Stray Light in GOES Imager data

May 15th, 2013
GOES-13 0.63 µm visible channel images (click image to play animation)

GOES-13 0.63 µm visible channel images (click image to play animation)

Each year, about every 6 months, the Earth-Sun-Satellite geometry is such that the GOES Imager can look right at the Sun. In the past, there were ‘keep-out zones’ in which the satellites did not image because it was known to be looking at the Sun during those times. The imagery above, from GOES-13, shows visible light in the night-time imagery. (Click here for a similar GOES-15 animation). Stray light values typically peak around 0500 UTC for GOES-East and around 0900 UTC for GOES-West.

In addition, imagery was not possible during the so-called ‘eclipse season’ because the satellites lacked sufficient batteries to power the instruments as they passed through Earth’s shadow. Now, an improved battery system on the current generation GOES-13/14/15 satellites allows for imaging to proceed while the satellite is in the Earth’s shadow.

This new scheduling, however, introduces issues. The GOES Imager is calibrated by periodic looks into deep space, regions from which only very small amounts of radiation (at 3.9, 6.5, 10.7 and 13.3 µm) are being emitted. These ‘space looks’ are on either side of the full-disk GOES Image. During the ‘eclipse season’, that space look can include part of the solar energy, meaning the very small amount of radiation that the satellite is designed to detect is actually potentially significant. Thus, the calibration of the image can be affected. NOAA NESDIS does operationally correct images with ‘stray light’, but this correction does not consider the impact of a corrupted space view. The GOES-13 stray light corrections were implemented in 2012, as discussed here on this blog.

In addition to the calibration images, solar radiation can also be scattered off clouds towards the imager. So, instead of detecting only emitted radiation at night, the GOES Imager is detecting emitted terrestrial radiation in addition to scattered/reflected solar radiation. This solar radiation contaminates the signal, and results in ‘too much’ radiance being detected, resulting in warmer-than-actual inferred blackbody/brightness temperatures.

GOES-13 imagery from infrared channels (click image to enlarge)

GOES-13 imagery from infrared channels (click image to enlarge)

When Stray Light issues occur, the most noticeable effects are in the 3.9 µm channel (Above loop, bottom left) and in products that use the 3.9 µm channel, such as the brightness temperature difference (Above loop, top left). In other words, this calibration issue can affect derived products that use 3.9 µm data at night. The image below shows how the 3.9 µm imagery can change when Stray Light is an issue. Compare the 0415 UTC image, on the left, when Stray Light did not contaminate the space look, with the 0502 UTC image on the right, when Stray Light was an issue.

GOES-13 3.9 µm imagery

GOES-13 3.9 µm imagery

NESDIS is considering methods of mitigating the stray light issues that occasionally occur in the GOES Imager.

GOES-14 is no longer sending images

November 3rd, 2012
GOES-14 0.62 µm Visible Image

GOES-14 0.62 µm Visible Image

GOES-14 came out of storage in mid-August for an annual north-south maneuver and for GOES-R Testing. While in normal mode, GOES-13 suffered an anomaly, and GOES-14 replaced GOES-13 temporarily as GOES-East before GOES-13 returned to service.

After operating in SRSO-R mode for Hurricane Sandy, GOES-14 was switched off after the 1845 UTC image on 1 November 2012 (above). It will remain in stand-by mode until recalled because of anomalies with GOES-West (GOES-15) or GOES-East (GOES-13). For more information on the future plans for GOES-14, click here.

Welcome back GOES-13

October 18th, 2012
GOES-13 Imager at 1445 UTC 18 October

GOES-13 Imager at 1445 UTC 18 October

GOES-13 replaced GOES-14 as the operational GOES-East satellite at 1444 UTC on 18 October 2012. The image above shows the 5 imager channels at 1445 UTC.

In September of 2012, Imagery from both the GOES-13 Sounder and from the GOES-13 Imager showed increasing amounts of noise. On September 23, 2012, GOES-13 was placed in standby mode after both the Sounder and Imager suffered anomalies. The 1046 UTC image and the 2115 UTC image, both on September 23rd, were the last images produced by the sounder and imager, respectively. GOES-14, which had been switched on for an annual north-south maneuver and for subsequent GOES-R simulations, has been standing in as GOES-East for GOES-13 since 24 September.

An outgas was performed on the GOES-13 Sounder that has improved image quality. During an outgas, the sounder instruments are heated (in this case, for nearly 2 days). This drives off molecules that have condensed onto sensors during the satellite’s lifetime. These volatile molecules originate from the various lacquers and coatings that are on the surfaces of the satellite (a rough analogy is new car smell). Sounder imagery from before and after the outgas shows the improvement in all shortwave channels. Similarly, imagery from the imager (below), shows that GOES-13 and GOES-14 have comparably clean signals.

GOES-13 and GOES-14 Imager data from 1302 UTC 16 October (click to toggle between images)

GOES-13 and GOES-14 Imager data from 1302 UTC 16 October (click to toggle between images)

The reduction in noise for Sounder channels means that sounder-derived products will be cleaner. The imagery below is the Total Precipitable Water product derived from the sounder. Cleaner signals in the shortwave infrared channels means fewer fictitious clouds (a comparison using GOES-14 is available here). It is possible that Channel 15, the noisiest of the shortwave IR channels on the sounder, will soon be excluded from both sounder-derived TPW and cloud-top pressure.

Total Precipitable Water derived from the GOES-13 Sounder

Total Precipitable Water derived from the GOES-13 Sounder

NOAA/NESDIS scientists will continue to monitor GOES-13 performance before GOES-14 is put back into storage. In the meantime, a drift-stop maneuver on GOES-14 will occur at 1356 UTC on 19 October, stopping GOES-14′s eastward drift towards the GOES-East station longitude of 75 W. GOES-14 will be very near 90 W when the drift-stop occurs. This link from the Washington Post Capital Weather Gang blog gives additional information. See also this memo from NOAA SSD. Real-time sounder imagery is available here.