Landsat 8-9 Collection 2 (C2) Level 2 Science Product (L2SP) Guide

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LSDS-1619Version 4.0Department of the InteriorU.S. Geological SurveyLandsat 8-9Collection 2 (C2)Level 2 Science Product (L2SP) GuideVersion 4.0March 2022

Landsat 8-9Collection 2 (C2)Level 2 Science Product (L2SP) GuideMarch 2022Document Owner:Digitally signed by KRISTISAYLERDate: 2022.03.24 10:13:33-05'00'KRISTI SAYLERKristi SaylerLSRD Project ManagerU.S. Geological SurveyDateApproved By:Digitally signed by TIMOTHYTIMOTHYGLYNNDate: 2022.03.24 09:55:30GLYNN-05'00'Timothy A. GlynnLSDS CCB ChairU.S. Geological SurveyDateEROSSioux Falls, South Dakota- ii -LSDS-1619Version 4.0

Executive SummaryThis document describes relevant characteristics of the Landsat 8 (L8) and Landsat 9(L9) Collection 2 (C2) Level 2 Science Products (L2SP) to facilitate their use in the landremote sensing community.Landsat 8-9 Level 2 Science Products contain: Surface Reflectance (SR) derived from Landsat 8-9 Collection 2 Level 1Operational Land Imager (OLI) dataSurface Temperature (ST) derived from Landsat 8 Collection 2 Level 1 ThermalInfrared Sensor (TIRS) Band 10 dataIntermediate bands used in calculation of the ST productsQuality Assessment (QA) masks indicating the usefulness of the pixel dataLandsat 8-9 SR products are created with the Land Surface Reflectance Code(LaSRC). Landsat 8-9 ST products are created with a single channel algorithm jointlycreated by the Rochester Institute of Technology (RIT) and National Aeronautics andSpace Administration (NASA) Jet Propulsion Laboratory (JPL).A primary characteristic of Collection 2 data is the implementation of the Sentinel 2Global Reference Image (GRI) into updated Landsat 8 OLI ground control points forimproved geometric accuracy. This improves interoperability of the Landsat archive boththrough time and with other remotely sensed datasets. Additionally, Collection 2includes updated global digital elevation modeling sources and calibration andvalidation updates.Information about Landsat 4-7 Collection 2 Level 2 products can be found in theLandsat 4-7 Collection 2 Level 2 Science Product Guide.- iii -LSDS-1619Version 4.0

Document eChangeNumberLSDS-1619Version 1.0May 2020CR 15400LSDS-1619Version 2.0September 2020CR 20016LSDS-1619Version 3.0September 2021CR 20746LSDS-1619Version 4.0March 2022CR 20976- iv -LSDS-1619Version 4.0

ContentsExecutive Summary . iiiDocument History . ivContents . vList of Figures . viList of Tables . viSection 1Introduction . 11.1 Background . 11.1.1Surface Reflectance . 11.1.2Surface Temperature . 31.2 Document Organization . 4Section 2Known Issues . 52.1 Surface Reflectance . 5Section 3Caveats and Constraints . 63.1 Surface Reflectance . 63.2 Surface Temperature . 7Section 4Product Access . 9Section 5Product Packaging . 10Section 6Product Characteristics . 116.1 Band Specifications. 116.1.1Cloud and Cloud Shadow Specifications . 136.1.2Radiometric Saturation Band . 156.1.3Aerosol QA Band . 166.1.4Level 2 Metadata . 186.1.5Level 2 Special Notes . 18Section 7Auxiliary Data . 197.1 Surface Reflectance Auxiliary Data . 197.1.1Landsat 8 Ratio Map . 197.1.2ETOPO5 . 197.1.3LDCMLUT . 197.1.4MODIS Fused Data . 197.2 Surface Temperature Auxiliary Data . 207.2.1ASTER Emissivity Data . 207.2.2GEOS-5 FP-IT Data . 20Section 8Citation Information . 21Section 9Acknowledgments . 22Section 10 User Services . 23Appendix ADefault File Characteristics . 24Appendix BMetadata Fields . 25Appendix CAcronyms . 34References . 36-v-LSDS-1619Version 4.0

List of FiguresFigure 1-1. Example of LaSRC Atmospheric Correction: Landsat 8 Top of AtmosphereReflectance RGB (4,3,2) composite (left) and the corresponding Landsat 8 SurfaceReflectance product (right) . 2Figure 1-2. Example of Landsat 9 Surface Reflectance RGB composite (Bands 4,3,2)(left) and the corresponding color-enhanced Surface Temperature (right). 4Figure 2-1. Landsat 8 Top of Atmosphere (TOA) Reflectance for the SWIR-2 band (left)and an example of the speckle observed in the corresponding Surface Reflectanceproduct (right) . 5Figure 3-1. Spatial Extent of ASTER GED Emissivity . 8List of TablesTable 1-1. Differences between Landsat 4–7 (LEDAPS) and Landsat 8-9 (LaSRC)Surface Reflectance Algorithms . 3Table 6-1. Collection 2 (C2) Landsat 8-9 Level 2 Science Products (L2SP) BandSpecifications . 12Table 6-2. Landsat 8-9 Pixel Quality Assessment (QA PIXEL) Bit Index . 13Table 6-3. Landsat 8-9 Pixel Quality Assessment (QA PIXEL) Value Interpretations . 14Table 6-4. Landsat 8-9 Radiometric Saturation Quality Assessment (QA RADSAT) BitIndex . 16Table 6-5. Landsat 8-9 Internal Surface Reflectance Aerosol Quality Assessment(SR QA AEROSOL) Bit Index . 17Table 6-6. Landsat 8-9 SR QA AEROSOL Values . 17Table 6-7. Landsat 8-9 SR QA AEROSOL Value Interpretations . 18Table A-1. Collection 2 Default File Characteristics . 24- vi -LSDS-1619Version 4.0

Section 11.1IntroductionBackgroundLandsat satellite data have been produced, archived, and distributed by the U.S.Geological Survey (USGS) since 1972. Users rely upon these data for conductinghistorical studies of land surface change but have shouldered the burden of postproduction processing to create applications-ready datasets. To alleviate this burden onthe user, the USGS has initiated an effort to produce a collection of Landsat Level 2Science Products (L2SP) to support land surface change studies.Landsat Collection 2 (C2) marks the second major reprocessing effort on the Landsatarchive by the USGS that results in several data product improvements that harnessrecent advancements in data processing, algorithm development, and data access anddistribution capabilities.1.1.1 Surface ReflectanceLandsat 8-9 Surface Reflectance (SR) Science Products are generated from LandSurface Reflectance Code (LaSRC) version 1.5.0 (derived from NASA LaSRC version3.5.5). The original LaSRC algorithm was developed by Dr. Eric Vermote, NationalAeronautics and Space Administration (NASA) Goddard Space Flight Center (GSFC)and was modified by the USGS Earth Resources Observation and Science (EROS)Center. LaSRC generates Top of Atmosphere (TOA) Reflectance and TOA BrightnessTemperature (BT) using the calibration parameters from the metadata. Atmosphericcorrection routines are then applied to Landsat 8-9 TOA Reflectance data, usingauxiliary input data such as water vapor, ozone, and Aerosol Optical Thickness (AOT)retrieved from Moderate Resolution Imaging Spectroradiometer (MODIS), and digitalelevation derived from Earth Topography Five Minute Grid (ETOPO5) to generateSurface Reflectance. The result is delivered as the Landsat Surface Reflectance dataproduct.Specific details about the SR algorithm can be found in Section 4.7 of the Landsat 8-9Calibration and Validation (Cal/Val) Algorithm Description Document (ADD).-1-LSDS-1619Version 4.0

Figure 1-1. Example of LaSRC Atmospheric Correction: Landsat 8 Top ofAtmosphere Reflectance RGB (4,3,2) composite (left) and the correspondingLandsat 8 Surface Reflectance product (right)Figure 1-1 shows a comparison of a Landsat 8 TOA Reflectance composite (Bands4,3,2), and a Surface Reflectance composite image of Seattle, WA, using data acquiredby Landsat 8 (Path 47 Row 27) on October 14, 2013. Both images are linearly scaledfrom ρ 0.0 to 0.15.The LaSRC algorithm is distinctly different from the algorithm used to process Landsat4–5 Thematic Mapper (TM) and Landsat 7 Enhanced Thematic Mapper Plus (ETM )Level 1 (L1) products to Surface Reflectance, known as the Landsat EcosystemDisturbance Adaptive Processing System (LEDAPS). Details of these differences aredescribed in Table 1-1.ParameterInstrumentsLEDAPSLaSRCLandsat 4-5 TM,Landsat 7 ETM NASA GSFC, MEaSUREsJeff Masek, NASAYesVisible (Bands 1–5,7)NASA GSFCEric Vermote, NASAYesVisible (Bands 1–7, 9 OLI)Landsat 8-9 OLI/TIRS(Original) research grantPrincipal InvestigatorGlobal coverageTOA ReflectanceTOA BrightnessTemperatureSRThermal bands used in SRprocessing?Radiative transfer modelThermal correction levelThermal band unitsThermal (Band 6)Thermal (Bands 10 & 11 TIRS)Visible (1–5, 7) bandsYes (Brightness temperature Band 6 isused in cloud estimation)6STOA onlyKelvinVisible (Bands 1–7) (OLI only)PressureNCEP GridWater vaporNCEP Grid-2-NoInternal algorithmTOA onlyKelvinCalculated internallybased on elevationMODIS CMGLSDS-1619Version 4.0

ParameterLEDAPSLaSRCAir temperatureDEMNCEP GridETOPO5 (CMGDEM)OzoneOMI/TOMSnot usedETOPO5 (CMGDEM)MODIS CMG Coarse resolutionozoneAOTSun angleView zenith angleUndesirable zenith anglecorrectionPan band processed?XML metadata?Brightness temperaturecalculatedCloud maskData formatFill valuesCorrelation between chlorophyllabsorption and bound water absorption ofsceneScene center from input metadataFrom input metadataSR not processed when solar zenithangle 76 degreesNoYesScene center from input metadataHard-coded to “0”SR not processed when solar zenithangle 76 degreesNoYesYes (Band 6 TM/ETM )Yes (Bands 10 & 11 TIRS)Internal AlgorithmCFMask (v3.3.1)CFMask (v3.3.1)UINT16UINT1600CloudCloudAdjacent cloudAdjacent cloudCloud shadowCloud shadowDDVQA bandsAerosolsFillCirrusLand waterAerosol Interpolation FlagSnowAtmospheric opacity6S Second Simulation of a Satellite Signal in the Solar Spectrum, AOT Aerosol Optical Thickness, CFMask C Version of Function Of Mask, CMA Climate Modeling Grid - Aerosol, CMG Climate Modeling Grid, DDV Dark Dense Vegetation, DEM Digital Elevation Model, ETM Enhanced Thematic Mapper Plus, GSFC Goddard Space Flight Center, INT Integer, LaSRC Land Surface Reflectance Code, LEDAPS LandsatEcosystem Disturbance Adaptive Processing System, MEaSUREs Making Earth Science Data Records forUse in Research Environments, MODIS Moderate Resolution Imaging Spectroradiometer, NA NotApplicable, NASA National Aeronautics and Space Administration, NCEP National Centers forEnvironmental Prediction, OLI Operational Land Imager, OMI Ozone Monitoring Instrument, QA QualityAssessment, SR Surface Reflectance, TIRS Thermal Infrared Sensor, TM Thematic Mapper, TOA Topof Atmosphere Reflectance, TOMS Total Ozone Mapping Spectrometer, XML Extensible Markup LanguageTable 1-1. Differences between Landsat 4–7 (LEDAPS) and Landsat 8-9 (LaSRC)Surface Reflectance Algorithms1.1.2 Surface TemperatureThe Landsat 8-9 Surface Temperature (ST) product is generated from the singlechannel algorithm version 1.3.0 (derived from June 2017 version of RIT ST code). TheLandsat 8-9 Collection 2 ST is derived from the Collection 2 Level 1 Thermal InfraredSensor (TIRS) band 10 using Top of Atmosphere (TOA) Reflectance, TOA BrightnessTemperature (BT), Advanced Spaceborne Thermal Emission and ReflectionRadiometer (ASTER) Global Emissivity Dataset (GED) data, ASTER NormalizedDifference Vegetation Index (NDVI) data, and atmospheric profiles of geopotentialheight, specific humidity, and air temperature extracted from reanalysis data.Specific details about the ST algorithm can be found in Section 4.7 of the Landsat 8-9Calibration and Validation (Cal/Val) Algorithm Description Document (ADD).-3-LSDS-1619Version 4.0

Figure 1-2. Example of Landsat 9 Surface Reflectance RGB composite (Bands4,3,2) (left) and the corresponding color-enhanced Surface Temperature (right)Figure 1-2 shows a comparison of a Landsat 9 Surface Reflectance composite (Bands4,3,2), and color-enhanced Surface Temperature for an area in Nepal, using dataacquired by Landsat 9 (Path 141 Row 40) on January 19, 2022. Blue areas in theSurface Temperature product indicate cooler temperatures; red areas indicate warmertemperatures.1.2Document OrganizationThis document contains the following sections: Section 1 provides an introductionSection 2 describes known issuesSection 3 provides an explanation of caveats and constraintsSection 4 provides details on product accessSection 5 provides details on product packagingSection 6 provides an explanation of product characteristicsSection 7 provides information on auxiliary data used in creation of theproductSection 8 provides document citation informationSection 9 provides document acknowledgmentsSection 10 provides User Services contact informationAppendix A provides a table of default file characteristicsAppendix B provides a list of metadata fieldsAppendix C provides a list of acronymsThe References section contains a list of reference documents-4-LSDS-1619Version 4.0

Section 22.1Known IssuesSurface ReflectanceThe missing Climate Modeling Grid (CMG) aerosol values can cause a “blockiness”artifact in the Landsat 8-9 Surface Reflectance data products. To prevent this, LaSRCinterpolates missing aerosol grid values to fit continuously within the Landsat grid cells.While making the resulting data product appear consistent, interpolated values are notdirect measurements. Therefore, a Quality Assessment (QA) band(SR QA AEROSOL) is provided with the Surface Reflectance data product that showswhether the aerosol was a valid retrieval, or it was interpolated from the surroundinggrid points.LaSRC uses an internal algorithm to identify water pixels. Some low-radiance specklingmay appear over water in some Surface Reflectance bands. Shown in Figure 2-1, thespeckling exists over water in Band 7 (shortwave infrared 2). The images were createdusing Landsat 8 data (Path 13, Row 10) acquired on March 30, 2013.Figure 2-1. Landsat 8 Top of Atmosphere (TOA) Reflectance for the SWIR-2 band(left) and an example of the speckle observed in the corresponding SurfaceReflectance product (right)For a full list of known issues in Collection 2 Level 2 science products, please -collection-2-known-issues.-5-LSDS-1619Version 4.0

Section 33.1Caveats and ConstraintsSurface Reflectance1. Landsat 8-9 Collection 2 Surface Reflectance (SR) products are generated onlyfrom scenes that have been processed to Tier 1 (T1) or Tier 2 (T2); Real-Time (RT)data cannot be used to create SR products. When acquired, scenes are processedand placed into the RT Tier. Landsat 9 data are processed to T1 or T2 upondownlink, usually within 4-6 hours of data acquisition. For Landsat 8, however,follow-on processing to apply refined Thermal Infrared Sensor (TIRS) instrument lineof sight model parameters takes place 14 to 16 days later, and the scenes are thenplaced into T1 or T2. The SR processing is done within 24 hours of availability ofT1/T2 and necessary auxiliary data. In summary, Landsat 8 Collection 2 SR databecome available 15 to 17 days after data acquisition. Visit the LandsatCollection 2 Generation Timeline for a visual look at this timeframe.2. The following date range applies to the availability of Landsat archive for SurfaceReflectance processing, with the exceptions noted in #3 below: Landsat 8 OLI/TIRS: March 18, 2013 to present Landsat 9 OLI/TIRS: October 31, 2021 to present3. Landsat 8-9 data cannot be processed to Surface Reflectance between specificdates. More information pertaining to the auxiliary data characteristics andavailability is shown in Section 7. The most up-to-date information regarding datagaps is in the “Caveats and Constraints” section of at/landsat-collection-2-surface-reflectance.4. Landsat 8-9 OLI Band 8 (panchromatic band) is not processed to Top ofAtmosphere or Surface Reflectance.5. SR is not run on scenes with a solar zenith angle of greater than 76º. The primaryphysical issues with retrieving SR from high solar zenith angles (low sun angle)include: Solar elevation varies more near the poles [1], especially when relyingupon sun-synchronous observations. Lower solar elevations at high latitudes results in longer atmosphericpaths (i.e., more scattering) [1]. The degree of uncertainty in SR retrieval greatly increases, from beingnegligible to highly inaccurate, at solar zenith angle 76 degrees.References: [1] Campbell, J.W., & Aarup, T. (1989). Photosynthetically availableradiation at high latitudes. Limnology and Oceanography, 34(8), 14901499. http://dx.doi.org/10.4319/lo.1989.34.8.1490.6. For reasons mentioned in #5 above, the Surface Reflectance data processed overhigh latitudes ( 65º) have larger uncertainty and should be analyzed carefully.-6-LSDS-1619Version 4.0

7. Corrections from Landsat 8-9 OLI Bands 1 and 2 (coastal aerosol and blue bands,respectively) should not be used for analysis, as they are already used within thealgorithm to perform aerosol inversion tests, making them potentially unreliable.8. Users are cautioned against using pixels flagged as high aerosol content. SeeSection 6.1.3 for details.9. Aerosol retrieval is attempted over all pixels, although a separate routine is used forpixels flagged by LaSRC as water. These conditions are detailed in the Aerosol QAband (Section 6.1.3).10. There are additional adverse conditions that can affect the efficacy of Landsat 8-9SR retrievals, such as:3.2 Hyper-arid or snow-covered regions Low sun angle conditions Coastal regions where land area is small relative to adjacent water Areas with extensive cloud contaminationSurface Temperature1. For the reasons mentioned in Section 3.1, Landsat 8 Collection 2 ST productsbecome available 15 to 17 days after data acquisition.2. Landsat 8-9 TIRS-only data (LT08/LT09) cannot be processed to TOABrightness Temperature or Surface Temperature.3. The Advanced Spaceborne Thermal Emission and Reflection Radiometer GlobalEmissivity Dataset (ASTER GED) by Land Processes Distributed Active ArchiveCenter (LP DAAC) is used in the ST algorithm for TIRS data. Where ASTERGED data is missing, there will be missing data in the Landsat ST product. Figure3-1 shows a map of ASTER GED emissivity tiles coverage.Note: To investigate the availability of any given pixel, the “ASTER GlobalEmissivity Dataset 100 meter HDF5 V003” data can be attained fromhttps://www.doi.org/10.5067/Community/ASTER GED/AG100.003.-7-LSDS-1619Version 4.0

Figure 3-1. Spatial Extent of ASTER GED Emissivity4. Goddard Earth Observing System, Version 5 (GEOS-5) Forward Processing forInstrument Teams (FP-IT) data are used in the Single Channel algorithm foratmospheric correction of Landsat 8-9 data.5. Atmospheric auxiliary data used for processing a Level 1 product into the ST aredescribed in the Landsat Atmospheric Auxiliary Data Data Format Control Book(DFCB).6. Data products must contain both sunlit optical and thermal data (e.g., LC08products for Landsat 8, LC09 products for Landsat 9) to be successfullyprocessed to Surface Temperature, as Landsat NDVI and Normalized DifferenceSnow Index (NDSI) are required to temporally adjust the ASTER GED product tothe target Landsat scene. Therefore, nighttime acquisitions cannot be processedto Surface Temperature.A known error exists in the Landsat Surface Temperature retrievals relative to cloudsand possibly cloud shadows. The characterization of these issues has beendocumented by Cook et al., 2014 (see the References section for more details).-8-LSDS-1619Version 4.0

Section 4Product AccessLandsat 8-9 SR and ST products can be downloaded from EarthExplorer (EE). Thedatasets for each sensor are located under the Landsat category, Landsat Collection2 Level 2 subcategory: Landsat 8-9 OLI/TIRS C2 L2.After reviewing the search results and selecting a scene, users can download all bandsor select and download selected bands.Direct access to Landsat 8-9 Collection 2 SR and ST is also available via commercialcloud environment. For additional information, please visit Landsat Commercial CloudData Access.Visit the Landsat Data Access webpage for information about downloading Landsatproducts.-9-LSDS-1619Version 4.0

Section 5Product PackagingLandsat Collection 2 L2SP can be downloaded as individual bands as Cloud OptimizedGeoreferenced Tagged Image File Format (GeoTIFF) (COG) files. The filenames arestructured as the Level 2 product identifier (ProductID) appended with the suffix “ SR ”followed by a band designation to denote the Surface Reflectance transformation. TheSurface Temperature filenames use ProductID appended with the suffix “ ST ” followedby the band designation.Following are the components of a typical ProductID:LXSS LLLL PPPRRR YYYYMMDD yyyymmdd CX TX(e.g., LC08 L2SP 039037 20150728 20200318 02 T1)LXSSLLLLLandsatSensor (“O” OLI; “T” TIRS; “C” OLI/TIRS)Satellite (“08” Landsat 8, “09” Landsat 9)Processing correction level (“L2SP” if SR and ST are generated or “L2SR”if ST could not be generated)PPP PathRRR RowYYYY Year of acquisitionMM Month of acquisitionDDDay of acquisitionyyyy Year of Level 2 processingmm Month of Level 2 processingddDay of Level 2 processingCXCollection number (“02”)TXCollection category ( “T1” Tier 1; “T2” Tier 2)The suffixes that append the file names are listed in Table 6-1, and typically include aband type (SR, ST, QA), a band name, and a file format extension (‘TIF’, ‘xml’, ‘txt’,‘json’).- 10 -LSDS-1619Version 4.0

Section 66.1Product CharacteristicsBand SpecificationsCollection 2 Landsat 8-9 L2SP are generated at 30-meter spatial resolution on aUniversal Transverse Mercator (UTM) or Polar Stereographic (PS) mapping grid. Table6-1 lists the specifications for Collection 2 L2SP bands. All packages include ExtensibleMarkup Language (XML) and JavaScript Object Notation (JSON)-based metadata.Collection 2 Landsat 8-9 L2SP are delivered in files named with the ProductID andappended with “ SR ” or “ ST ” followed by the band designation. The default fileformat is COG. The QA PIXEL, SR QA AEROSOL, and QA RADSAT bands aredelivered as bit-packed layers.The ST intermediate bands are delivered with the ST product. These layer bands areused in the creation of the ST band. The ST TRAD band contains the Level 1 thermalband converted to thermal surface radiance. The ST URAD and ST DRAD bandsrespectively contain the upwelled and downwelled thermal radiance. The ST ATRANband contains the atmospheric transmittance. The ST EMIS band and ST EMSD bandcontain the calculated surface emissivity and its expected standard deviation.The ST QA band contains the uncertainty of the ST band, in Kelvin. The ST CDISTband contains the distance of the pixel from the nearest cloud labeled in the QA PIXELband, in kilometers.- 11 -LSDS-1619Version 4.0

Band DesignationProductID SR B1ProductID SR B2ProductID SR B3ProductID SR B4ProductID SR B5ProductID SR B6ProductID SR B7ProductID ST B10Band NameBand 1 SRBand 2 SRBand 3 SRBand 4 SRBand 5 SRBand 6 SRBand 7 SRBand 10 STLevel 2 PixelProductID QA PIXELQuality BandProductID SR QA AEROSOLAerosol QARadiometricProductID QA RADSATSaturation QASurfaceProductID ST QATemperatureUncertaintyThermalProductID ST TRADRadianceUpwelledProductID ST URADRadianceDownwelledProductID ST DRADRadianceAtmosphericProductID ST ATRANTransmittanceEmissivityProductID ST EMISestimated fromASTER GEDEmissivityProductID ST EMSDstandarddeviationPixel distance toProductID ST CDISTcloudLevel 2 MetadataProductID MTLfileData TypeUnitsDataRangeMultiplicativeScale FactorAdditive Bit IndexUINT8Bit Index0 - 2551 - 2551NANAUINT16Bit Index0 - 655350 - 3829NANANAINT16Kelvin0 - 327670 - 32767-99990.01NA0 – 22000-99990.001NA0 – 28000-99990.001NA0 - 28000-99990.001NAINT16INT167273 - 436367273 – 436367273 - 436367273 - 436367273 - 436367273 - 436367273 - 43636293 - UINT16UINT16INT161 - 655351 - 655351 - 655351 - 655351 - 655351 - 655351 - 655351 - 65535Valid Range1 - 65535 21824 – 65534W/(m2.sr.μm)/0 - 22000DN2W/(m .sr.μm)/0 - 28000DNW/(m2.sr.μm)/0 - -0.2-0.2-0.2-0.2149INT16Unitless0 - 100000 - 10000-99990.0001NAINT16Unitless0 - 100000 - 10000-99990.0001NAINT16Unitless0 - 327670 – 10000-99990.0001NAINT16Kilometers0 - 240000 – 24000-99990.01NANANANANANANANATable 6-1. Collection 2 (C2) Landsat 8-9 Level 2 Science Products (L2SP) Band Specifications- 12 -LSDS-1619Version 4.0

6.1.1 Cloud and Cloud Shadow SpecificationsThe Level 2 Pixel Quality Assessment band (QA PIXEL) includes the information fromthe Level 1 Quality Assessment (QA PIXEL) band which is carried through unchangedinto Level 2 product package. The Cloud Confidence, Cloud Shadow, and Snow/Iceflags derived from the CFMask algorithm version 3.3.1. In order to support higher levelscience data products, water values are re-calculated, and high-confidence cloud pixelsare dilated, making QA PIXEL comparable to the legacy CFMask bands. CloudShadow, Snow/Ice, and Cirrus Confidence flags in bits 10-15 each have a reservedvalue for future improvements. They match the respective flags in bits 2, 4, and 5 andmay be used interchangeably. Specific details about Landsat Collection 2 Cloud CoverAssessment (CCA) algorithm can be found in Section 4.4.18 of the LSDS-1747 Landsat8-9 OLI/TIRS Calibration / Validation Algorithm Description Document.Table 6-2 describes the bit assignments for the QA PIXEL band. Most commonQA PIXEL bit values are given in Table 6-3.BitFlag Description0Fill1Dilated Cloud2Cirrus3Cloud4Cloud Shadow5Snow6Clear7Water8-9Cloud Confidence10-11Cloud Shadow Confidence12-13Snow/Ice Confidence14-15Cirrus ConfidenceValues0 for image data1 for fill data0 for cloud is not dilated or no cloud1 for cloud dilation0 for Cirrus Confidence: no confidence levelset or Low Confidence1 for high confidence cirrus0 for cloud confidence is not high1 for high confidence cloud0 for Cloud Shadow Confidence is not high1 for high confidence cloud shadow0 for Snow/Ice Confidence is not high1 for high confidence snow cover0 if Cloud or Dilated Cloud bits are set1 if Cloud and Dilated Cloud b

Table 6-4. Landsat 8-9 Radiometric Saturation Quality Assessment (QA_RADSAT) Bit . production processing to create appl ications-ready datasets. To alleviate this burden on . Landsat 8-9 OLI/TIRS (Original) research grant NASA GSFC, MEaSUREs NASA GSFC Principal Investigator Jeff Masek, NASA Eric Vermote, NASA .

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