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Announcement: Please visit out new web application, SLIDER, for every pixel of real-time GOES-16 and Himawari-8 imagery.

True Color Imagery

Fig. 1. Example of True Color imagery over parts of Florida, Cuba, and the Bahamas as collected by NASA’s MODerate-resolution Imaging Spectroradiometer (MODIS) sensor. Cyan/aquamarine colors are shallow water sand banks and reef structures. True Color provides a depiction of Earth that is similar to what normal human vision would observe from space. The GOES-R Advanced Baseline Imager (ABI) will be able to produce imagery of similar quality but at dramatically higher temporal refresh (minutes, vs. the 1-2 times per day currently available from the MODIS Terra + Aqua tandem).

1) Product Information:

- Who is developing and distributing this product?

The Cooperative Institute for Research in the Atmosphere (CIRA) in Fort Collins, Colorado, the Cooperative Institute for Meteorological Satellite Studies (CIMSS) in Madison, Wisconsin, and the Naval Research Laboratory (NRL) in Monterey, California are developing and distributing the Simulated True Color product.

- Who is receiving this product, and how?

The Simulated True Color products are sent to the National Weather Service (NWS) Regional Headquarters from which they are distributed to Weather Forecast Offices (WFOs) for display on their local AWIPS systems. Imagery updates are available approximately two times per day from the MODIS sensors on board Terra (~10:30 AM local time) and Aqua (~1:30 PM local time).

- What is the product size?

The size of Simulated True Color product images is determined by the span and resolution of the AWIPS domain itself. Since current AWIPS system displays accommodate 1-byte per pixel, a good rule of thumb is that the size of the imagery (in bytes) corresponds roughly to the total number of pixels in a given AWIPS domain. For example, an AWIPS domain having dimensions of 1000 x 1000 pixels will require approximately 1 Megabyte (~106 bytes).

2) Product Description:

Fig. 2. The example above illustrates some of the benefits of true color imagery for a scene over Southern California. While single-band visible imagery (left) provides a good depiction of the marine stratocumulus clouds offshore and the inland convection, true color (right) provides additional detail of blue Pacific, green farmland and vegetated terrain, tan deserts, and the gray urban zones along the coast.

- Purpose of this product:

True Color imagery approximates the response of normal human vision, providing a depiction of the satellite-observed scene. The purpose of doing so is to provide a visually intuitive depiction that is useful to experts and non-experts alike, improving the interpretation of various features such as vegetation, water bodies, clouds and snow, deserts, etc., based on usage of natural colors to highlight those features. For this reason, ‘true color’ and ‘natural color’ are often interchanged when referring to this kind of popular satellite imagery.

- Why is this a GOES-R Proving Ground Product?

Simulated True Color demonstrates the kind of imagery that will be possible in the GOES-R era. GOES-R will feature the Advanced Baseline Imager (ABI) sensor which when combined with complementary data from the Visible/Infrared Imager/Radiometer Suite (VIIRS) on the National Polar-orbiting Operational Environmental Satellite System (NPOESS) satellites will be able to produce versions of the imagery shown here at much higher time resolution.

- How is this product created now?

By combining satellite measurements from bands having responses similar to those of the human retina (namely, blue, green, and red bands), we can create an image that appears as a color photograph. The bands are corrected for atmospheric scattering (otherwise there would be a milky appearance to the imagery, due to the affects of Earth’s atmosphere which accounts for blue skies during the daylight hours). The challenge for the GOES-R ABI is that it will not include one of the required (green) bands. We can overcome this challenge by forming a relationship between the missing green band and nearby bands that we do have. The relationship is formed using a satellite dataset which contains all the ABI bands as well as the green band (here, from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument). Once a relationship is determined, we can use the bands the ABI will have to approximate the green band that it will not. This is why we call it "simulated" true color as opposed to just "true color." The basic concept of the approach is illustrated below.

Fig. 3. An approach to simulating the green band (G) on GOES-R ABI using blue (B), red (R) and near-infrared (NIR) bands. Data from MODIS, which contains all four bands, is used to create a relationship, or function "F(x,y,z)" between band G and the B/R/NIR triplet. This function is represented as a look-up table that can be interrogated by arbitrary combinations of B/R/NIR band reflectance data (each ranging in value between 0 and 100%).

3) Product Examples and Interpretation

Among 3-color composite imagery, True Color requires perhaps the least amount of user training from the standpoint of interpreting colors. To reasonable approximation, these images resemble what an astronaut on the Space Shuttle or International Space Station might observe from roughly 500 miles above the surface. Minor exceptions to this statement include the fact that the response of human vision to color is not replicated perfectly by the satellite sensor, and we have taken the additional step of subtracting-away the atmospheric signal which would contribute to a milky "haze" appearance due to the scattering of sunlight - an effect that is particularly strong at more slant-path views through the atmosphere (e.g., toward the horizon).

Despite the visually intuitive nature of the imagery, interpreting various cloud structures, snow cover, and complex topography are inherently challenging due simply to the way these features appear from the satellite vantage point. The examples below demonstrate how true color depicts lush green deciduous forests over Pennsylvania, the tan sediment-laden waters of the Mississippi River delta, and turquoise shallow-water sand bars in the Caribbean.

Fig. 4. Examples of True Color imagery for various domains.

Drawn on the true color image on the right are two-toned yellow/red lines enclosing regions over the water where sunlight reflection may occur. These so-called "sun glint" zones reside on the red-side of the line, and usually appear as a general brightening of the water surface that can sometimes confuse image interpretation. Sun glint patterns on the water surface are related to local wind speeds. Higher winds roughen the waters and broaden the glint zone area. Locally calm winds and smooth waters can either remove the glint effect entirely (forming dark patches on the water surrounded by brighter regions where the winds are not as calm) or create an "extreme" bright glint feature if the sun/satellite geometry is such that the sun is mirror-reflected directly to the satellite. Be careful when interpreting cloud cover in these areas, but note also that the information provided by sun glint can be a powerful tool in understanding mesoscale boundaries.

True color imagery is formed by combining red, green, and blue spectral band information. Since the GOES-R ABI only includes the red and blue bands, a technique has been developed to approximate what the green band signal would have been. We use a look-up-table to generate the missing green channel. Hence, the resultant product is called "simulated" true color. It is useful to compare against un-simulated true color imagery (i.e., compare the imagery created based on the look-up-table generated green band against an image that uses the actual green band).

Figure 5 shows several comparisons between true color (left panels), what GOES-R ABI will be able to provide (center panels), and the relative difference between the green information between truth and approximation (right panels) which key-in on areas where we will see the greatest disagreement. The extent to which this disagreement impacts a user’s ability to interpret the imagery will depend on the application. In most cases, the agreement is close, but in some cases (particularly over shallow water regions) artifacts may be introduced.

Fig. 5 Examples of True Color (left), Simulated True Color (center), and differences between the two images (right; in terms of percent reflectance in the green channel) imagery for various locations. Red colors denote most significant errors. The central image is based on channels that will be available on the GOES-R Advanced Baseline Imager, and provides a reasonable approximation to True Color in most cases.

4) Advantages and Limitations

The main advantage of true color imagery over various false color or gray-scale imagery enhancements is the intuitive familiarity of the colors as they relate to physical components of the scene, which reduces the amount of training required to make use of the imagery.

The main limitation at this time, and one that will likely go away with the installation of AWIPS-II, is the limitation of 8-bit color (256 colors) to represent a scene that draws (potentially) from a 24-bit (256^3 = almost 17 million) palette of possible colors. The best approach to dealing with this issue would be to use a unique 8-bit color palette for each new true color image, but this is impractical. The next best approach may be for developers to build palettes that are regionally and seasonally dependent, and install/update these palettes at specific forecast offices.

Finally, users should be aware of the caveats related to the simulation of the green band, as mentioned above and illustrated in Figure 5. Ongoing developments in the synthetic true color algorithm, including dedicated look-up-tables for challenging areas, will hopefully mitigate some of the problems described here.