TheAdvanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) is a Japaneseremote sensing instrument onboard theTerra satellite launched byNASA in 1999. It has been collecting data since February 2000.
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ASTER provides high-resolution images of Earth in 14 differentbands of theelectromagnetic spectrum, ranging fromvisible to thermalinfrared light. Theresolution of images ranges between 15 and 90 square meters. ASTER data is used to create detailedmaps of surface temperature of land,emissivity,reflectance, and elevation.[1]
In April 2008, the SWIR detectors of ASTER began malfunctioning and were publicly declared non-operational by NASA in January 2009. All SWIR data collected after 1 April 2008 has been marked as unusable.[2]
The ASTER GlobalDigital Elevation Model (GDEM) is available at no charge to users worldwide via electronic download.[3]
As of 2 April 2016, the entire catalogue of ASTER image data became publicly available online at no cost.[4] It can be downloaded with a free registered account from either NASA's Earth Data Search delivery system[5] or from theUSGS Earth Explorer delivery system.[6]
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| Band | Label | Wavelength (μm) | Resolution (m) | Nadir or backward | Description |
|---|---|---|---|---|---|
| B1 | VNIR_Band1 | 0.520 - 0.60 | 15 | Nadir | Visible green/yellow |
| B2 | VNIR_Band2 | 0.630 - 0.690 | 15 | Nadir | Visible red |
| B3N | VNIR_Band3N | 0.760–0.860 | 15 | Nadir | Near infrared |
| B3B | VNIR_Band3B | 0.760–0.860 | 15 | Backward | |
| B4 | SWIR_Band4 | 1.600–1.700 | 30 | Nadir | Short-wave infrared |
| B5 | SWIR_Band5 | 2.145–2.185 | 30 | Nadir | |
| B6 | SWIR_Band6 | 2.185–2.225 | 30 | Nadir | |
| B7 | SWIR_Band7 | 2.235–2.285 | 30 | Nadir | |
| B8 | SWIR_Band8 | 2.295–2.365 | 30 | Nadir | |
| B9 | SWIR_Band9 | 2.360–2.430 | 30 | Nadir | |
| B10 | TIR_Band10 | 8.125–8.475 | 90 | Nadir | Long-wave infrared or thermal IR |
| B11 | TIR_Band11 | 8.475–8.825 | 90 | Nadir | |
| B12 | TIR_Band12 | 8.925–9.275 | 90 | Nadir | |
| B13 | TIR_Band13 | 10.250–10.950 | 90 | Nadir | |
| B14 | TIR_Band14 | 10.950–11.650 | 90 | Nadir | |
On 29 June 2009, the Global Digital Elevation Model (GDEM) was released to the public.[8][9]A joint operation betweenNASA and Japan'sMinistry of Economy, Trade and Industry (METI), the Global Digital Elevation Model is the most complete mapping of the earth ever made, covering 99% of its surface.[10]The previous most comprehensive map, NASA'sShuttle Radar Topography Mission, covered approximately 80% of the Earth's surface,[11] with a global resolution of 90 meters,[12] and a resolution of 30 meters over the US.The GDEM covers the planet from 83 degrees North to 83 degrees South (surpassingSRTM's coverage of 56 °S to 60 °N), becoming the first earth mapping system that provides comprehensive coverage of the polar regions.[11] It was created by compiling 1.3 millionVNIR images taken by ASTER using single-pass[13]stereoscopiccorrelation techniques,[8] with terrain elevation measurements taken globally at 30-meter (98 ft) intervals.[10]
Despite the high nominal resolution, however, some reviewers have commented that the true resolution is considerably lower, and not as good as that of SRTM data, and serious artifacts are present.[14][15]
Some of these limitations have been confirmed by METI and NASA, who point out that the version 1 of the GDEM product is "research grade".[16]
![[icon]](/mt/?noimg=&dark=on&url=http%3a%2f%2fen.m.wikipedia.org%2fwiki%2fFile%3aWiki_letter_w_cropped.svg) | This sectionneeds expansion. You can help byadding missing information.(October 2011) |
During October 2011, version 2 of Global Digital Elevation Model was publicly released.[17] This is considered an improvement upon version 1. These improvements include increased horizontal and vertical accuracy,[18] better horizontal resolution, reduced presence of artifacts, and more realistic values over water bodies.[3] However, one reviewer still regards the Aster version 2 dataset, although showing 'a considerable improvement in the effective level of detail', to still be regarded as 'experimental or research grade' due to presence of artefacts.[19]A 2014 study[18] showed that over rugged mountainous terrain the ASTER version 2 data set can be a more accurate representation of the ground than the SRTM elevation model. The model was decommissioned as of August 5 2025.[20]
ASTER v3 was released on 5 August 2019.[21]
The improved GDEM V3 adds additional stereo-pairs, improving coverage and reducing the occurrence of artifacts. The refined production algorithm provides improved spatial resolution, increased horizontal and vertical accuracy. The ASTER GDEM V3 maintains the GeoTIFF format and the same gridding and tile structure as V1 and V2, with 30-meter postings and 1 x 1 degree tiles. Version 3 is claimed to have significant improvements over the previous release. Automated processing of 2.3 million scenes from the ASTER archive was used to create the ASTER GDEM, which included stereo-correlation to create individual scene-based ASTER DEMs, masking to remove cloudy pixels, stacking all cloud-screened DEMs, removing residual bad values and outliers, averaging selected data to create final pixel values.
