ASTER GDEM
ASTER GDEM is an easy-to-use, highly accurate DEM covering all
the land on earth, and available to all users regardless of size or
location of their target areas.Anyone can easily use the ASTER GDEM
to display a bird's-eye-view map or run a flight simulation, and
this should realize visually sophisticated maps. By utilizing the
ASTER GDEM as a platform, institutions specialized in disaster
monitoring, hydrology, energy, environmental monitoring etc. can
perform more advanced analysis. (See another
page,"Application")
For example, in "GEOSS Project(**)", DEM is considered to be an
important platform and thus ASTER GDEM is expected to make
significant contribution.
*Kashmir3DKashmir3D is a multi-functional free software for
making realistic bird's-eye views, landscape CG, flight simulation
movies and panorama mountain views. It supports almost all the
publicly available map/topographic data (sold or free) as well as
ASTER GDEM.
**GEOSSGEOSS is an ambitious international project involving
approximately 60 nations including the G8 member states (Japan
included) and approximately 30 international organizations, aiming
to establish within 10 years a comprehensive global-scale system
that coordinates various existing and future observation facilities
such as satellites and ground stations. This project is anticipated
to provide valuable information for policy makers.
Schedule
Outline of ASTER GDEM
* Global DEM for all the land area covered by ASTER.* Enhanced
accuracy due to the use of multiple ASTER images over the same
area.* User-friendly, allowing selective cropping.
Concept of ASTER G-DEM development
Format of ASTER DEM
File Name(Example of N35~36,E135~136)
ASTGTM_ N35E135_dem.tif
ASTGTM_ N35E135_num.tif
Output format
GeoTIFF, signed 16 bits
Geographic coordinates
Geographic latitude and longitude
Tile Size
3601-by-3601 pixels (1-by-1 degree)
Posting interval
1 arc-second
DN values
1m/DN referenced to the WGS84/EGM96 geoid-9999 for void pixels,
and 0 for sea water body
Stacking number or reference DEMSRTM3:-1,-2CDED:-6Alaska DEM:-11
etc.
Coverage
North 83 degrees to south 83 degrees, 22,600 tiles
*The detail is described in ReadMe file.
Comparison with other DEMs
ASTER GDEM
SRTM3*
GTOPO30**
10 m mesh digital elevation data
Data source
ASTER
Space shuttle radar
From organizations around the world that have DEM data
1:25,000 topographic map
Generation and distribution
METI/NASA
NASA/USGS
USGS
GSI
Release year
2009 ~
2003 ~
1996 ~
2008~
Data acquisition period
2000 ~ ongoing
11 days (in 2000)
Posting interval
30m
90m
1000m
about 10m
DEM accuracy (stdev.)
7~14m
10m
30m
5m
DEM coverage
83 degrees north ~ 83 degrees south
60 degrees north ~ 56 degrees south
Global
Japan only
Area of missing data
Areas with no ASTER data due to constant cloud cover (supplied
by other DEM)
Topographically steep area (due to radar characteristics)
None
None
Other examples of available DEMs- NED: with a resolution of 30
m, covering the entire U.S.A., provided by USGS
*SRTM3: Shuttle Radar Topography Mission Data at 3
Arc-Seconds**GTOPO30: Global 30 Arc-Second Elevation Data Set
Comparison between ASTER GDEM and SRTM3
Distinction from ASTER Level4Z DEM
ASTER Level4Z is provided for a given square of approximately 60
x 60 km corresponding to the scene acquired by ASTER. In contrast,
ASTER GDEM is developed based on a grid of 1 x 1 degree in latitude
and longitude and requires no scene selection or mosaicking.
About "ASTER" , an earth observing satellite sensor
What is ASTER?:An achievement from an international joint
project between the Ministry of Economy, Trade and Industry of
Japan (METI) and the National Aeronautics and Space Administration
(NASA)An earth observing sensor developed in Japan to be onboard
the satellite "Terra"In stable operation for more than 9 years
since its launch in December 1999What ASTER tells us:1) Surface
conditionThe sensor comprehensively captures spectral ranging from
visible to thermal-infrared (invisible to the human eye), and
offers detailed information on earth surface conditions (e.g.
vegetation, geological features) together with their
distribution.2) Surface temperatureDistribution of surface
temperature can be observed by the thermal infrared sensor. This
will be helpful to detailed studies of such phenomenon as the urban
heat island effect.3) DEMDEM is generated from a stereo-pair of
images acquired with nadir and backward angles over the same area.
ASTER GDEM will be developed based on this data.Reference about
ASTERASTER Ground Data System (ASTER GDS) ProjectASTER Science
Project
Areas of DEM applications
1. Stereoscopic visualization of satellite and other
two-dimensional images
Bird's-eye views and flight simulations can be generated by the
combined use of DEM data and satellite or map data.
2. Automated calculation of slope direction and angle, catchment
area, faults, etc.
Further achievements can be obtained by analyzing the DEM as a
platform in combination with other data. Some examples are shown
below.
* Disaster 1 (volcanic hazard map)
By a simulation using DEM as a platform, possible lava flow can
be estimated. Local authorities can provide more advanced "volcanic
hazard maps" that are crucial to ensure the safety of the
residents.
* Disaster 2 (flood hazard map)
By simulating a process of rainfall, catchment, runoff and
inundation using DEM as a platform, flood risk areas can be
estimated. Local authorities can provide advanced "flood hazard
maps" to the residents.
* Hydrology (water resource management)
Melted water is a valuable water resource in the oasis of
Xinjiang Uyghur Autonomous Region, China. By calculating water
catchment area using DEM, a potential water supply can be estimated
even for unmapped areas. The obtained result can be utilized for
water resource management in the oasis.
* Energy (oil resource exploration)
Oil source rock and reservoir formations are extracted from
ASTER data. Strike and dip of those formations are measured from
DEM, and a simulation of the underground geological structure will
reveal their prospective anticlinal structure. In this way, oil and
natural gas potentials can be evaluated without conducting a field
investigation, even in an area of conflict.
GDEM Data Use
- Intended users GDEM data will be distributed to any users
(individual/organization) who conduct work or research in 9
societal benefit areas (disaster, health, energy, climate, weather,
ecosystem, agriculture, and biodiversity) defined by GEOSS (Global
Earth Observation System of System).(Refer to GEOSS homepage URL:
http://www.epa.gov/geoss/)
- PriceGDEM data will be provided free of charge to the users
who utilize the data for the above purposes.
- User Registration and LoginTo obtain ASTER GDEM data, register
on ASTER GDEM Distribution site.
- Conditions of ASTER GDEM useWhen registering, it is required
to agree to the conditions of data use(Agreement for GDEM
distribution and data use), such as prohibition of secondary
distribution of GDEM original data, credit title obligation in the
case of displaying GDEM original data or the products produced by
GDEM on Internet, scientific journal or any other
publications.Follow the below instructions on credit title.To
display in the image"ASTER GDEM is a product of METI and NASA"To
include in writingClearly describe that the original data of ASTER
GDEM is the property of METI and NASA.
- ImmunityBecause there are known inaccuracies and artifacts in
the data set, please use the product with awareness of its
limitations.The data are provided "as is" and neither NASA nor
METI/ERSDAC will be responsible for any damages resulting from use
of the data.
- Information of Validation resultThe summary of validation on
ASTER GDEM is described in the Read Me which is attached to
downloaded data.-More detailed validation result is described in
Validation Report.
METI and NASA Release ASTER Global DEM
The Ministry of Economy, Trade, and Industry (METI) of Japan and
the United States National Aeronautics and Space Administration
(NASA) today jointly released Version 1 of the Advanced Spaceborne
Thermal Emission and Reflection Radiometer (ASTER) Global Digital
Elevation Model (GDEM). Previously, METI and NASA announced their
intent to contribute the ASTER GDEM to the Global Earth Observation
System of Systems (GEOSS). Consequently, the ASTER GDEM is
available at no charge to users worldwide via electronic download
from the Earth Remote Sensing Data Analysis Center (ERSDAC) of
Japan and from NASAs Land Processes Distributed Active Archive
Center (LP DAAC).
ASTER Global DEM
The ASTER instrument was built by METI and launched onboard
NASAs Terra spacecraft in December 1999. It has an along-track
stereoscopic capability using its near infrared spectral band and
its nadir-viewing and backward-viewing telescopes to acquire stereo
image data with a base-to-height ratio of 0.6. The spatial
resolution is 15 m in the horizontal plane. One nadir-looking ASTER
VNIR scene consists of 4,100 samples by 4,200 lines, corresponding
to about 60 km-by-60 km ground area.
The methodology used to produce the ASTER GDEM involved
automated processing of the entire 1.5-million-scene ASTER archive,
including stereo-correlation to produce 1,264,118 individual
scene-based ASTER DEMs, cloud masking to remove cloudy pixels,
stacking all cloud-screened DEMs, removing residual bad values and
outliers, averaging selected data to create final pixel values, and
then correcting residual anomalies before partitioning the data
into 1-by-1 tiles. It took approximately one year to complete
production of the beta version of the ASTER GDEM using a fully
automated approach.
The ASTER GDEM covers land surfaces between 83N and 83S and is
composed of 22,600 1-by-1 tiles. Tiles that contain at least 0.01%
land area are included. The ASTER GDEM is in GeoTIFF format with
geographic lat/long coordinates and a 1 arc-second (30 m) grid of
elevation postings. It is referenced to the WGS84/EGM96 geoid.
Pre-production estimated accuracies for this global product were 20
meters at 95 % confidence for vertical data and 30 meters at 95 %
confidence for horizontal data.
Initial studies to validate and characterize the ASTER GDEM
confirm that pre-production accuracy estimates are generally
achieved for most of the global land surface, although results do
vary and true accuracies do not meet pre-production estimates for
some areas. In addition, Version 1 of the ASTER GDEM does contain
certain residual anomalies and artifacts that affect the accuracy
of the product and may be impediments to effective utilization for
certain applications. Consequently, METI and NASA acknowledge that
Version 1 of the ASTER GDEM should be viewed as experimental or
research grade. Nevertheless, they are confident that the ASTER
GDEM represents an important contribution to the global earth
observation community.
ASTER GDEM tiles may be downloaded electronically from ERSDAC by
visiting http://www.gdem.aster.ersdac.or.jp/and from the LP DAAC by
visiting https://wist.echo.nasa.gov/~wist/api/imswelcome/.
Pre-release announcement (Jun.26,2009)
METI and NASA Announce Plans for ASTER Global DEM Release
The Advanced Spaceborne Thermal Emission and Reflection
Radiometer (ASTER) Global Digital Elevation Model (GDEM) was
developed jointly by the Ministry of Economy, Trade, and Industry
(METI) of Japan and the United States National Aeronautics and
Space Administration (NASA). Initial studies to validate and
characterize the ASTER GDEM recently were completed by NASA and
METI, in cooperation with the U.S Geological Survey (USGS) and the
Earth Remote Sensing Data Analysis Center (ERSDAC) of Japan, as
well as with support from the U.S. National Geospatial-Intelligence
Agency (NGA) and numerous other collaborators from around the
world.
ASTER Global DEM
Following review of the validation results, METI and NASA have
decided to jointly release the ASTER GDEM on June 29, 2009.
Previously, METI and NASA announced their intent to contribute the
ASTER GDEM to the Global Earth Observation System of Systems
(GEOSS). Upon release, the ASTER GDEM will be available at no
charge to users worldwide via electronic download from ERSDAC and
from NASAs Land Processes Distributed Active Archive Center (LP
DAAC) by visiting http://www.gdem.aster.ersdac.or.jp/ and
https://wist.echo.nasa.gov/~wist/api/imswelcome/, respectively.
The ASTER instrument was built by METI and launched onboard
NASAs Terra spacecraft in December 1999. It has an along-track
stereoscopic capability using its near infrared spectral band and
its nadir-viewing and backward-viewing telescopes to acquire stereo
image data with a base-to-height ratio of 0.6. The spatial
resolution is 15 m in the horizontal plane. One nadir-looking ASTER
VNIR scene consists of 4,100 samples by 4,200 lines, corresponding
to about 60 km-by-60 km ground area.
The methodology used to produce the ASTER GDEM involved
automated processing of the entire 1.5-million-scene ASTER archive,
including stereo-correlation to produce 1,264,118 individual
scene-based ASTER DEMs, cloud masking to remove cloudy pixels,
stacking all cloud-screened DEMs, removing residual bad values and
outliers, averaging selected data to create final pixel values, and
then correcting residual anomalies before partitioning the data
into 1-by-1 tiles. It took approximately one year to complete
production of the beta version of the ASTER GDEM using a fully
automated approach.
The ASTER GDEM covers land surfaces between 83N and 83S and is
composed of 22,600 1-by-1 tiles. Tiles that contain at least 0.01%
land area are included. The ASTER GDEM is in GeoTIFF format with
geographic lat/long coordinates and a 1 arc-second (30 m) grid of
elevation postings. It is referenced to the WGS84/EGM96 geoid.
Pre-production estimated accuracies for this global product were 20
meters at 95 % confidence for vertical data and 30 meters at 95 %
confidence for horizontal data. Initial validation studies
concluded that the ASTER GDEM generally meets the pre-production
accuracy predications, but results do vary and include areas where
GDEM accuracy does not meet the pre-production estimates.
The topography of the land surface is one of the most
fundamental geophysical measurements of the Earth, and it is a
dominant controlling factor in virtually all physical processes
that occur on the land surface. Topography of the land surface also
significantly controls processes within the overlying atmosphere,
and it reflects the processes within the underlying lithosphere.
Consequently, topographic information is important across the full
spectrum of earth sciences, and the availability of an up-to-date,
high resolution (1-arc-sec or less) global DEM has been a priority
of earth scientists for a long time. The ASTER GDEM, with 30m grid
postings and produced from a consistent primary data source, is
expected to meet the requirements of many users for global
topographic information.