GVAR (GOES Variable Format) is the transmission of full resolution GOES N series data to ground stations within the footprint of NOAA's operational geostationary satellites GOES-13 (75W) and GOES-15 (135W), respectively. Dissemination schedules are maintained by NESDIS. With a geostationary orbit, any location within the satellite footprint is able to receive nearly continuous data coverage. To receive the data, users can purchase the necessary equipment (computer, software, antenna) from commercial companies for unlimited access to GOES signals. There is no fee or license requirement required by NOAA to receive this data. Archived data are available from NOAA through CLASS. Some commercial companies and other sites offer the data either processed or in raw form. Archived data acquired from NOAA usually incurs a fee for reproduction.
The GVAR data transmission format was developed to allow full use of the capabilities of the advanced, three-axis stabilized spacecraft while retaining as much commonality as possible with receiving equipment presently in use from earlier spin-stabilized GOES spacecraft. The GVAR format is based on the operational visible and infrared spin scan radiometer atmospheric sounder (VAS) mode AAA format, which consisted of a repeating sequence of 12 fixed-length equal size blocks. The transmission of these blocks was synchronized with the spin rate of the earlier GOES spacecraft, that is, one complete 12 block sequence per satellite rotation. The GVAR transmission sequence consists of 12 distinct blocks numbered 0 through 11. Blocks 0 through 10 are transmitted when an Imager scan line is completed. Block 10 is followed by a variable number of block 11s, according to what data are available for transmission.
The conversion of the raw data from the instruments to 10-bit scaled radiances is carried out in real time in the Sensor Processing System (SPS) at the Command and Data Acquisition (CDA) facility at Wallops, VA, and is described in a NOAA Technical Memorandum - Operational Calibration of the Imagers and Sounders on the GOES-8 and -9 Satellites.
A 10-bit GVAR count value (0-1023) can be converted to a scene radiance according to the following equation:
|
R = (X - b)/m, |
(1) |
where R is radiance(mW/[m2-sr-cm-1]) and X is the GVAR count value. The coefficients m and b are the scaling slope and intercept, respectively. The values of m and b are listed in Table 1. They depend on the channel selected, but for a given channel they are constant for all time and are the same for all satellites of the series.
| Channel | m | b |
|---|---|---|
| 2 | 227.3889 | 68.2167 |
| 3 | 38.8383 | 29.1287 |
| 4 | 5.2285 | 15.6854 |
| 5 | 5.0273 | 15.3332 |
| Channel | m | b |
|---|---|---|
| 2 | 227.3889 | 68.2167 |
| 3 | 38.8383 | 29.1287 |
| 4 | 5.2285 | 15.6854 |
| 6 | 5.5297 | 16.5892 |
There are three steps to convert a 10-bit GVAR count value (0-1023) to temperature.
Step 1: Convert the GVAR count value to a radiance using the way described in part I.
Step 2: Convert radiance to effective temperature using the inverse of the Planck function as follows:
|
(2) | ||||||
| c1 = 1.191066 x 10-5 [mW/(m2-sr-cm-4)] | |||||||
| c2 = 1.438833 (K/cm-1) |
where Teff is effective temperature (K), ln stands for natural logarithm, and R is radiance. The coefficients n, c1, and c2 are the central wavenumber of the channel and the two radiation constants, respectively. The constants c1 and c2 are invariant, but n depends on the spectral characteristics of the channel and will vary from instrument to instrument.
Step 3: Convert effective temperature Teff to actual temperature T (K) using the following equation:
|
T = a + b * Teff |
(3) |
where a and b are two conversion coefficients.
Note in the conversions that:
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2556.71 | -0.578526 | 1.001512 |
| 2/b | 2558.62 | -0.581853 | 1.001532 |
| 3 | 1481.91 | -0.593903 | 1.001418 |
| 4/a | 934.30 | -0.322585 | 1.001271 |
| 4/b | 935.38 | -0.351889 | 1.001293 |
| 5/a | 837.06 | -0.422571 | 1.001170 |
| 5/b | 837.00 | -0.466954 | 1.001257 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2555.18 | -0.579908 | 1.000942 |
| 2/b | 2555.18 | -0.579908 | 1.000942 |
| 3 | 1481.82 | -0.493016 | 1.001076 |
| 4/a | 934.59 | -0.384798 | 1.001293 |
| 4/b | 934.28 | -0.363703 | 1.001272 |
| 5/a | 834.02 | -0.302995 | 1.000941 |
| 5/b | 834.09 | -0.306838 | 1.000948 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2552.9845 | -0.60584483 | 1.0011017 |
| 2/b | 2552.9845 | -0.60584483 | 1.0011017 |
| 3 | 1486.2212 | -0.61653805 | 1.0014011 |
| 4/a | 936.10260 | -0.27128884 | 1.0009674 |
| 4/b | 935.98981 | -0.27064036 | 1.0009687 |
| 5/a | 830.88473 | -0.26505411 | 1.0009087 |
| 5/b | 830.89691 | -0.26056452 | 1.0008962 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2562.07 | -0.644790 | 1.000775 |
| 2/b | 2562.07 | -0.644790 | 1.000775 |
| 3 | 1481.53 | -0.543401 | 1.001495 |
| 4/a | 931.76 | -0.306809 | 1.001274 |
| 4/b | 931.76 | -0.306809 | 1.001274 |
| 5/a | 833.67 | -0.333216 | 1.001000 |
| 5/b | 833.04 | -0.315110 | 1.000967 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2562.45 | -0.650731 | 1.001520 |
| 2/b | 2562.45 | -0.650731 | 1.001520 |
| 3/a | 1536.43 | -4.764728 | 1.012420 |
| 3/b | 1536.94 | -4.775517 | 1.012403 |
| 4/a | 933.21 | -0.360331 | 1.001306 |
| 4/b | 933.21 | -0.360331 | 1.001306 |
| 6 | 751.91 | -0.253449 | 1.000743 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2562.45 | -0.650563 | 1.001519 |
| 2/b | 2562.45 | -0.650563 | 1.001519 |
| 3/a | 1536.43 | -4.764832 | 1.012421 |
| 3/b | 1536.27 | -4.760714 | 1.012385 |
| 4/a | 933.21 | -0.360250 | 1.001306 |
| 4/b | 933.21 | -0.360250 | 1.001306 |
| 6 | 751.77 | -0.252130 | 1.000742 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2561.74 | -1.437204 | 1.002562 |
| 2/b | 2561.74 | -1.437204 | 1.002562 |
| 3/a | 1522.52 | -3.625663 | 1.010018 |
| 3/b | 1521.66 | -3.607841 | 1.010010 |
| 4/a | 937.23 | -0.386043 | 1.001298 |
| 4/b | 937.27 | -0.380113 | 1.001285 |
| 6 (ITT original) | 753.15 | -0.195055 | 1.000610 |
| 6 (ITT updated) | 751.93 | -0.134688 | 1.000481 |
| 6 | 749.83 | -0.134801 | 1.000482 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2572.47 | -1.530285 | 1.002507 |
| 2/b | 2572.47 | -1.530285 | 1.002507 |
| 3/a | 1529.33 | -3.561161 | 1.009501 |
| 3/b | 1530.10 | -3.577037 | 1.009444 |
| 4/a | 934.04 | -0.263369 | 1.001176 |
| 4/b | 933.94 | -0.260576 | 1.001179 |
| 6/a | 753.38 | -0.199338 | 1.000616 |
| 6/b | 753.91 | -0.234004 | 1.000692 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2577.98 | -1.596954 | 1.002631 |
| 2/b | 2577.98 | -1.5969544 | 1.002631 |
| 3/a | 1529.35 | -3.580129 | 1.009547 |
| 3/b | 1530.13 | -3.595987 | 1.009490 |
| 4/a | 936.20 | -0.2875616 | 1.001258 |
| 4/b | 936.14 | -0.2888648 | 1.001265 |
| 6/a | 753.30 | -0.1938129 | 1.000605 |
| 6/b | 753.84 | -0.2296604 | 1.000684 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2577.3518 | -1.5297091 | 1.0025608 |
| 2/b | 2577.3518 | -1.5297091 | 1.0025608 |
| 3/a | 1519.3488 | -3.4647892 | 1.0093656 |
| 3/b | 1518.5610 | -3.4390527 | 1.0094427 |
| 4/a | 933.98541 | -0.29201763 | 1.0012018 |
| 4/b | 934.19579 | -0.31824779 | 1.0012303 |
| 6/a | 752.88143 | -0.22508805 | 1.0006686 |
| 6/b | 752.82392 | -0.21700982 | 1.0006503 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2560.75 | -1.633214 | 1.002639 |
| 2/b | 2560.75 | -1.633214 | 1.002639 |
| 3/a | 1538.62 | -3.193019 | 1.008531 |
| 3/b | 1538.66 | -3.191726 | 1.008510 |
| 4/a | 935.09 | -0.3433922 | 1.001259 |
| 4/b | 934.89 | -0.3246338 | 1.001239 |
| 6/a | 752.91 | -0.2157592 | 1.000648 |
| 6/b | 752.76 | -0.2044856 | 1.000623 |
| Channel/Detector | n | a | b |
|---|---|---|---|
| 2/a | 2562.7905 | -1.5693377 | 1.0025034 |
| 2/b | 2562.7905 | -1.5693377 | 1.0025034 |
| 3/a | 1521.1988 | -3.4706545 | 1.0093296 |
| 3/b | 1521.5277 | -3.4755568 | 1.0092838 |
| 4/a | 935.89417 | -0.36151367 | 1.0012715 |
| 4/b | 935.78158 | -0.35316361 | 1.0012570 |
| 6/a | 753.72229 | -0.21475817 | 1.0006485 |
| 6/b | 753.93403 | -0.24630068 | 1.0007178 |
The use of Teff accounts for the variation of the Planck function across the spectral passband of the channel. The differences between the values of T and Teff increase with decreasing temperature. They are usually of the order of 0.1 K. In the worst case, near 180 K, they are approximately 0.3 K.
A change of one GVAR count is equivalent to a temperature change of approximately 0.11 K in channels 2,4,5, and 6 for a scene at 300K, and a change of approximately 0.04 K in channel 3 for a scene at 290 K.
The errors resulting from the above approximations can be reduced by a factor of 10 if the following second-order polynomial is adopted:
|
T = a + b * Teff + g * Teff2 |
4) |
This yields errors under 0.001 K, even at temperatures above 310 K or under 210 K. The a, b, and g coefficients and centroid wavenumber n for all detectors are listed in the tables 3-1 through 3-8 below (see comments about central wavenumber definition under Step 3 in Section II):
As mentioned at the beginning of this memorandum, the methods described here to convert imager GVAR data to scene radiance or temperature are also applicable to GOES sounders. The GOES sounder scaling coefficients are listed in Table A2 of the above-mentioned NOAA Technical Memorandum - Operational Calibration of the Imagers and Sounders on the GOES-8 and -9 Satellites. As described in the memorandum, infrared sounder data in GVAR are scaled radiances packaged in 16-bit words. The conversion of the raw data from the instruments to 16-bit scaled radiances is carried out in real time in the SPS at the CDA facility at Wallops, VA. The related coefficients (n, a, b, and g) of GOES sounders for the first- and second-order polynomials (Equations [3] and [4]) - are included in the following tables (see comments about central wavenumber definition under Step 3 in Section II):
Coefficients (n, a and b) for the first-order polynomial:
Coefficients (n, a, b, and g) for the second-order polynomial:
The GOES-8 through GOES-15 Imager and Sounder look-up tables of radiances, brightness temperatures vs. GVAR counts are listed below for the currently operational spectral response functions. The look-up tables for the Imagers cover all the detectors, while the look-up tables for the Sounders only cover detector 1 for each infrared channel. This arrangement intends to avoid huge disk space the Sounder look-up tables might have occupied. Sounder look-up tables are arranged according to their channels and are also compressed.
Imagers:
Sounders:
The mode - A count value Xa is derived from the temperature with the following equations3:
For 163K <= T <= 242K, Xa = 418 - T.
For 242K <= T <= 330K, Xa = 660 - 2T.
Mode - A count values are on an eight-bit scale and range in value from 0 to 255, with high counts representative of low temperatures. Beyond the difference in precision, there is a fundamental difference between GVAR counts and mode-A counts--their units. GVAR counts are scaled radiances, whereas mode-A counts are temperatures.
[1] Weinreb, M.P., M. Jamieson, N. Fulton, Y. Chen, J.X. Johnson, J. Bremer, C. Smith, and J. Baucom, "Operational calibration of Geostationary Operational Environmental Satellite-8 and -9 imagers and sounders," Applied Optics, 36, pp. 6895-6904, 1997.
[2] Johnson, J.X., GOES-8 radiance to brightness-temperature conversions, internal memorandum, Sept. 20, 1996.
[3] Bristor, C.L. (ed.), "Central processing and analysis of geostationary satellite data," NOAA Tech. Memo. NESS 64, U.S. Dep't. Commerce, National Oceanic and Atmospheric Administration, Washington, DC, 155 pp. (1975)