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Landsat 8 OLI and TIRS Calibration Notices

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Calibration Notices

The detectors of Landsat 8’s Operational Land Imager (OLI) can register data up to 14 bits. However, only the upper or lower 12 bits can be transmitted to the ground. In normal operations, the upper 12 bits are transmitted. When acquiring in the upper 12-bit mode, the lower 2 bits collapse (saturate) into the lowest data value. The lowest two bits are very noisy.

In 2013 and again in 2015, some Landsat 8 scenes were acquired in lower truncation - meaning data from only the lower 12 bits were captured. During acquisitions in lower truncation, regions of high brightness within a scene exceed the lower 12-bit range of 4096, causing the count to begin again, using the 13th and 14th bits, which are beyond the lower 12 bits being reported. This causes the numeric values to "roll over" and start counting from zero again. Pixels affected by ‘roll over’ do not correctly reflect the brightness of the ground measured and will visually take on an apparently random value (See Figure 1). These roll over values cannot be differentiated from valid values elsewhere in the image and the cloud information in the QA bands will be unreliable. Users should be cautious when using these images for operational activities, although most cloud free data will not be affected.

Figure 1.  Example of oversaturated pixels in Landsat 8 Operational Land Imager (OLI) data acquired with lower 12 bits only

Figure 1. Example of oversaturated pixels in Landsat 8 Operational Land Imager (OLI) data acquired with lower 12 bits only

The 2013 scenes were acquired during the on-orbit checkout period, prior to data becoming available to all users. The affected scenes are listed on this file: (2013_Lower-12-bit-scenes.xlsx)

The scenes acquired in 2015 are being used to investigate the value of the lower two bits and support the possibility of downloading all 14 bits of data for Landsat 9. Data to support two studies were acquired: 1) a night interval through the western United States over fires and urban areas, and 2) a day interval off the coast of eastern Australia over dark water. The artifacts are most noticeable over fires in the night data, and over clouds in the day data. The locations and dates of the intervals are listed in the table below.

Table 1. Areas and scenes affected by 2015 Landsat 8 12-bit lower truncation studies.

Table 1. Areas and scenes affected by 2015 Landsat 8 12-bit lower truncation studies.

We welcome any feedback about the value these data. Feel free to use the Contact Us form.

On March 6, 2015 the Landsat 8 Thermal Infrared Sensor (TIRS) switched from A side to B side electronics to resolve a problem with the A side encoder electronics. At that time, a plan was outlined for reprocessing data acquired since the problem began.

Beginning April 30, 2015, Landsat 8 scenes acquired from December 19, 2014 to March 13, 2015 began reprocessing to repopulate the TIRS data in the products. This calibration notice details the data changes during this timeframe. The reprocessing effort is expected to complete by May 18, 2015.

Some TIRS data for a number of scenes will not be processed due to non-nominal instrument configuration. There were several intervals identified that the data was good for a portion of the interval, but where the SSM was commanded to rotate off nadir making the TIRS data unusable for the other portion of the interval. The reprocessing will process those where TIRS was well outside the field of view of OLI due to an off nadir SSM as OLI only products.

The table below identifies the reprocessing specifics for the anomaly period.

TIRS Scene Select Mechanism (SSM) encoder anomaly reprocessing

Acquisition Date Range

Sensor Acquired

Current Status

Reprocessing Event

End State

December 19, 2014 - March 1, 2015

OLI & TIRS

Side A TIRS data are currently zeroed out (black)

Scenes will be reprocessed to include valid TIRS bands.

OLI & TIRS data available with some exceptions (see below)

January 30, 2015

OLI & TIRS

TIRS Path 14 Rows 40-121 SSM off nadir

Reprocess as OLI Only

OLI only data available

February 2, 2015

OLI & TIRS

TIRS Path 35 Rows 13-43 SSM off nadir

Reprocess as OLI Only

OLI only data available

February 10, 2015

OLI & TIRS

TIRS Paths 11,27,43,59,75,91 SSM off nadir

Reprocess as OLI Only

OLI only data available

February 11, 2015

OLI & TIRS

TIRS Paths 2, 6,18,34,50,82, 107,123,139, 155,171,187, 203, 219 SSM off nadir

Reprocess as OLI Only

OLI only data available

February 19, 2015

OLI & TIRS

TIRS Path 21 Rows 28 - 50 SSM off nadir

Reprocess as OLI Only

OLI only data available

March 2, 2015 - March 3, 2015

None

No TIRS or OLI imagery acquired due to TIRS side-swap activities

Nothing to reprocess

No Data

March 3, 2015 - March 4, 2015

OLI

OLI-only imaging resumes

Nothing to reprocess

OLI only data available

March 4, 2015

OLI & TIRS

Side B TIRS Paths 5,94,110,126,142,158,174, 190,206,222 SSM off nadir

Reprocess as OLI Only

OLI only data available

March 4, 2015 - March 7, 2015

OLI & TIRS

Side B TIRS data are currently zeroed out (black)

Scenes will be reprocessed to include valid TIRS data.

OLI & TIRS data available

March 7, 2015 - March 13, 2015

OLI & TIRS

Nominal TIRS data

Nothing to reprocess

OLI & TIRS data available

 

The Calibration Parameter Files (CPF) for the anomaly period have updated UT1-UTC parameters which may have a slight improvement to OLI and TIRS bands within L1GT products of less than 3 meters. From December 19th 2014 to March 7th 2015 there were no TIRS calibration collections and therefore TIRS data for that period were processed using nominal pre-anomaly calibration parameters. This may cause a slight degradation in thermal measurements but worst case errors are estimated at 0.2 K when viewing a 300 K target. The errors introduced by not having calibration collects for this period of time are much smaller than the errors introduced by TIRS stray light, which can reach up to 2 to 4 K.

Several intervals were identified as having a single event which could cause an anomaly within the imagery. During the acquisition of these intervals the Mission Operations Center issued commands to switch modes of operation on the SSM and a movement of the SSM occurred. These data will be processed as nominal however the TIRS quality score will be lowered to an 8 from the nominal 9 indicating a lower quality. The images below are examples where the mode of operation was changed within a scene causing a small anomaly visible in the TIRS data. There are 8 similar occurrences but each are different in location, and appearance.

OLI Data from Path 075 Row 17 from 26 Feb, 2015
TIRS data from the same scene with SSM anomaly

OLI Data from Path 075 Row 17 from 26 Feb, 2015 	TIRS data from the same scene with SSM anomaly

 

OLI Data from Path 024 Row 23 from 19 Dec, 2015
TIRS data from the same scene with SSM anomaly

OLI Data from Path 024 Row 23 from 19 Dec, 2015 	TIRS data from the same scene with SSM anomaly

On February 3, 2014, the entire Landsat 8 archive will be cleared from the online cache and reprocessed to take advantage of calibration improvements identified during its first year of operation. All Landsat 8 scenes will be removed from the online cache at this time and these data will be reprocessed starting with the most recent acquisitions and proceeding back to the beginning of the mission. Data will then become available for download. Scenes waiting to be reprocessed will also be available for on-demand product orders. Reprocessing is expected to take approximately 50 days.

The Operational Land Imager (OLI) and Thermal Infrared Sensor (TIRS) instruments onboard the satellite have proven to be outstanding sensors; however, all sensors have required radiometric and geometric refinements to ensure good calibration and data continuity. This reprocessing campaign includes all previously implemented calibration parameter updates implemented since launch. These changes are described in more detail below.

Changes to Operational Land Imager (OLI) data

All spectral bands of the OLI sensor have shown minor striping, noticeable primarily in dark uniform areas; the striping is worse in coastal aerosol (CA) and short wave infrared (SWIR) bands. Striping has been reduced by making refinements to the detector linearization correction in the Radiometric Look-Up Table (RLUT). The relative radiometric accuracy is improved by this change; however, the absolute accuracy remains unchanged.

An additional change to the relative gains in the Calibration Parameter File (CPF) will be updated to further reduce striping in the cirrus band. This change will not affect the absolute radiometric accuracy.

The OLI radiometric calibration is being updated to reflect better knowledge of the prelaunch test data, on which the original calibration was based. The reflectance will change at most 0.8 percent, except for the cirrus Band 9, which will change by 7.3 percent (see table). This calibration update will make the reflectance appear brighter than when these data were processed with the previous radiometric calibration. These changes apply only to data converted to reflectance. An improvement to the absolute accuracy of the radiance values, around 2 percent for most bands, will also be implemented.

OLI Bands Radiance Change (%) Reflectance Change (%)
1 (Coastal Aerosol) -2.1 0.8
2 (Blue) -2.0 0.4
3 (Green) -1.7 0.0
4 (Red) -1.9 0.3
5 (NIR) -1.4 0.0
6 (SWIR1) -2.2 0.4
7 (SWIR2) 1.5 0.5
8 (Pan) -1.6 0.2
9 (Cirrus) 0.7 7.3

Table 1. OLI Radiance and Reflective Changes

Changes to Thermal Infrared Sensor (TIRS) data

The TIRS temperature offsets noted on November 14, 2013 Calibration Notice is a primary driver for this reprocessing effort.

These offsets remove 0.29 W/m2/sr/um (~2.1 K) from Band 10 and 0.51 W/m2/sr/um (~4.4 K) from band 11, relative to products processed prior to February 3, 2014. The offsets represent an average error introduced by stray light coming from outside the TIRS field of view and will improve the data accuracy for typical growing season data (10° to 30° C) where the surrounding areas are similar in temperature.

The Root Mean Square (RMS) variability of this correction is 0.12 W/m2/sr/um (~0.8 K) for Band 10 and remains greater at 0.2 W/m2/sr/um (~1.75 K) for Band 11. Due to the larger calibration uncertainty associated with Band 11, it is recommended that users refrain from relying on Band 11 data in quantitative analysis of the TIRS data, such as the use of split window techniques for atmospheric correction and retrieval of surface temperature values.

TIRS Bands Radiance Offset
[W/m2/sr/um]
Temperature Offset
[K @ 300K]
10 -0.29 +/- 0.12 -2.1 +/- 0.8
11 -0.51 +/- 0.2 -4.4 +/- 1.75

Table 2. TIRS offset changes

Geometric Alignment between the Sensors

There are a few geometric changes that will also be fixed in the reprocessing. Based on the analysis of on-orbit data, the alignment between the TIRS instrument and the OLI instrument will be adjusted according to these time periods:

Effective Date Range Change in TIRS alignment Change in TIRS alignment
Launch-
09/19/2013
12 microradians 8.5 meters
09/20/2013-
09/30/2013
25 microradians 18 meters
10/01/2013-
11/27/2013
10 microradians 7.1 meters

Table 3. Geometric alignment changes

There is no change to the TIRS alignment in products after the calibration update on November 27, 2013, which already accounted for this adjustment. These adjustments will improve the alignment of the TIRS thermal bands to the OLI reflective bands.

Due to an apparent seasonal variation in the common alignment of the OLI and TIRS instruments to the Landsat 8 spacecraft attitude control system, a sensor alignment update has been applied to both instruments effective October 1, 2013. The magnitude of this change is approximately 12 microradians (8.5 meters) across track and 8 microradians (6 meters) along track. This change does not impact precision Level-1T (L1T) products (which are corrected using ground control points) but will change the geolocation of systematic Level-1GT (L1GT) products.

New Ground Control Points (GCPs) will become available for three WRS-2 path/rows and GCPs contained within large water bodies will be removed on February 3, 2014 to coincide with the Landsat 8 archive reprocessing. As a consequence of the improved GCPs, scenes once created as a L1GT product may now process to a L1T product. The January 16, 2014 Calibration notice details this update.

In addition to the details provided above, the changes noted in the January 6, 2014 Calibration Notice (found the website above) will also be included in this reprocessing.

An incorrect bias adjustment for Thermal Infrared Sensor (TIRS) data was discovered in the latest release of the Landsat 8 processing system, which has caused a significant error in the TIRS products produced from Landsat 8 scenes acquired from January 14, 2014 to January 23, 2014. (The Operational Land Imager (OLI) bands are not affected.) All Landsat 8 scenes processed between January 14 and January 23 will be purged from the online cache and will become available for on demand order processing. An estimated 3 percent absolute radiometric error is observed and the errors do cause significant striping and banding in bands 10 and 11.

The screenshot below shows a scene processed with the incorrect bias parameters on the left and as it should appear on the right.

Image displaying incorrect bias adjustment (left), and corrected (right) Image displaying incorrect bias adjustment (left), and corrected (right)
Figure 1: Image displaying incorrect bias adjustment (left), and corrected (right)

New Ground Control Points (GCPs) will become available for three WRS-2 path/rows listed below on February 3, 2014 to coincide with the Landsat 8 archive reprocessing:

 Path 

 Row 

 Location 

151

30

Kazakhstan/Kyrgyzstan

138

41

Bhutan

172

43

Red Sea

Because these GCPs are more accurate than previous versions, users should consider replacing Landsat 8 images downloaded before February 3rd, 2014. It is recommended that previously downloaded images for these paths/rows be re-ordered to employ the new GCPs, as scenes once created as a systematic Level-1GT (L1GT) product may now process to a precision Level-1T (L1T) product.

Additionally, GCPs that were determined to be contained within large bodies of water were removed from use during Level-1 processing. Although the presence of these points typically has little effect on the quality of the geometric registration of the L1T imagery, there have been cases where the removal of these GCPs changes the product type from L1GT to L1T.

Several calibration parameter updates will be implemented as part of the Landsat 8 data reprocessing on February 3, 2014 that will result in improved product quality. This reprocessing campaign includes all previously implemented calibration parameter updates that have been implemented since launch. These changes are described in more detail below.

The OLI detector linearization correction coefficients have been refined for all spectral bands to decrease striping in imagery over dark uniform areas. The absolute radiometric accuracy is not significantly affected.

The OLI radiance conversion coefficients are also improved slightly by correcting for a slight error in pre-launch calibration that resulted in product radiance values with as much as a +2% error. A slight improvement to the absolute accuracy of the reflectance values, mainly the cirrus band, will also be implemented. The relative gains will also be updated to reduce striping in the cirrus band, but this will not affect the absolute radiometric accuracy.

The previously mentioned TIRS temperature offset (See the November 15, 2013 Notice) will also be implemented on February 3, 2014. These offsets remove 0.29 W/m^2/sr/um from TIRS band 10 and 0.51 W/m^2/sr/um from TIRS band 11, relative to products processed prior to February 3, 2014. These offsets will remove an average error introduced by stray light coming from outside the TIRS field of view and will improve the data accuracy for typical growing season data (10° to 30° C) where the surrounding areas are similar in temperature. The RMS variability of this correction is 0.12 W/m^2/sr/um for TIRS band 10 and but remains greater at 0.2 W/m^2/sr/um for TIRS band 11. Due to the larger calibration uncertainty associated with TIRS band 11, it is recommended that users refrain from relying on band 11 data in quantitative analysis of the TIRS data, such as the use of split window techniques for atmospheric correction and retrieval of surface temperature values.

Based on the analysis of on-orbit data, the alignment between the TIRS instrument and the OLI instrument will be adjusted according to these time periods:

Effective Date Range

Change in TIRS alignment

Launch-09/19/2013

12 microradians

09/20/2013-09/30/2013

25 microradians

10/01/2013-11/27/2013

10 microradians

There is no change to the TIRS alignment in products after the calibration update on November 27, 2013, which already accounted for this adjustment.

 

Previous updates included in reprocessing effort:

These changes in calibration were implemented in the past, but data processed prior to these dates was not reprocessed, so scenes processed prior to these dates do not include these updates.

June 28, 2013
Tightened the prelaunch geometric processing thresholds to account for the higher accuracy observed while using the on-orbit geometric calibration derived during the commissioning period.

August 9, 2013
Adjusted the OLI linearity correction coefficients based on analysis of updated pre-launch calibration information which improves the striping at various radiance levels. This update affected all OLI spectral bands with respect to striping, but didn’t significantly affect the absolute radiometric accuracy. (See the August 9, 2013 Notice)

August 21, 2013
Improved the geodetic consistency with Landsat 1-7 imagery and reduced striping. (See the August 21, 2013 Notice)

September 27, 2013
Adjusted the TIRS alignment to account for the safe hold anomaly that occurred on September 19, 2013. (See the September 27, 2013 Notice)

November 27, 2013
In addition to the TIRS alignment adjustment shown in the table above, the gains of the detectors on the edges of each sensor chip assembly of the OLI spectral bands was adjusted slightly to reduce the potential stripes. The largest change is less than 0.3%, doesn’t affect the overall radiometric accuracy of the products.

The majority of the radiometric calibration changes indicated in the October 25, 2013 calibration notice have been deferred to early-2014, to coincide with a software update for the Landsat Product Generation System (LPGS). Therefore, reprocessing of the entire Landsat 8 archive will not occur before early-2014.

When the reprocessing effort begins, the OLI radiance-to-reflectance conversion coefficients will be adjusted for the cirrus band (Band 9) to account for on-orbit performance. The prelaunch derived coefficients were calculated using heliostat measurements, which were expected to be in error because little sunlight reaches the ground at these wavelengths. This adjustment changes the reflectance by about 7 percent in the cirrus band. Additionally, the precision of the other spectral bands' radiance-to-reflectance conversion coefficients will be increased, changing the reflectance by up to 0.3 percent.

Relating to TIRS thermal band calibration, prior to the early-2014 update, users may subtract 0.29 W/(m2 sr µm) from every TIRS Band 10 calibrated radiance value, and 0.51 W/(m2 sr µm) for every TIRS Band 11 calibrated radiance value to provide values closer (on average) to the actual radiances. The equations to convert from calibrated product pixel values to calibrated radiance values can be found on the Landsat 8 Web page. These numbers are based on comparisons to surface water temperatures and correspond to a -2.1 K correction (Band 10) and a -4.4 K correction (Band 11) for a 295 K brightness temperature. The rms variability in the required adjustment is roughly 0.12 W/(m2 sr µm) (0.8 K) for Band 10 and 0.2 W/(m2 sr µm) (1.75 K) for Band 11. Studies indicate that the errors are scene dependent and probably related to out-of-field response in the TIRS instrument.

Given the larger uncertainty in the Band 11 values, users should work with TIRS Band 10 data as a single spectral band (like Landsat 7 Enhanced Thematic Mapper Plus (ETM+)) and should not attempt a split-window correction using both TIRS Bands 10 and 11.

Updates will be provided on this page as understanding of the calibration improves, and also when the reprocessing effort is planned to begin.

In the near future, calibration changes will be made that will affect the Thermal Infrared Sensor (TIRS) Band 10 and all of the Operational Land Imager (OLI) bands onboard Landsat 8.

The calibration for TIRS Band 10 will be lowered by a constant 0.32 W/(m2 sr µm) for every TIRS Band 10 pixel. This adjustment is being made due to significant discrepancies as compared to surface water temperature measurements. Studies are ongoing to better characterize the source of the calibration errors, and if possible, provide a more accurate scene-dependent correction. No adjustment will be made to TIRS Band 11, as indications are that its calibration is further off and more variable. Until indicated otherwise, users should work with TIRS Band 10 data as a single spectral band (like Landsat 7 Enhanced Thematic Mapper Plus (ETM+)) and should not attempt a split-window correction using both TIRS Bands 10 and 11.

Prior to this reprocessing effort, users can subtract 0.32 W/(m2 sr µm) from the TIRS Band 10 Top-of-Atmosphere (TOA) radiance data to improve the accuracy of their current image products or to avoid downloading a new image product after reprocessing occurs. Once a more accurate scene-dependent correction is determined, a second purge and reprocessing will take place.

The OLI radiance-to-reflectance conversion coefficients will be adjusted for the cirrus band (Band 9) to account for on-orbit performance. The prelaunch derived coefficients were calculated using heliostat measurements, which were expected to be in error because little sunlight reaches the ground at these wavelengths. This adjustment changes the reflectance by about 7 percent in the cirrus band. Additionally, the precision of the other spectral bands’ radiance-to-reflectance conversion coefficients will be increased, changing the reflectance by up to 0.3 percent.

The relative gains of single detectors on the edges of each OLI Sensor Chip Assembly (SCA) will be updated to correct slight striping that is typically not visible. This update will affect all OLI spectral bands.

On September 19, 2013 (DOY 262) at approximately 20:08 UTC, Landsat 8 experienced an unplanned transition to safe hold following an attitude control anomaly. Precision attitude control was recovered and imaging operations resumed on day of year 264 (September 21, 2013). Post-anomaly calibration checks detected a systematic change in the alignment between the OLI and TIRS sensors. No change in the OLI alignment to the spacecraft attitude control system was apparent so the shift is being attributed to the TIRS instrument.

The magnitude of the change - a pitch axis offset of approximately 30 microradians (about 0.2 TIRS pixels) - is large enough to threaten the thermal-to-reflective band registration requirements. Band registration tests confirm that the along-track TIRS-to-OLI band registration performance has been degraded since the safe hold event.

A calibration parameter file (CPF) update to the ACS_to_TIRS_Rotation_Matrix parameter was developed to correct this offset and was put into production on September 27, 2013. This update is effective from September 21, 2013, so a subdivision of the 3rd quarter CPF effective date range will be required. The new parameters will also be used for the upcoming 4th quarter CPF unless the ongoing monitoring of TIRS-to-OLI alignment indicates that further changes are required.

No direct cause for the alignment change is known but it may be related to the change in the spacecraft thermal environment during the safe hold period. If this is the case, it is possible that, over time, the alignment will drift back closer to its earlier position.

Discrepancies have been noted between calibrated Landsat 8 TIRS Bands 10 and 11 data, and surface-water temperature measurements collected to validate thermal band calibration.

Surface-water temperatures derived from TIRS data, after correction for atmospheric transmission and emissivity, are warmer than measured surface-water temperatures by 2K or more. These discrepancies also may not be consistent across the focal plane. This indicates a possible bias or other error in TIRS calibration that places the calibration uncertainty beyond the specified performance of 2 percent.

Users are cautioned to be aware of potential impacts to their analyses and results. The calibration team continues to analyze TIRS data and compare results to surface-water temperature measurements to discover the source of the discrepancy.

Updates to TIRS calibration coefficients will be incorporated into Landsat 8 data processing as soon as the discrepancy is sufficiently understood. Details will be provided on this website as they become available.

An update to the CPF on August 21, 2013 improves the geodetic consistency with Landsat 1-7 imagery. Due to some GLS 2000 scenes having significant geodetic errors, a limit is set between the systematically corrected product and the GLS 2000 reference. This limit has been increased from 100 meters and is now set at 200 meters. Scenes with a difference less than 200 meters will be consistent with historical Landsat imagery. There are no known GLS 2000 reference scenes that are off more than 200 meters.

This update also improves the OLI relative calibration which reduces striping in very uniform scenes. The largest improvement is in the Coastal Aerosol (Band 1) where the magnitude of the striping is largest (see figures below), but all reflective bands are affected. The radiometric accuracy has not been affected since these changes are relative to the existing absolute calibration. The banding visible in the figures below is not affected, but will be addressed in a future calibration update.

Band 1. Previous CPF (left); Updated CPF (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters. Striping has been reduced in the right image, but banding remains the same.

Figure 1. Band 1. Previous CPF (left); Updated CPF (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters. Striping has been reduced in the right image, but banding remains the same.

Full resolution zoom of band 1. Previous CPF (left); Updated CPF (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters. The banding becomes more defined on the right since the striping has been reduced.

Figure 2. Full resolution zoom of band 1. Previous CPF (left); Updated CPF (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters. The banding becomes more defined on the right since the striping has been reduced.

Response Linearization Look Up Tables (RLUT) are additional files that accompany Calibration Parameter Files (CPF) and contain parameters used to linearize the output of the OLI detectors. This is done to correct the relationship between Digital Number (DN) values and the dynamic range of the instrument. Linearization also helps to limit saturated pixels to true saturations, and on the dark end, limit zero values to missing data.

An update to the RLUT on August 9, 2013 decreases the striping that was initially seen within the Coastal Aerosol (Band 1), SWIR1 (Band 6), and SWIR2 (Band 7) spectral bands of some Landsat 8 scenes (see figures 1 and 2 below).

The magnitude of these stripes is small and vary based on the brightness of the scene. This improvement will be seen in very uniform areas; however this update may increase the striping and banding slightly in extremely uniform areas of very low reflectance scenes ( < 0.1% reflectance; see figure 3 below). This will be corrected with a future system release.

Band 6 (~5% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

Figure 1. Band 6 (~5% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

Band 7 (~5% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

Figure 2. Band 7 (~5% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

Band 6 (~0.1% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

Figure 3. Band 6 (~0.1% reflectance). Original RLUT inputs (left); Updated RLUT inputs (right). Each image has been radiometrically stretched to show the effect of the updated calibration parameters.

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