ADEOS (Advanced Earth Observing Satellite), Japan
 


ADEOS

ADEOS (also known as "Midori" in Japanese) is a remote sensing satellite operated by the National Space Development Agency of Japan (NASDA) for global observation of land, ocean and atmospheric processes. ADEOS was launched on 17 August 1996. ADEOS was expected to acquire data on worldwide environmental changes such as the greenhouse effect, ozone layer depletion, deforestation and abnormal climactic conditions. The main imaging instruments on ADEOS are the high resolution AVNIR and the low resolution OCTS.

The satellite encountered several problems after launch. The satellite's mission ended in June 1997, after 10 months in operation, due to a breakdown of the solar panel array.

ADEOS is to be followed by ADEOS-2, initially scheduled to be launched in November 2001. The launch has since been postponed to a later date in 2002.


ADEOS-1 Orbit

Type Sun-Synchronous
Altitude 797 km
Period 101 min
Repeat Cycle 41 days

ADEOS-1 Sensors

  • OCTS (Ocean Colour and Temperature Sensor): OCTS is an optical radiometer developed by NASDA for global measurement of ocean colour and sea surface temperature. It has 8 bands in the visible and near-infrared region and 4 bands in the thermal region. OCTS data can be used for determination of the ocean primary production and carbon cycle and for getting information on ocean conditions for fishery and environmental monitoring.
  • AVNIR (Advanced Visible and Near Infrared Radiometer): AVNIR developed by NASDA is a high spatial resolution optical sensor for observing land and coastal zones in the visible and near-infrared regions. It has 4 spectral bands with a 16 m spatial resolution and 1 panchromatic band with an 8 m spatial resolution.
  • NSCAT (NASA Scatterometer): NSCAT is an active radar instrument developed by NASA's Jet Propulsion Laboratory (JPL), USA, for measurement of global wind speeds and directions over the ice-free oceans. It uses an array of antennas that radiate microwave pulses at Ku band (14 GHz frequency). Study using NSCAT data are expected to lead to improve methods of global weather forecasting and modeling.
  • TOMS (Total Ozone Mapping Spectrometer): TOMS is developed by NASA's Goddard Space Flight Center (GSFC) for measurement of total ozone spatial distribution.
  • POLDER (Polarization and Directionality of the Earth's Reflectances): POLDER is developed by the French Space Agency (CNES) for observation of the polarisation, directional and spectral characteristics of the solar light reflected by aerosols, clouds, oceans and land surfaces.
  • IMG (Interferometric Monitor for Greenhouse Gases)
  • ILAS (Improved Limb Atmospheric Spectrometer)
  • RIS (Retroreflector in Space)


ADEOS-2 Sensors

  • GLI (Global Imager): GLI is an optical sensor developed by NASDA, Japan. It observes the reflected solar radiation from the Earth's surface, including land, oceans and clouds and/or infrared radiation with a multi-channel system for measuring the biological content, such as chlorophyll, organic substance, and vegetation index as well as temperature, snow and ice, and cloud distribution. These data will be used for understanding the global circulation of carbon and climate changes. GLI has 36 bands in the visible-NIR, SWIR and thermal IR. The VNIR and SWIR bands have two resolution modes: 250 m and 1 km, while the thermal IR has a resolution of 1 km. GLI is an advanced version of the Ocean Color and Temperature Scanner (OCTS) on-board ADEOS.
  • AMSR (Advanced Microwave Scanning Radiometer): AMSR is a passive microwave radiometer. It detects microwave emissions from the Earth's surface and atmosphere. Various geophysical parameters, particularly those related to water, can be estimated from AMSR data. In addition to the conventional parameters, such as water vapor, precipitation, and sea surface wind speed, novel geophysical parameters, including sea surface temperature and soil moisture, are expected to be retrieved by using new frequency channels. AMSR is an eight-frequency, total-power microwave radiometer with dual polarization (except two vertical channels in the 50GHz band). Conical scanning is employed to observe the Earth's surface with a constant incidence angle. It carries an offset-parabolic antenna with a diameter of 2m, the largest space-borne microwave radiometer antenna of its kind.
  • SeaWinds (Sea Winds Scatterometer): NASA's SeaWinds Scatterometer is an active microwave scatterometer operating at 13.4 GHz microwave frequency. It is the continuation of NSCAT on board the ADEOS satelite. It will provide high accuracy wind speed and direction measurements over at least 90% of the ice-free global oceans every 2 days. SeaWinds will provide a continuing set of long term wind data for studies of ocean circulation, climate, air-sea interaction and weather forecasting.
  • POLDER (Polarization and Directionality of the Earth's Reflectances)
  • ILAS-2

Back to Main Index
 
Please send comments/enquiries/suggestions about this tutorial to Dr. S. C. Liew at scliew@nus.edu.sg Copyright © CRISP, 2001