|
||||
for x = 0, rgb_output:width() - 1, 1 do
|
||||
for y = 0, rgb_output:height() - 1, 1 do
|
||||
local ch23_8 = get_calibrated_value(0, x, y, true)
|
||||
local ch31_4 = get_calibrated_value(1, x, y, true)
|
||||
local centerPixel = x - rgb_output:width() / 2
|
||||
local theta = (centerPixel / rgb_output:width() * 98) * math.pi / 180
|
||||
local d0 = 8.24 - 2.622*math.cos(theta) + 1.846 * (math.cos(theta))^2
|
||||
|
||||
local result = math.cos(theta)*(d0+d1*math.log(285 - ch23_8)+c2*math.log(285-ch31_4))+c3
|
||||
local output = result / 300
|
||||
set_img_out(0, x, y, output)
|
||||
end
|
||||
|
||||
set_progress(x, rgb_output:width())
|
||||
end
|
||||
end
|
||||
|
||||
31
resources/scripted_compos/ndvi.lua
Normal file
31
resources/scripted_compos/ndvi.lua
Normal file
|
|
@ -0,0 +1,31 @@
|
|||
-- NDVI
|
||||
|
||||
function init()
|
||||
img_lut = image8.new()
|
||||
img_lut:load_png(get_resource_path("lut/NDVI.png"))
|
||||
return 3
|
||||
end
|
||||
|
||||
function process()
|
||||
for x = 0, rgb_output:width() - 1, 1 do
|
||||
for y = 0, rgb_output:height() - 1, 1 do
|
||||
local cch2 = get_calibrated_value(0, x, y, true)
|
||||
local cch1 = get_calibrated_value(1, x, y, true)
|
||||
|
||||
|
||||
|
||||
local ndvi = (cch2-cch1)/(cch2+cch1)
|
||||
|
||||
local ndvi_lutval = ((ndvi-(-1))*256)/(1-(-1))+0
|
||||
|
||||
local lut_result[0] = img_lut:get(0 * img_lut:height() * img_lut:width() + ndvi_lutval) / 255.0
|
||||
local lut_result[1] = img_lut:get(1 * img_lut:height() * img_lut:width() + ndvi_lutval) / 255.0
|
||||
local lut_result[2] = img_lut:get(2 * img_lut:height() * img_lut:width() + ndvi_lutval) / 255.0
|
||||
|
||||
for c = 0, 2, 1 do
|
||||
set_img_out(c, x, y, lut_result[c])
|
||||
end
|
||||
end
|
||||
set_progress(x, rgb_output:width())
|
||||
end
|
||||
end
|
||||
|
|
@ -471,17 +471,19 @@
|
|||
},
|
||||
"3a21": {
|
||||
"equation": "cch3a, cch2, cch1",
|
||||
"description": "descriptions/3a21.md",
|
||||
"description": "descriptions/321.md",
|
||||
"equalize": true,
|
||||
"geo_correct": true
|
||||
},
|
||||
"4/221 Merge": {
|
||||
"equation": "ch1 < 0.065 ? (ch4 - 0.7) * 2.66 : ch2 * 2.2 - 0.15, ch1 < 0.065 ? (ch4 - 0.7) * 2.66 : ch2 * 2.2 - 0.15, ch1 < 0.065 ? (ch4 - 0.7) * 2.66 : ch1 * 2.2 - 0.15",
|
||||
"description": "descriptions/4221merge.md",
|
||||
"geo_correct": true
|
||||
},
|
||||
"NOAA Natural Color": {
|
||||
"equation": "cch2 * 0.6 + min(cch1, cch2) * 0.4, cch2, cch1",
|
||||
"individual_equalize": true,
|
||||
"description": "descriptions/NOAANatColor.md",
|
||||
"geo_correct": true
|
||||
},
|
||||
"Natural Color": {
|
||||
|
|
@ -504,6 +506,7 @@
|
|||
"124": {
|
||||
"equation": "ch1, ch2, ch4",
|
||||
"individual_equalize": true,
|
||||
"description": "descriptions/124.md",
|
||||
"geo_correct": true,
|
||||
"project": {
|
||||
"width": 4096,
|
||||
|
|
@ -517,22 +520,26 @@
|
|||
"Thermal Channel": {
|
||||
"equation": "cch4",
|
||||
"apply_lut": true,
|
||||
"description": "descriptions/ThermalCal.md",
|
||||
"geo_correct": true
|
||||
},
|
||||
"Night Microphysics": {
|
||||
"equation": "cch5-cch4,cch4-cch3b,cch4",
|
||||
"geo_correct": true,
|
||||
"description": "descriptions/NightMicro.md",
|
||||
"individual_equalize": true,
|
||||
"white_balance": true
|
||||
},
|
||||
"Day Microphysics": {
|
||||
"equation": "cch1, cch3a^2.5,cch4",
|
||||
"description": "descriptions/DayMicro.md",
|
||||
"geo_correct": true,
|
||||
"individual_equalize": true
|
||||
},
|
||||
"Clouds Underlay (Merge)": {
|
||||
"channels": "ch4",
|
||||
"lua": "scripted_compos/underlay_with_clouds.lua",
|
||||
"description": "descriptions/CloudUnderlay.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.4,
|
||||
"scalar": 4.0,
|
||||
|
|
@ -544,6 +551,7 @@
|
|||
"Clouds Underlay (Isolate)": {
|
||||
"channels": "ch4",
|
||||
"lua": "scripted_compos/underlay_with_clouds.lua",
|
||||
"description": "descriptions/CloudUnderlay.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.58,
|
||||
"scalar": 4.0,
|
||||
|
|
@ -554,6 +562,7 @@
|
|||
},
|
||||
"Snow enhancement": {
|
||||
"equation": "((3*ch1-ch4)/2)^1.7, ((3*ch1+ch4)/4)^1.7, (ch1-ch3a)^1.7",
|
||||
"description": "descriptions/Snow.md",
|
||||
"individual_equalize": true,
|
||||
"white_balance": true,
|
||||
"geo_correct": true,
|
||||
|
|
@ -561,11 +570,13 @@
|
|||
},
|
||||
"NDVI (Vegetation)": {
|
||||
"equation": "((cch2-cch1)/(cch2+cch1)+1)/2",
|
||||
"description": "descriptions/NDVI.md",
|
||||
"geo_correct": true,
|
||||
"autogen": false
|
||||
},
|
||||
"Sea Surface Temperature": {
|
||||
"channels": "cch4",
|
||||
"description": "descriptions/SST.md",
|
||||
"lua": "scripted_compos/sst_landmask.lua",
|
||||
"lua_vars": {
|
||||
"minval": 0,
|
||||
|
|
@ -593,6 +604,7 @@
|
|||
},
|
||||
"NO enhancement": {
|
||||
"lut": "lut/WXtoImg-NO_mod.png",
|
||||
"description": "descriptions/NO.md",
|
||||
"channels": "ch3b, ch4",
|
||||
"autogen": false,
|
||||
"geo_correct": true,
|
||||
|
|
@ -607,11 +619,13 @@
|
|||
"ZA enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"lut": "lut/WXtoImg-ZA.png",
|
||||
"description": "descriptions/ZA.md",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"MB enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/MB.md",
|
||||
"lut": "lut/WXtoImg-MB.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
|
|
@ -624,54 +638,63 @@
|
|||
},
|
||||
"BD enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/BD.md",
|
||||
"lut": "lut/WXtoImg-BD.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"CC enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/CC.md",
|
||||
"lut": "lut/WXtoImg-CC.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"EC enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/EC.md",
|
||||
"lut": "lut/WXtoImg-EC.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"HE enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/HE.md",
|
||||
"lut": "lut/WXtoImg-HE.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"HF enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/HF.md",
|
||||
"lut": "lut/WXtoImg-HF.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"JF enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/JF.md",
|
||||
"lut": "lut/WXtoImg-JF.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"JJ enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/KJ.md",
|
||||
"lut": "lut/WXtoImg-JJ.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"TA enhancement": {
|
||||
"channels": "ch3b, ch4",
|
||||
"description": "descriptions/TA.md",
|
||||
"lut": "lut/WXtoImg-TA.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true
|
||||
},
|
||||
"Color general cloud IR": {
|
||||
"channels": "cch4, cch4",
|
||||
"description": "descriptions/ColorGeneralIR.md",
|
||||
"lut": "lut/Multispectral.png",
|
||||
"autogen": false,
|
||||
"geo_correct": true,
|
||||
|
|
@ -714,6 +737,7 @@
|
|||
"Clouds Underlay": {
|
||||
"channels": "chb",
|
||||
"lua": "scripted_compos/underlay_with_clouds.lua",
|
||||
"description": "descriptions/CloudUnderlay.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.58,
|
||||
"scalar": 4.0,
|
||||
|
|
@ -725,6 +749,7 @@
|
|||
"MCIR": {
|
||||
"channels": "chb",
|
||||
"lua": "scripted_compos/underlay_with_clouds.lua",
|
||||
"description": "descriptions/MCIR.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.35,
|
||||
"scalar": 2.5,
|
||||
|
|
@ -741,6 +766,7 @@
|
|||
"MSA": {
|
||||
"channels": "cha",
|
||||
"lua": "scripted_compos/underlay_with_clouds.lua",
|
||||
"description": "descriptions/MSA.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.02,
|
||||
"scalar": 2.0,
|
||||
|
|
@ -757,6 +783,7 @@
|
|||
"MCIR Rain": {
|
||||
"channels": "cha, chb",
|
||||
"lua": "scripted_compos/underlay_with_clouds_lut.lua",
|
||||
"description": "descriptions/MCIR_precip.md",
|
||||
"lua_vars": {
|
||||
"minoffset": 0.2,
|
||||
"scalar": 1.5,
|
||||
|
|
@ -787,61 +814,73 @@
|
|||
},
|
||||
"NO enhancement": {
|
||||
"lut": "lut/WXtoImg-NO_mod_APT.png",
|
||||
"description": "descriptions/NO.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"ZA enhancement": {
|
||||
"lut": "lut/WXtoImg-ZA.png",
|
||||
"description": "descriptions/ZA.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"MB enhancement": {
|
||||
"lut": "lut/WXtoImg-MB.png",
|
||||
"description": "descriptions/MB.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"MD enhancement": {
|
||||
"lut": "lut/WXtoImg-MD.png",
|
||||
"description": "descriptions/MD.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"BD enhancement": {
|
||||
"lut": "lut/WXtoImg-BD.png",
|
||||
"description": "descriptions/BD.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"CC enhancement": {
|
||||
"lut": "lut/WXtoImg-CC.png",
|
||||
"description": "descriptions/CC.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"EC enhancement": {
|
||||
"description": "descriptions/EC.md",
|
||||
"lut": "lut/WXtoImg-EC.png",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"HE enhancement": {
|
||||
"lut": "lut/WXtoImg-HE.png",
|
||||
"description": "descriptions/HE.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"HF enhancement": {
|
||||
"lut": "lut/WXtoImg-HF.png",
|
||||
"description": "descriptions/HF.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"JF enhancement": {
|
||||
"lut": "lut/WXtoImg-JF.png",
|
||||
"description": "descriptions/JF.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"JJ enhancement": {
|
||||
"lut": "lut/WXtoImg-JJ.png",
|
||||
"description": "descriptions/JJ.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
},
|
||||
"TA enhancement": {
|
||||
"lut": "lut/WXtoImg-TA.png",
|
||||
"description": "descriptions/TA.md",
|
||||
"channels": "cha, chb",
|
||||
"autogen": false
|
||||
}
|
||||
|
|
@ -941,10 +980,12 @@
|
|||
"221": {
|
||||
"equation": "ch2, ch2, ch1",
|
||||
"geo_correct": true,
|
||||
"description": "descriptions/221.md",
|
||||
"equalize": true
|
||||
},
|
||||
"321": {
|
||||
"equation": "ch3, ch2, ch1",
|
||||
"description": "descriptions/321.md",
|
||||
"geo_correct": true,
|
||||
"project": {
|
||||
"width": 4096,
|
||||
|
|
@ -958,16 +999,19 @@
|
|||
},
|
||||
"124": {
|
||||
"equation": "ch1, ch2, ch4",
|
||||
"description": "descriptions/124.md",
|
||||
"geo_correct": true,
|
||||
"individual_equalize": true
|
||||
},
|
||||
"Natural Color": {
|
||||
"equation": "((0.5*max(ch4,min(ch2,ch1)) + 0.5*ch2)+0.3*ch3)*0.85, ch2, ch1",
|
||||
"description": "descriptions/NatColor.md",
|
||||
"geo_correct": true,
|
||||
"white_balance": true
|
||||
},
|
||||
"Thermal Channel": {
|
||||
"equation": "1 - ch5",
|
||||
"description": "descriptions/ThermalUncal.md",
|
||||
"individual_equalize": true,
|
||||
"geo_correct": true,
|
||||
"project": {
|
||||
|
|
@ -982,22 +1026,26 @@
|
|||
},
|
||||
"Day Microphysics": {
|
||||
"equation": "ch1, ch4^2.5, ch5",
|
||||
"description": "descriptions/DayMicro.md",
|
||||
"individual_equalize": true,
|
||||
"geo_correct": true
|
||||
},
|
||||
"Night Microphysics": {
|
||||
"equation": "ch6-ch5, ch5-ch4, ch5",
|
||||
"description": "descriptions/NightMicro.md",
|
||||
"individual_equalize": true,
|
||||
"geo_correct": true
|
||||
},
|
||||
"654": {
|
||||
"equation": "1 - ch6, 1 - ch5, 1 - ch4",
|
||||
"description": "descriptions/543b.md",
|
||||
"individual_equalize": true,
|
||||
"geo_correct": true,
|
||||
"autogen": true
|
||||
},
|
||||
"456": {
|
||||
"equation": "1 - ch4, 1 - ch5, 1 - ch6",
|
||||
"description": "descriptions/3b45.md",
|
||||
"individual_equalize": true,
|
||||
"geo_correct": true,
|
||||
"autogen": true
|
||||
|
|
@ -1005,6 +1053,7 @@
|
|||
"NO enhancement": {
|
||||
"lut": "lut/WXtoImg-NO_mod_meteor.png",
|
||||
"channels": "ch4, ch5",
|
||||
"description": "descriptions/NO.md",
|
||||
"autogen": true,
|
||||
"geo_correct": true,
|
||||
"individual_equalize": true,
|
||||
|
|
|
|||
Loading…
Add table
Add a link
Reference in a new issue