Status of GCOM-W1 development and expected meteorological applications

The Global Change Observation Mission (GCOM) consists of two polar orbiting satellite observing systems, GCOM-W (Water) and GCOM-C (Climate), and three generations to achieve global and long-term monitoring of the Earth. GCOM-W1 is the first satellite of the GCOM-W series and scheduled to be launched in Japanese fiscal year 2011. The mission instrument will be the Advanced Microwave Scanning Radiometer-2 (AMSR2), which is the successor instrument of AMSR on ADEOS-II and AMSR-E on EOS Aqua platform. Development of the GCOM-W1 system progresses favorably. The mechanical and thermal tests using the GCOM-W1 structural and thermal model were successfully completed. The GCOM-W1 and AMSR2 proto-flight models are under their proto-flight testing. In the middle of 2010, AMSR2 will be delivered to satellite system prior to the system proto-flight test of GCOM-W1. Retrieval algorithms are being developed by collaborating with principal investigators. Algorithm comparisons or integrations are now underway for several algorithms to find best available algorithms for post-launch processing. Also, maintaining and extending the validation sites such as the Mongolian Plateau site for soil moisture is being implemented. In addition to the long-term climate variability monitoring, meteorological applications will be the most important operational utilization of AMSR2 data. Currently, AMSR-E data are being used for numerical prediction through data assimilation at several meteorological agencies. Also, retrieved geophysical parameters such as sea surface temperature are being used for diagnostics of the weather and ocean variations.

[1]  Peter Bauer,et al.  Direct 4D‐Var assimilation of all‐sky radiances. Part I: Implementation , 2010 .

[2]  R. Oyama,et al.  Analysis of Tropical Cyclones Using Microwave Satellite Imagery , 2008 .

[3]  Mark A. Bourassa,et al.  NASA's Ocean Vector Winds Science Team Workshops , 2010 .

[4]  E. O'connor,et al.  The CloudSat mission and the A-train: a new dimension of space-based observations of clouds and precipitation , 2002 .

[5]  Kozo Okamoto,et al.  Operational status and recent developments on cloud and precipitation assimilation at JMA , 2010 .

[6]  Keiji Imaoka,et al.  The Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E), NASDA's contribution to the EOS for global energy and water cycle studies , 2003, IEEE Trans. Geosci. Remote. Sens..

[7]  Misako Kachi,et al.  Long-term observations of water and climate by AMSR-E and GCOM-W , 2009, Remote Sensing.

[8]  Timothy L. Olander,et al.  The Dvorak Tropical Cyclone Intensity Estimation Technique: A Satellite-Based Method that Has Endured for over 30 Years , 2006 .

[9]  Akira Shibata A wind speed retrieval algorithm by combining 6 and 10 GHz data from Advanced Microwave Scanning Radiometer: Wind speed inside hurricanes , 2006 .

[10]  Li Li,et al.  Global survey and statistics of radio-frequency interference in AMSR-E land observations , 2005, IEEE Transactions on Geoscience and Remote Sensing.

[11]  J. Comiso,et al.  Trends in the sea ice cover using enhanced and compatible AMSR‐E, SSM/I, and SMMR data , 2008 .

[12]  Misako Kachi,et al.  Global Change Observation Mission (GCOM) for Monitoring Carbon, Water Cycles, and Climate Change , 2010, Proceedings of the IEEE.