JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-CG Complex & General

[A-CG46] [EE] Satellite Earth Environment Observation / Satellite Based Remote Sensing of Weather, Climate, and Environment

Sun. May 21, 2017 10:45 AM - 12:15 PM 104 (International Conference Hall 1F)

convener:Riko Oki(Japan Aerospace Exploration Agency), Allen A Huang(University of Wisconsin Madison), Gail Skofronick Jackson(NASA Goddard Space Flight Center), Yoshiaki HONDA(Center for Environmental Remote Sensing, Chiba University), Paul Chang(NOAA College Park), Chairperson:Nobuhiro Takahashi(Institute for Space-Earth Environmental Research, Nagoya University)

12:00 PM - 12:15 PM

[ACG46-30] Assimilation of cloudy infrared radiances of the geostationary Himawari-8 imager

★Invited papers

*NAOTAKA UEKIYO1, KOZO OKAMOTO1, DAISAKU UESAWA2, RYO YOSHIDA2, YUSUKE IOKA2 (1.Meteorological Research Institute/JMA, 2.Meteorological Satellite Center/JMA)

Keywords:satellite observation, Himawari-8, data assimilation, numerical weather prediction, cloudy observation

We introduce the current status of experiment of assimilating cloud-affected infrared observation
from a geostationary satellite, Hiamawari-8, into JMA global numerical weather prediction model.
Infrared observation data from geostationary satellites such as Himawari-8 are contributing
to improving analysis and forecast accuracy in numerical weather prediction.
However, cloud-affected observation data are rarely used in the practical assimilation system
due to the nonlinearity physical process in clouds, complex and non-Gaussian statistics and so on.
Assimilation of cloud-affected observation data is crucial for improving the accuracy of
analyses and forecasts in numerical weather prediction(NWP).
The radiance data to be assimilated were created by averaging pixels from the original radiances
(ASR, or All Sky Radiance), which was developped at Meteorological Satellite Center (MSC) in 2016.
In this study, we assimilated infrared radiances by assuming a single layer cloud ("simple cloud"),
in which cloud effect in radiative transfer is calculated simply by using the cloud-top pressure and an effective fraction of cloud.
The results of the experiments so far showed that even with this simple treatment, appropriately selected data offer valuable information not available from cloud-free observations.