ZA NOAA general purpose meteorological IR enhancement option. Increases contrast by saturating the very low and very high temperature regions where there is typically very little information. This enhancement option is temperature normalised.
MB NOAA cold cloud top enhancement option. Useful for showing where the strongest rainfall is occurring in thunderstorms. This enhancement option is temperature normalised.
MD NOAA MD enhancement is a modification of the popular, general use 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 (30C to 7C). The middle cloud range is somewhat broader than the MB, and enhancement of details is minimised. Otherwise, it is the same as the MB enhancement. This enhancement option is temperature normalised.
BD NOAA hurricane enhancement option. Highlights certain temperatures in the eye and eye wall of the storm system which are known to be related to the intensity of the hurricane. This enhancement option is temperature normalised.
CC NOAA CC enhancement curve. This enhancement option is temperature normalised.
HE The NOAA HE enhancement is used principally by weather offices in the western United States. It provides good enhancement of a wide variety of cloud types, but is somewhat complex, and may be difficult to use at first. It enhances low and middle level clouds common along the Pacific Coast of North America in two separate gray shade ranges. 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 -60C. This enhancement option is temperature normalised.
HF The NOAA HF enhancement is the most current of the "H" series of enhancements, and is used principally by weather offices in the western United States. It provides good enhancement of 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 degree increments down to -60 C. Tw o additional "repeat gray" segments define cloud top temperatures colder than -60C. This enhancement option is temperature normalised.
JF The NOAA JF enhancement 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 -33C) is nearly identical to the general-use MB enhancement. Maximum enhancement is provided at the warm end (25 to 10C) to depict sea surface temperatures and warm low clouds in tropical and subtropical areas. This enhancement option is temperature normalised.
JJ The NOAA JJ enhancement 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, but it is difficult to determine the actual temperatures with any accuracy. This enhancement option is temperature normalised.
LC The NOAA LC curve is used on images from the 3.9 micron shortwave infrared channel (CH2) of GOES. It provides maximum enhancement in the temperature range where fog and low clouds typically occur (36C to -9C). Another enhanced thermal range is from -10C to -29C, the region of precipitation generation in mid latitude weather systems. Since CH2 is sensitive to "hot spots," a steep, reverse ramp is found at the warm end (68C to 50C) to show any observable fires as white. There is no enhancement at the very cold end (-30 to -67C), due to the instrument noise normally present at these temperatures. This enhancement option is temperature normalised.
TA NOAA TA enhancement curve. This enhancement option is temperature normalised.
WV The modified NOAA WV curve is used for the 6.7 micron water vapor channel (CH3) on GOES. The only temperature range that is enhanced is between -5C and -90C. Temperatures colder than -90C are shown as white, and temperatures warmer than -5C are displayed as black. This enhancement option is temperature normalised. (See also WV-old).
NO NOAA colour IR contrast enhancement option. Greatly increases contrast in the darker land/sea regions and colours the cold cloud tops. Allows fine detail in land and sea to be seen and provides a very readable indication of cloud top temperatures. This enhancement option is temperature normalised.
MCIR Colours the NOAA sensor 4 IR image using a map to colour the sea blue and land green. High clouds appear white, lower clouds gray or land/sea coloured, clouds generally appear lighter, but distinguishing between land/sea and low cloud may be difficult. Darker colours indicate warmer regions.
MSA[:SeaToLand[:LandToCloud[:ColdRegion]]] Multispectral analysis. Uses a NOAA channel 2-4 image and determines which regions are most likely to be cloud, land, or sea based on an analysis of the two images. Produces a vivid false-coloured image as a result. This enhancement takes up to three options separated from the enhancement name by colons. The first option is the sea to land adjustment. The default value is 50 with the valid range being 0 to 100. This should be decreased if land appears blue, and increased if water appears green. The second option is the land to cloud adjustment. The default value is 50 with the valid range being 0 to 100. This should be decreased if cloud appears green and increased if land appears gray or white. The final option should be 0 to indicate warm or summertime analysis or 1 to indicate there are large cold regions. Note that perfect colouring is difficult to obtain, especially with low illumination angles. This enhancement does not use a palette nor is it
temperature normalised.
MSA-precip[:SeaToLand[:LandToCloud[:ColdRegion]]] Same as MSA multispectral analysis, but high cold cloud tops are coloured the same as the NO enhancement to give an approximate indication of the probability and intensity of precipitation.
HVC Creates a false colour image from NOAA APT images based on temperature using the HVC colour model. Uses the temperature derived from the sensor 4 image to select the hue and the brightness from the histogram-equalised other image to select the value and chroma. The HVC colour model attempts to ensure that different colours at the same value will appear to the eye to be the same brightness and the spacing between colours representing each degree will appear to the eye to be similar. Bright areas are completely unsaturated in this model. The palette used can be changed using the -P option.
HVCT Similar to HVC (below), but with blue water and with colours more indicative of land temperatures. The palette used can be changed using the -P option. sea Creates a false colour image from NOAA APT images based on sea surface temperature. Uses the sea surface temperature derived from just the sensor 4 image to colour the image. Land appears black and cold high cloud will also appear black. The sea surface temperature may be incorrect due to the presence of low cloud, or of thin or small clouds in the pixel evaluated, or from noise in the signal. The palette used can be changed using the -P option.
therm Produces a false colour image from NOAA APT images based on temperature. Provides a good way of visualising cloud temperatures. The palette used can be changed using the -P option.
sea Creates a false colour image from NOAA APT images based on sea surface temperature. Uses the sea surface temperature derived from just the sensor 4 image to colour the image. Land appears black and cold high cloud will also appear black. The sea surface temperature may be incorrect due to the presence of low cloud, or of thin or small clouds in the pixel evaluated, or from noise in the signal. The palette used can be changed using the -P option.