DEA Surface Reflectance (Landsat 8 OLI-TIRS)
DEA Surface Reflectance (Landsat 8 OLI-TIRS)
- Version:
- Type:
Baseline, Raster
- Resolution:
15-30 m
- Coverage:
19 Mar 2013 to Present
- Data updates:
Daily frequency, Ongoing
About
DEA Surface Reflectance (Landsat 8 OLI-TIRS) is part of a suite of Digital Earth Australia (DEA)’s Surface Reflectance datasets that represent the vast archive of images captured by the US Geological Survey (USGS) Landsat and European Space Agency (ESA) Sentinel-2 satellite programs, validated, calibrated, and adjusted for Australian conditions — ready for easy analysis.
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Key specifications
For more specifications, see the Specifications tab.
Technical name |
Geoscience Australia Landsat 8 OLI-TIRS Analysis Ready Data Collection 3 |
Bands |
22 bands of data (nbart_coastal_aerosol, nbart_blue, and more) |
Catalogue ID |
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Currency |
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Collection |
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Tags |
geoscience_australia_landsat_collection_3, analysis_ready_data, satellite_images, earth_observation |
Licence |
Cite this product
Data citation |
Fuqin, Li., Jupp, D.L.B., Sixsmith, J., Wang, L., Dorj, P., Vincent, A., Alam, I., Hooke, J., Oliver, S., Thankappan, M. 2019. GA Landsat 8 OLI/TIRS Analysis Ready Data Collection 3. Geoscience Australia, Canberra. https://pid.geoscience.gov.au/dataset/ga/132317
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Publications
Li, F., Jupp, D. L. B., Reddy, S., Lymburner, L., Mueller, N., Tan, P., & Islam, A. (2010). An evaluation of the use of atmospheric and BRDF correction to standardize Landsat data. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 3(3), 257–270. https://doi.org/10.1109/JSTARS.2010.2042281
Li, F., Jupp, D. L. B., Thankappan, M., Lymburner, L., Mueller, N., Lewis, A., & Held, A. (2012). A physics-based atmospheric and BRDF correction for Landsat data over mountainous terrain. Remote Sensing of Environment, 124, 756–770. https://doi.org/10.1016/j.rse.2012.06.018
Background
The United States Geological Survey’s (USGS) Landsat satellite program has been capturing images of the Australian continent for more than 30 years. This data is highly useful for land and coastal mapping studies.
In particular, the light reflected from the Earth’s surface (surface reflectance) is important for monitoring environmental resources – such as agricultural production and mining activities – over time.
We need to make accurate comparisons of imagery acquired at different times, seasons and geographic locations. However, inconsistencies can arise due to variations in atmospheric conditions, sun position, sensor view angle, surface slope and surface aspect. These need to be reduced or removed to ensure the data is consistent and can be compared over time.
What this product offers
This product takes Landsat 8 imagery captured over the Australian continent and corrects for inconsistencies across land and coastal fringes. The result is accurate and standardised surface reflectance data, which is instrumental in identifying and quantifying environmental change.
The imagery is captured using the Operational Land Imager (OLI) and Thermal Infra-Red Scanner (TIRS) sensors aboard Landsat 8.
This product is a single, cohesive Analysis Ready Data (ARD) package, which allows you to analyse surface reflectance data as is, without the need to apply additional corrections.
It contains three sub-products that provide corrections or attribution information:
The resolution is a 30 m grid based on the USGS Landsat Collection 1 archive.
Applications
The development of derivative products to monitor land, inland waterways and coastal features, such as:
urban growth
coastal habitats
mining activities
agricultural activity (e.g. pastoral, irrigated cropping, rain-fed cropping)
water extent
The development of refined information products, such as:
areal units of detected surface water
areal units of deforestation
yield predictions of agricultural parcels
Compliance surveys
Emergency management
Technical information
Operational Land Imager (OLI) and Thermal Infrared Sensor (TIRS)
OLI is a push-broom sensor with a four-mirror telescope and 12-bit quantisation. OLI collects data for visible, near infrared, and short wave infrared spectral bands as well as a panchromatic band.
TIRS measures land surface temperature in two thermal bands with new technology that applies quantum physics to detect heat.
The Analysis Ready Data concept
The Analysis Ready Data (ARD) package allows you to get up and running with your analysis as quickly as possible with minimal data preparation and additional input. This makes it simpler for you to develop applications and for the database to execute queries.
The satellite data has been processed to a minimum set of requirements and organised into a form that allows immediate analysis and interoperability through time and with other datasets. It has been adapted from CEOS Analysis Ready Data (CARD4L).
The technical report containing the data summary for the Phase 1 DEA Surface Reflectance Validation is available.
ARD sub-products
This sub-product produces standardised optical surface reflectance data using robust physical models which correct for variations and inconsistencies in image radiance values. Corrections are performed using Nadir corrected Bi-directional reflectance distribution function Adjusted Reflectance (NBAR).
This sub-product performs the same function as Surface Reflectance (Landsat 8 OLI-TIRS NBAR), but also applies terrain illumination correction.
The NBAR and NBART sibling products depend upon the OA product to provide accurate and reliable contextual information about the Landsat data. This ‘data provenance’ provides a chain of information which allows the data to be replicated or utilised by derivative applications. It takes a number of different forms, including satellite, solar and surface geometry and classification attribution labels.
Lineage
This product is derived from the USGS Landsat Collection 1 archive.
The Moderate Resolution Imaging Spectroradiometer (MODIS) MCD43A1 Version 6 Bidirectional Reflectance Distribution Function and Albedo (BRDF/Albedo) Model Parameters dataset was provided by the National Aeronautics and Space Administration (NASA). It was produced daily using 16 days of Terra and Aqua MODIS data at 500 m resolution. See USGS: MCD43A1, NASA: MODIS BRDF / Albedo Parameter, Schaaf et al. (2002)
The ozone data was provided by Environment Canada. See Environment Canada: Global Ozone Maps
The Aerosol Optical Thickness data was provided by the Commonwealth Scientific and Industrial Research Organisation (CSIRO). See Qin et al. (2015)
The Precipitable Water for Entire Atmosphere data was provided by the National Oceanic and Atmospheric Administration (NOAA) / Earth System Research Laboratory (ESRL) / Physical Sciences Division (PSD). See Kalnay et al. (1996)
The baseline Digital Surface Model (DSM) data produced from the Shuttle Radar Topography Mission (SRTM) was provided by the National Geospatial-Intelligence Agency (NGA). See NGA: SRTM, NASA: SRTM
Level 1 Collection 1 data was provided by the United States Geological Survey (USGS)’s Earth Resources Observation and Science (EROS) Center. See USGS: EROS, USGS: Landsat Collection 1
Processing steps
Software
References
Berk, A., Conforti, P., Kennett, R., Perkins, T., Hawes, F., & van den Bosch, J. (2014, June 13). MODTRAN6: A major upgrade of the MODTRAN radiative transfer code (M. Velez-Reyes & F. A. Kruse, Eds.). https://doi.org/10.1117/12.2050433
Dymond, J. R., & Shepherd, J. D. (1999). Correction of the topographic effect in remote sensing. IEEE Transactions on Geoscience and Remote Sensing, 37(5), 2618–2619. https://doi.org/10.1109/36.789656
Hudson, S. R., Warren, S. G., Brandt, R. E., Grenfell, T. C., & Six, D. (2006). Spectral bidirectional reflectance of Antarctic snow: Measurements and parameterization. Journal of Geophysical Research, 111(D18), D18106. https://doi.org/10.1029/2006JD007290
Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., & Gandin, L. et al. (1996). The NCEP/NCAR 40-Year Reanalysis Project. Bulletin Of The American Meteorological Society, 77(3), 437-471. https://doi.org/10.1175/1520-0477(1996)077<0437:tnyrp>2.0.co;2
Li, F., Jupp, D. L. B., Reddy, S., Lymburner, L., Mueller, N., Tan, P., & Islam, A. (2010). An evaluation of the use of atmospheric and brdf correction to standardize landsat data. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 3(3), 257–270. https://doi.org/10.1109/JSTARS.2010.2042281
Li, F., Jupp, D. L. B., Thankappan, M., Lymburner, L., Mueller, N., Lewis, A., & Held, A. (2012). A physics-based atmospheric and BRDF correction for Landsat data over mountainous terrain. Remote Sensing of Environment, 124, 756–770. https://doi.org/10.1016/j.rse.2012.06.018
Qin, Y., Mitchell, R., & Forgan, B. W. (2015). Characterizing the aerosol and surface reflectance over Australia using AATSR. IEEE Transactions on Geoscience and Remote Sensing, 53(11), 6163–6182. https://doi.org/10.1109/TGRS.2015.2433911
Schaaf, C., Gao, F., Strahler, A., Lucht, W., Li, X., & Tsang, T. et al. (2002). First operational BRDF, albedo nadir reflectance products from MODIS. Remote Sensing Of Environment, 83(1-2), 135-148. https://www.doi.org/10.1016/s0034-4257(02)00091-3
SZA. (2011). Retrieved May 2019, from http://sacs.aeronomie.be/info/sza.php
Zhu, Z., Wang, S., & Woodcock, C. (2015). Improvement and expansion of the Fmask algorithm: cloud, cloud shadow, and snow detection for Landsats 4–7, 8, and Sentinel 2 images. Remote Sensing Of Environment, 159, 269-277. https://doi.org/10.1016/j.rse.2014.12.014
Zhu, Z., & Woodcock, C. E. (2012). Object-based cloud and cloud shadow detection in Landsat imagery. Remote Sensing of Environment, 118, 83–94. https://doi.org/10.1016/j.rse.2011.10.028
Accuracy
For detailed information on accuracy and limitations, refer to the sub-products’ pages:
Quality assurance
For detailed information on quality assurance, refer to the sub-products’ pages:
Bands
Bands are distinct layers of data within a product that can be loaded using the Open Data Cube (on the DEA Sandbox or NCI) or DEA’s STAC API. Here are the bands of the product: ga_ls8c_ard_3.
Aliases |
Resolution |
No-data |
Units |
Type |
Description |
|
---|---|---|---|---|---|---|
nbart_coastal_aerosol |
nbart_band01
coastal_aerosol
|
30 |
-999 |
- |
int16 |
- |
nbart_blue |
nbart_band02
blue
|
30 |
-999 |
- |
int16 |
- |
nbart_green |
nbart_band03
green
|
30 |
-999 |
- |
int16 |
- |
nbart_red |
nbart_band04
red
|
30 |
-999 |
- |
int16 |
- |
nbart_nir |
nbart_band05
nir
nbart_common_nir
|
30 |
-999 |
- |
int16 |
- |
nbart_swir_1 |
nbart_band06
swir_1
nbart_common_swir_1
swir1
|
30 |
-999 |
- |
int16 |
- |
nbart_swir_2 |
nbart_band07
swir_2
nbart_common_swir_2
swir2
|
30 |
-999 |
- |
int16 |
- |
nbart_panchromatic |
nbart_band08
panchromatic
|
15 |
-999 |
- |
int16 |
- |
oa_fmask |
fmask
|
30 |
0 |
- |
uint8 |
- |
oa_nbart_contiguity |
nbart_contiguity
|
30 |
255 |
- |
uint8 |
- |
oa_azimuthal_exiting |
azimuthal_exiting
|
30 |
NaN |
- |
float32 |
- |
oa_azimuthal_incident |
azimuthal_incident
|
30 |
NaN |
- |
float32 |
- |
oa_combined_terrain_shadow |
combined_terrain_shadow
|
30 |
255 |
- |
uint8 |
- |
oa_exiting_angle |
exiting_angle
|
30 |
NaN |
- |
float32 |
- |
oa_incident_angle |
incident_angle
|
30 |
NaN |
- |
float32 |
- |
oa_relative_azimuth |
relative_azimuth
|
30 |
NaN |
- |
float32 |
- |
oa_relative_slope |
relative_slope
|
30 |
NaN |
- |
float32 |
- |
oa_satellite_azimuth |
satellite_azimuth
|
30 |
NaN |
- |
float32 |
- |
oa_satellite_view |
satellite_view
|
30 |
NaN |
- |
float32 |
- |
oa_solar_azimuth |
solar_azimuth
|
30 |
NaN |
- |
float32 |
- |
oa_solar_zenith |
solar_zenith
|
30 |
NaN |
- |
float32 |
- |
oa_time_delta |
time_delta
|
30 |
NaN |
- |
float32 |
- |
For all ‘nbart_’ bands, Surface Reflectance is scaled between 0 and 10,000.
Product information
This metadata provides general information about the product.
Product ID |
ga_ls8c_ard_3
|
Used to load data from the Open Data Cube. |
Short name |
DEA Surface Reflectance (Landsat 8 OLI-TIRS) |
The name that is commonly used to refer to the product. |
Technical name |
Geoscience Australia Landsat 8 OLI-TIRS Analysis Ready Data Collection 3 |
The full technical name that refers to the product and its specific provider, sensors, and collection. |
Version |
3.0.0 |
The version number of the product. |
Lineage type |
Baseline |
Baseline products are produced directly from satellite data. |
Spatial type |
Raster |
Raster data consists of a grid of pixels. |
Spatial resolution |
15-30 m |
The size of the pixels in the raster. |
Temporal coverage |
19 Mar 2013 to Present |
The time span for which data is available. |
Update frequency |
Daily |
The expected frequency of data updates. Also called ‘Temporal resolution’. |
Update activity |
Ongoing |
The activity status of data updates. |
Currency |
Currency is a measure based on data publishing and update frequency. |
|
Latest update date |
See Table A of the report. |
|
Catalogue ID |
The Data and Publications catalogue (eCat) ID. |
|
Licence |
See the Credits tab. |
Product categorisation
This metadata describes how the product relates to other DEA products.
Collection |
|
Tags |
geoscience_australia_landsat_collection_3, analysis_ready_data, satellite_images, earth_observation |
Access the data
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Learn how to use the DEA Explorer. |
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Data sources |
Learn how to access the data via AWS. |
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Code examples |
Learn how to use the DEA Sandbox. |
Version history
No previous versions are available.
Frequently asked questions
Why doesn’t DEA make Landsat thermal bands available to users?
Landsat satellite sensors not only collect data in the short-wave spectrum but also collect data into the thermal infrared bands. The USGS makes this data available in the form of a surface temperature and emissivity product: Landsat Collection 2 Surface Temperature. It provides this separately to the surface reflectance products.
This USGS Surface Temperature product is a global product that uses global datasets to perform corrections on the data that are collected by the satellite sensors. The land surface temperature outputs are very sensitive to the atmospheric profile data that is used to perform the correction. For the global analysis, the NASA Modern Era Retrospective-Analysis for Research and Applications (MERRA) atmospheric data is used to provide values for height, air temperature, and humidity. While this dataset works well for a global correction, studies over Australia have shown that the correction can be improved when higher resolution datasets are considered (Li et al, 2015).
DEA’s ARD product provides high-quality data corrections for Australian conditions. At present, we do not produce a custom land surface temperature dataset for Australia, and so we have not included the thermal bands in our ARD package.
If you would like to use USGS Landsat thermal data directly, we provide a Jupyter notebook that shows you how to combine DEA ARD data with USGS thermal data.
Acknowledgments
This research was undertaken with the assistance of resources from the National Computational Infrastructure (NCI), which is supported by the Australian Government.
Landsat level 0 and level 1 data courtesy of the U.S. Geological Survey.
The authors would like to thank the following organisations:
National Aeronautics and Space Administration (NASA)
Environment Canada
The Commonwealth Scientific and Industrial Research Organisation (CSIRO)
National Oceanic and Atmospheric Administration (NOAA) / Earth System Research Laboratories (ESRL) / Physical Sciences Laboratory (PSD)
The National Geospatial-Intelligence Agency (NGA)
The United States Geological Survey (USGS) / Earth Resources Observation and Science (EROS) Center
Spectral Sciences Inc.
License and copyright
© Commonwealth of Australia (Geoscience Australia).
Released under Creative Commons Attribution 4.0 International Licence.