AMSR-related Satellite Catalog:
GCOM-W (AMSR2 mounted)
Get to know AMSR and satellites -- Advanced Microwave Scanning Radiometer AMSR series
  • Global Observing Satellite for Greenhouse Gases and Water Cycle
    GOSAT-GW (AMSR3 mounted)
    [Under Development]
  • Global Change Observation Mission - Water "SHIZUKU"
    GCOM-W (AMSR2 mounted)
    [In Operation]
  • NASA Aqua Satellite
    Aqua (AMSR-E mounted)
    [AMSR-E Operation Completed]
  • Advanced Earth Observation Satellite-II "Midori II"
    ADEOS-II (AMSR mounted)
    [Operation Completed]
  • Marine Observation Satellite MOS-1 / MOS1b
    MOS-1 / MOS-1b (MSR mounted)
    [Operation Completed]
  • AMSR-related Satellite Catalog
  • GCOM-W
  • Overview

Global Change Observation Mission - Water "SHIZUKU"
GCOM-W (AMSR2 mounted)

Mission

GCOM-W / AMSR2
GCOM-W / AMSR2

The Global Change Observation Mission (GCOM) is a satellite project that aims to observe global environmental changes on Earth from space over a long period of time. GCOM-W "SHIZUKU" is responsible for observations related to the water cycle.

Since water on the earth plays an important role in the process of energy redistribution from the sun, a detailed study of water movement is essential to improve the prediction accuracy of climate change. The high-performance observation instrument (AMSR2) onboard GCOM-W has a large antenna with a diameter of about 2 m and can catch faint microwaves emitted from sea surface temperature, ocean wind speed, and water vapor in the atmosphere from an altitude of about 700 km. By analyzing these weak microwaves, we aim to elucidate climate change that causes extreme weather events using a variety of information.

  • SST

    Sea Surface Temperature

  • SND

    Snow Depth

  • SMC

    Soil Moisture Content

  • PRC

    Precipitation

  • CLW

    Cloud Liquid Water Content

  • SSW

    Sea Surface Wind Speed

about GCOM-W

GCOM-W will construct and demonstrate the use of a global-scale, long-term, continuous observation system that will provide the observational data necessary to elucidate the mechanisms of climate and water cycle change.

Specifically, GCOM-W will focus on the following areas: (1) changes in the cryosphere, including sea ice, ice sheets, and snow cover, which are considered to be the earliest and most obvious signs of global warming; (2) changes in sea surface temperature, precipitation, and water vapor associated with El Niño and other atmospheric-oceanic interactions; and (3) changes in the ocean surface, ocean surface, and land surface water and energy exchange, which are essential to understand the changes in these areas. The objective of this project is to observe physical quantities such as ocean winds and soil moisture, which are indispensable for understanding these changes, and to demonstrate their utilization in order to quantitatively understand the exchange of water, energy, and water vapor between the atmosphere, ocean, and land.

GCOM-W Objectives and Observation Targets
Global Warming and Global Environmental Change

Global Warming and Global Environmental Change: Examples of Weather-related Disasters

Distribution of Major Weather-related Disasters (2005)
Distribution of Major Weather-related Disasters (2005)
Authority: Japan Meteorological Agency, Climate Change Monitoring Report 2005
Distribution of Major Weather-related Disasters (2006)
Distribution of Major Weather-related Disasters (2006)
Source: Japan Meteorological Agency, Climate Change Monitoring Report 2006

In recent years, flood damage caused by large typhoons and torrential rains has been frequent. On the other hand, damage caused by abnormally low rainfall and heat waves has also been reported in many parts of the world. The Fourth Assessment Report (AR4) of the IPCC points out that these weather disasters are causally related to global warming caused by the increase in anthropogenic greenhouse gas concentrations in recent years. Greenhouse gas concentrations are expected to continue to increase in the future. It is necessary to accurately predict the future in order to determine trends in the occurrence of meteorological disasters and to consider adaptation measures.


Examples of Hydrological Cycle Changes Associated with Global Warming

Examples of Hydrological Cycle Changes Associated with Global Warming: Precipitation

Percentage change in precipitation from 2090-2099 (compared to 1980-1999 average)
Percentage change in precipitation from 2090-2099 (compared to 1980-1999 average)
Source: Ministry of the Environment, Summary of the Report of Working Group I of the Fourth Assessment Report of the IPCC (official version), May 22, 2007
An increase in mean annual precipitation is expected at high latitudes with a fairly high probability.
Similar increases are expected in East Africa, Central Asia, and the equatorial Pacific.
Many subtropical regions are likely to experience a decrease in mean annual precipitation (up to 20% below current levels).
The largest decreases are projected in the Mediterranean, the Caribbean, and the west coasts of subtropical climate regions on each continent

Necessity of Satellite Observation

Necessity of Satellite Observation

Upper-air observation
Upper-air observation
Satellite oobservation (microwave)
Satellite observation (microwave)

For example, meteorological elements such as temperature, pressure, wind speed and direction, humidity, and precipitation are indispensable for understanding current and future weather, climate change, and water cycles. Even if we try to observe these elements using only instruments that can directly measure them, such as ground-based meteorological instruments, radiosondes, and offshore buoys and ships, we cannot obtain information on their global distribution due to the infrequency of observations and limited observation area. In particular, data acquisition is almost impossible over the open ocean and in sparsely populated inland and polar regions where weather observation is scarce. Remote observation by satellite is the best way to obtain global meteorological and hydrological data with high frequency and high temporal resolution, including such areas where meteorological observation is not available.



What the GCOM-W mission aims to achieve
What the GCOM-W mission aims to achieve

What the GCOM-W mission aims to achieve

What the GCOM-W mission aims to achieve

We monitor and elucidate the water cycle in the Earth's surface layer, which is the driving force of global system change, through long-term and continuous quantitative observations, and contribute to the precise prediction of water cycle changes associated with global warming by assimilating the data into numerical models of weather and climate (global models, land surface models, cloud-resolving models, etc.) and verifying these models.


Water cycle observation by GCOM-W

Water cycle observation by GCOM-W

Water cycle observation by GCOM-W
Water Cycle on the Earth's Surface
The Earth is a rare "water planet" with an abundance of water in various forms.
It circulates in the Earth's surface layer with energy exchange through phase changes of gas, liquid, and solid, and is the driving force of global system changes ranging from climatic changes to climate change.
Predicted Impacts of Global Warming on the Hydrological Cycle
Changes in the cryosphere, such as reductions in sea ice and snow cover, associated with global warming.
Impacts on water resources and ultimately food resources due to changes in precipitation and snow cover.
Frequent extreme weather events such as heat waves and heavy rainfall, and larger and stronger typhoons.
Direct impact on human life.
Observation of water circulation changes by GCOM-W
Monitoring and clarification of global water circulation changes through long-term and continuous quantitative observations.
Assimilation and validation into improved numerical models of weather and climate (land surface models, cloud-resolving models, etc.) will contribute to precise prediction of water circulation changes associated with global warming.

  • AMSR-related Satellite Catalog
  • GCOM-W
  • Satellite Characteristics

Global Change Observation Mission - Water "SHIZUKU"
GCOM-W (AMSR2 mounted)

Satellite Specifications

International Designation Code 2012-025A
Launch Date May 18, 2012
Launch Vehicle H-IIA Launch Vehicle No. 21
Location Tanegashima Space Center
Shape 2 box shape with wing-type solar array paddles
Approx. 4.9m×3.0m×5.1m (Depth)
(Length between the tips of the paddles: 17.7 m)
Weight 1900 kg
Orbiter Sun-Synchronous Subrecurrent/ Recurrent
Altitude 700km
Inclination Approx. 98 degrees
Period 13:30±15min
  • AMSR-related Satellite Catalog
  • GCOM-W
  • AMSR2

Advanced Microwave Scanning Radiometer 2 (AMSR2)

AMSR2 Overview

World's Largest Revolving Space Antenna AMSR2

SHIZUKU (GCOM-W)

The Advanced Microwave Scanning Radiometer 2 (AMSR2,) which will be loaded onto the GCOM-W, is a sensor to observe radiometers, or microwaves emitted naturally from the ground, sea surface and atmosphere, using six different frequency bands ranging from 7 GHz to 89 GHz. The strength of a natural microwave is determined by its characteristics and moisture, including the surface condition and temperature of the material. Although it depends on the frequency, the microwave is very weak. AMSR2 will detect such weak microwaves at an altitude of 700 kilometers and measure the strength of them with a very high accuracy. For example, by measuring the strength of a microwave emitted from the sea surface with the AMSR2, we can understand the water temperature of the sea surface to an accuracy of 0.5 degrees Celsius.

The antenna of the AMSR2, which receives microwaves from the ground, arc scans the ground surface at a ratio of one turn every 1.5 seconds and observes an area approximately 1,450 kilometers wide in one scan. Using this scanning method, the AMSR2 can observe over 99 percent of the Earth's area in just 2 days. The diameter of the antenna is about 2 meters, making it the world's largest observation sensor aboard a satellite. The height of the rotating part is about 2.7 meters and the weight is about 250 kilograms. The AMSR2 can keep rotating such a large and heavy antenna at a speed of one turn per 1.5 seconds for 24 hours a day and more than five years without a minute of rest.

  • AMSR-related Satellite Catalog
  • GCOM-W
  • AMSR2 Spec.

Advanced Microwave Scanning Radiometer 2 (AMSR2)

AMSR2 Specifications

AMSR2 Specifications
Scan and rate Conical scan at 40 rpm
Antenna Offset parabola with2.0mφ
Swath width Nominal 1450 km, effective 1620 km
The performance guarantee range is ±61° scanning angle (1450km). The product contains data for a scanning angle of ±75° (1620km).
Incidence angle Nominal 55 °
Digitization 12 bits
Dynamic range 2.7 〜 340 K
Polarization Vertical and horizontal
AMSR2 Channel Set
Center Freq.
GHz
Band width
MHz
Pol. Beam width
degree
Ground res.
km
Sampling interval
km
6.925/7.3 350 V, H 1.8 35 x 62 10
10.65 100 1.2 24 x 42
18.7 200 0.65 14 x 22
23.8 400 0.75 15 x 26
36.5 1000 0.35 7 x 12
89.0 3000 0.15 3 x 5 5
  • AMSR-related Satellite Catalog
  • GCOM-W
  • Reference Material

Reference Material

Handbook, Format description

The AMSR2 handbook and format description are available in the "GCOM-W" section of the Globe Portal System (G-Portal).

Algorithm description

AMSR2 algorithm description (rev.B)