Impact Assessment of Himawari-8 AHI Data Assimilation in NCEP GDAS/GFS with GSI

Author:

Ma Zaizhong1,Maddy Eric S.2,Zhang Banglin3,Zhu Tong4,Boukabara Sid Ahmed5

Affiliation:

1. Joint Center for Satellite and Data Assimilation, and I. M. Systems Group, Inc., College Park, Maryland

2. Joint Center for Satellite and Data Assimilation, College Park, Maryland, and Riverside Technology, Inc., Fort Collins, Colorado

3. I. M. Systems Group, Inc., College Park, Maryland

4. Joint Center for Satellite and Data Assimilation, College Park, Maryland

5. Joint Center for Satellite and Data Assimilation, and NOAA/National Environmental Satellite, Data, and Information Service, College Park, Maryland

Abstract

AbstractAs the first of the next-generation geostationary meteorological satellites, Himawari-8 was successfully launched in October 2014 by the Japan Meteorological Agency (JMA) and placed over the western Pacific Ocean domain at 140.7°E. It carries the Advanced Himawari Imager (AHI), which provides full-disk images of Earth at 16 bands in the visible and infrared domains every 10 min. Efforts are currently ongoing at the National Oceanic and Atmospheric Administration (NOAA)/National Environmental Satellite, Data, and Information Service (NESDIS)/Center for Satellite Applications and Research (STAR) to assimilate Himawari-8 AHI radiance measurements into the National Centers for Environmental Prediction (NCEP) Gridpoint Statistical Interpolation analysis system (GSI). All software development within the GSI to allow for assimilation of Himawari-8 AHI radiance has been completed.This study reports on the assessment of AHI preassimilation data quality by comparing observed clear-sky ocean-only radiances to those simulated using collocated ECMWF analysis, as well as describing procedures implemented for quality control. The impact of the AHI data assimilation on the resulting analyses and forecasts is then assessed using the NCEP Global Forecast System (GFS). A preliminary assessment of the assimilation of AHI data from infrared water vapor channels and atmospheric motion vectors (AMVs) on top of the current global observing system shows neutral to marginal positive impact on analysis and forecast skill relative to an assimilation without AHI data. The main positive impact occurs for short- to medium-range forecasts of global upper-tropospheric water vapor. The results demonstrate the feasibility of direct assimilation of AHI radiances and highlight how humidity information can be extracted within the assimilation system.

Publisher

American Meteorological Society

Subject

Atmospheric Science,Ocean Engineering

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