DEA Surface Reflectance (Sentinel-2C MSI)

DEA Surface Reflectance (Sentinel-2C MSI)

ga_s2cm_ard_3

Version:

3.2.1

Type:

Baseline, Raster

Resolution:

10-60 m

Coverage:

21 Jan 2025 to Present

Data updates:

Daily frequency, Ongoing

../../../_images/surface_reflectance_2_NBARTa_1.png

About

DEA Surface Reflectance Sentinel-2C Multispectral Instrument (MSI) is part of a suite of Digital Earth Australia’s (DEA) Surface Reflectance datasets that represent the vast archive of images which have been captured by the US Geological Survey (USGS) Landsat and European Space Agency (ESA) Sentinel-2 satellite programs, which have been 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 Sentinel-2C MSI Analysis Ready Data Collection 3

Bands

27 bands: nbart_coastal_aerosol, nbart_blue, and more

DOI

10.26186/150143

Collection

Geoscience Australia Sentinel-2 Collection 3

Licence

Creative Commons Attribution 4.0 International Licence

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 European Space Agency (ESA) operates the Sentinel-2 series of medium-resolution satellites. These are the Sentinel-2A and Sentinel-2B satellites (since 2015) and Sentinel-2C (starting in 2025, to replace Sentinel-2A). The spectral bands and spatial resolution of Sentinel-2 are similar to those of the Landsat series, but Sentinel-2 has a higher revisit frequency and spatial coverage. A combination of Sentinel-2 and Landsat data can provide good spatial and temporal coverage of the Earth’s surface and provide useful information to monitor environmental resources over time, such as agricultural production and mining activities. However, the raw remotely sensed data received by these satellites in the solar spectral range do not directly characterise the underlying reflectance of surface objects. The data are modified by the atmosphere, variation of solar and sensor positions as well as surface anisotropic conditions. To make accurate comparisons of imagery acquired at different times, seasons and geographic locations, and detect the change of surface, it is necessary to remove/reduce these effects to ensure the data are consistent and can be compared over time.

What this product offers

This product takes Sentinel-2C 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 Multispectral Instrument (MSI) sensor aboard Sentinel-2C.

This product is a single, cohesive Analysis Ready Data (ARD) package, which allows the analysis of surface reflectance data as is, without the need to apply additional corrections.

It contains two sub-products that provide corrections or attribution information:

The resolution is a 10/20/60 m grid based on the ESA Level 1C archive. Note: DEA produces NBAR as part of the Landsat ARD. This product is not produced as part of the Sentinel-2 ARD.

This Collection 3 (C3) product and has been created by reprocessing Collection 1 (C1) and making improvements to the processing pipeline and packaging. See the History tab for more details.

The introduction of a maturity concept.

The Collection 3 product is comprised of data produced to varying degrees of maturity. The maturity of a dataset is dictated by the quality of the ancillary information, such as BRDF and atmospheric data, used to generate the product. The maturity levels are Near Real Time (NRT), Interim and Final. The maturity level is designated in the filename and in the metadata.

  • Near Real Time (NRT) is a rapid ARD product produced < 48 hours after image capture.

  • Interim ARD – If there are extended delays (>18 days) in delivery of inputs to the ARD model, interim production is utilised until the issue is resolved.

  • Final ARD - As the higher quality ancillary datasets become available, a “Final” version of the Sentinel 2 ARD data is produced, which replaces the NRT or interim product.

Applications

This product can be used for:

  • 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

Multispectral Instrument (MSI)

MSI is a push-broom sensor with A Three-Mirror Anastigmat (TMA) telescope with a pupil diameter equivalent to 150 mm, isostatically mounted on the platform to minimise thermo-elastic distortions. Surface Reflectance values range between 0 and 10000. MSI collects data for visible, near infrared, and short wave infrared spectral bands.

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

  1. DEA Surface Reflectance NBART (Sentinel-2C MSI)

The sub-product produces standardised optical surface reflectance data using robust physical models which correct for variations and inconsistencies in the image of top atmospheric reflectance values. Corrections are performed using Nadir corrected Bidirectional reflectance distribution function Adjusted Reflectance (NBAR) with an additional terrain illumination correction applied (NBART).

  1. DEA Surface Reflectance OA (Sentinel-2C MSI)

The NBART product depends upon the Observation Attributes (OA) product to provide accurate and reliable contextual information about the Sentinel-2C data. This ‘data provenance’ provides a chain of information which allows the data to be replicated or utilised by derivative applications. The OA takes a number of different forms, including satellite, solar and surface geometry and classification attribution labels.

Lineage

This product is derived from the ESA Sentinel-2C level 1C 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 1C Collection 1 data was provided by the European Space agency’s Copernicus data hub, see https://scihub.copernicus.eu/

Processing steps

  1. Longitude and Latitude Calculation

  2. Satellite and Solar Geometry Calculation

  3. Aerosol Optical Thickness Retrieval

  4. BRDF Shape Function Retrieval

  5. Ozone Retrieval

  6. Elevation Retrieval and Smoothing

  7. Slope and Aspect Calculation

  8. Incidence and Azimuthal Incident Angles Calculation

  9. Exiting and Azimuthal Exiting Angles Calculation

  10. Relative Slope Calculation

  11. Terrain Occlusion Mask

  12. MODTRAN

  13. Atmospheric Correction Coefficients Calculation

  14. Bilinear Interpolation of Atmospheric Correction Coefficients

  15. Surface Reflectance Calculation (NBAR + Terrain Illumination Correction)

  16. Function of Mask (Fmask)

  17. Contiguous Spectral Data Mask Calculation

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

Product ID

The Product ID is ga_s2cm_ard_3. This ID is used to load data from the Open Data Cube (ODC), for example dc.load(product="ga_s2cm_ard_3", ...)

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.

Type

Units

Resolution

No-data

Aliases

Description

nbart_coastal_aerosol

int16

-

60

-999

nbart_band01
coastal_aerosol

NBART surface reflectance useful for shallow water and fine atmospheric particles like dust and smoke. Equivalent wavelength: 444.2 nm; Bandwidth: 21 nm.

nbart_blue

int16

-

10

-999

nbart_band02
blue

NBART surface reflectance for the blue spectral band. Equivalent wavelength: 489.0 nm; Bandwidth: 65 nm.

nbart_green

int16

-

10

-999

nbart_band03
green

NBART surface reflectance for the green spectral band. Equivalent wavelength: 560.6 nm; Bandwidth: 36 nm.

nbart_red

int16

-

10

-999

nbart_band04
red

NBART surface reflectance for the red spectral band. Equivalent wavelength: 666.5 nm; Bandwidth: 30 nm.

nbart_red_edge_1

int16

-

20

-999

nbart_band05
red_edge_1

NBART surface reflectance of the near-infrared (NIR) range useful for detecting vegetation. Equivalent wavelength: 707.1 nm; Bandwidth: 15 nm.

nbart_red_edge_2

int16

-

20

-999

nbart_band06
red_edge_2

NBART surface reflectance of the near-infrared range (NIR) useful for detecting vegetation. Equivalent wavelength: 741.1 nm; Bandwidth: 15 nm.

nbart_red_edge_3

int16

-

20

-999

nbart_band07
red_edge_3

NBART surface reflectance of the near-infrared (NIR) range useful for detecting vegetation. Equivalent wavelength: 784.7 nm; Bandwidth: 21 nm.

nbart_nir_1

int16

-

10

-999

nbart_band08
nir_1
nbart_common_nir

NBART surface reflectance of the near-infrared (NIR) range. Equivalent wavelength: 834.6 nm; Bandwidth: 114 nm.

nbart_nir_2

int16

-

20

-999

nbart_band8a
nir_2

NBART surface reflectance of the near-infrared (NIR) range which is narrower than ‘nbart_nir_1’. Equivalent wavelength: 865.6 nm; Bandwidth: 20 nm.

nbart_swir_2

int16

-

20

-999

nbart_band11
swir_2
nbart_common_swir_1
swir2

NBART surface reflectance of the short-wave infrared (SWIR-2) range. Equivalent wavelength: 1612.0 nm; Bandwidth: 89 nm.

nbart_swir_3

int16

-

20

-999

nbart_band12
swir_3
nbart_common_swir_2

NBART surface reflectance of the short-wave infrared (SWIR-3) range. Equivalent wavelength: 2191.3 nm; Bandwidth: 182 nm.

oa_s2cloudless_mask

uint8

Classification

60

0

s2cloudless_mask

The s2cloudless cloud mask band identifies the presence of clouds. Classification values: 0 = No cloud; 1 = Cloud.

oa_s2cloudless_prob

float64

-

60

NaN

s2cloudless_prob

The s2cloudless cloud probabilities band provides the probabilities of cloud presence as values between 0.0 and 1.0.

oa_fmask

uint8

Classification

20

0

fmask

Fmask: A categorical classification layer produced using the automated Fmask (‘Function of mask’) algorithm, used to mask out unwanted observations in satellite imagery (e.g. cloud or shadow). Classification values: 0 = null; 1 = clear; 2 = cloud; 3 = cloud shadow; 4 = snow; 5 = water.

oa_nbart_contiguity

uint8

Classification

10

255

nbart_contiguity

NBART contiguity: A layer indicating whether each pixel is ‘spectrally contiguous’, meaning that it contains valid observations in every spectral band. Classification values: 0 = non-contiguous; 1 = contiguous.

oa_azimuthal_exiting

float32

Degrees

20

NaN

azimuthal_exiting

Azimuthal exiting: The angle between true north and the exiting direction in the slope geometry.

oa_azimuthal_incident

float32

Degrees

20

NaN

azimuthal_incident

Azimuthal incident: The angle between true north and the incident direction in the slope geometry.

oa_combined_terrain_shadow

uint8

Classification

20

255

combined_terrain_shadow

Combined terrain shadow: Terrain shadow. Classification values: 0 = terrain shadow; 1 = not terrain shadow.

oa_exiting_angle

float32

Degrees

20

NaN

exiting_angle

Exiting angle: The angle between a ray reflected from a surface and the line perpendicular to the surface at the point of emergence.

oa_incident_angle

float32

Degrees

20

NaN

incident_angle

Incident angle: The angle between a ray incident on a surface and the line perpendicular to the surface at the point of incidence.

oa_relative_azimuth

float32

Degrees

20

NaN

relative_azimuth

Relative azimuth: The relative azimuth angle between the sun and view directions.

oa_relative_slope

float32

Degrees

20

NaN

relative_slope

Relative slope: The relative azimuth angle between the incident and exiting directions in the slope geometry.

oa_satellite_azimuth

float32

Degrees

20

NaN

satellite_azimuth

Satellite azimuth: The angle of the satellite’s position from true north; i.e. the angle between true north and a vertical circle passing through the satellite and the point being imaged on Earth.

oa_satellite_view

float32

Degrees

20

NaN

satellite_view

Satellite view or satellite zenith: The angle between the zenith and the satellite. (The zenith is the point in the sky or celestial sphere directly above the point being imaged on Earth.)

oa_solar_azimuth

float32

Degrees

20

NaN

solar_azimuth

Solar azimuth: The angle of the sun’s position from true north; i.e. the angle between true north and a vertical circle passing through the sun and the point being imaged on Earth.

oa_solar_zenith

float32

Degrees

20

NaN

solar_zenith

Solar zenith: The angle between the zenith and the centre of the sun’s disc.

oa_time_delta

float32

Seconds

20

NaN

time_delta

Timedelta: The time from satellite apogee (the point of orbit at which the satellite is furthest from the Earth).

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_s2cm_ard_3

Used to load data from the Open Data Cube.

Short name

DEA Surface Reflectance (Sentinel-2C MSI)

The name that is commonly used to refer to the product.

Technical name

Geoscience Australia Sentinel-2C MSI Analysis Ready Data Collection 3

The full technical name that refers to the product and its specific provider, sensors, and collection.

Version

3.2.1

The version number of the product. See the History tab.

Lineage type

Baseline

Baseline products are produced directly from satellite data.

Spatial type

Raster

Raster data consists of a grid of pixels.

Spatial resolution

10-60 m

The size of the pixels in the raster.

Temporal coverage

21 Jan 2025 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.

DOI

10.26186/150143

The Digital Object Identifier.

Catalogue ID

150143

The Data and Publications catalogue (eCat) ID.

Licence

Creative Commons Attribution 4.0 International Licence

See the Credits tab.

Product categorisation

This metadata describes how the product relates to other products.

Collection

Geoscience Australia Sentinel-2 Collection 3

Tags

geoscience_australia_sentinel_2_collection_3, analysis_ready_data, satellite_images, earth_observation, sentinel, european

Access the data

DEA Explorer

Learn how to use the DEA Explorer.

Data sources

Learn how to access the data via AWS.

Code examples

Learn how to use the DEA Sandbox.

Web services

Learn how to use DEA’s web services.

How to access Sentinel-2 data using the Open Data Cube

This product is contained in the Open Data Cube instance managed by Digital Earth Australia (DEA). This simplified process allows you to query data from its sub-products as part of a single query submitted to the database.

Introduction to DEA Surface Reflectance (Sentinel-2, Collection 3)

How to access DEA Maps

To view and access the data interactively via a web map interface:

  1. Visit DEA Maps

  2. Click Explore map data

  3. Select Baseline satellite data > DEA Surface Reflectance (Sentinel-2)

  4. Click Add to the map

Version history

Versions are numbered using the Semantic Versioning scheme (Major.Minor.Patch). Note that this list may include name changes and predecessor products.

v3.2.1

-

Current version

v1.0.0

of

DEA Surface Reflectance NBAR (Sentinel-2 MSI)

Acknowledgments

This research was undertaken with the assistance of resources from the National Computational Infrastructure (NCI), which is supported by the Australian Government.

Contains modified Copernicus Sentinel data 2015-present.

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.