Authors

A data assimilation system for global atmospheric observations has been developed using an ensemble method. This system is composed of the Atmospheric General Circulation model for the Earth Simulator (AFES) and the Local Ensemble Transform Kalman Filter (LETKF). It assimilates global atmospheric ob...

Full description

Bibliographic Details
Main Authors: Takeshi Enomoto, Takemasa Miyoshi, Jun Inoue, Qoosaku Moteki, Miki Hattori, Shozo Yamane
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.4835
http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.405.4835
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.405.4835 2023-05-15T15:06:05+02:00 Authors Takeshi Enomoto Takemasa Miyoshi Jun Inoue Qoosaku Moteki Miki Hattori Shozo Yamane The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.4835 http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.4835 http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf Atmospheric General Circulation Model Ensemble Kalman Filter Observing System Experiment Atmospheric Predictability Optimization text ftciteseerx 2016-01-08T03:01:52Z A data assimilation system for global atmospheric observations has been developed using an ensemble method. This system is composed of the Atmospheric General Circulation model for the Earth Simulator (AFES) and the Local Ensemble Transform Kalman Filter (LETKF). It assimilates global atmospheric observations from public data archives efficiently on the Earth Simulator. The new architecture of the renovated Earth Simulator required re-optimization of AFES and LETKF. The dynamical core of the AFES has been optimized to run twice as fast. The optimized version of LETKF achieved a bump of more than three times. A stream from 1 January 2008 is being conducted to give preliminary results. Smoother fields in the polar regions are achieved by the updated LETKF. Predicted precipitation compares well with satellite observations. Analysis error estimated as analysis ensemble spread is used to evaluate atmospheric observations and to study atmospheric predictability. Observing system experiments are conducted to clarify the influence of pressure observations by Arctic drifting buoys and to identify the planetary-scale propagation of the impact of additional dropsonde observations in the Indian Ocean. Precursory signals are found in various atmospheric phenomena in which the analysis ensemble spread increases prior to the events. Text Arctic Unknown Arctic Indian
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Atmospheric General Circulation Model
Ensemble Kalman Filter
Observing System Experiment
Atmospheric Predictability
Optimization
spellingShingle Atmospheric General Circulation Model
Ensemble Kalman Filter
Observing System Experiment
Atmospheric Predictability
Optimization
Takeshi Enomoto
Takemasa Miyoshi
Jun Inoue
Qoosaku Moteki
Miki Hattori
Shozo Yamane
Authors
topic_facet Atmospheric General Circulation Model
Ensemble Kalman Filter
Observing System Experiment
Atmospheric Predictability
Optimization
description A data assimilation system for global atmospheric observations has been developed using an ensemble method. This system is composed of the Atmospheric General Circulation model for the Earth Simulator (AFES) and the Local Ensemble Transform Kalman Filter (LETKF). It assimilates global atmospheric observations from public data archives efficiently on the Earth Simulator. The new architecture of the renovated Earth Simulator required re-optimization of AFES and LETKF. The dynamical core of the AFES has been optimized to run twice as fast. The optimized version of LETKF achieved a bump of more than three times. A stream from 1 January 2008 is being conducted to give preliminary results. Smoother fields in the polar regions are achieved by the updated LETKF. Predicted precipitation compares well with satellite observations. Analysis error estimated as analysis ensemble spread is used to evaluate atmospheric observations and to study atmospheric predictability. Observing system experiments are conducted to clarify the influence of pressure observations by Arctic drifting buoys and to identify the planetary-scale propagation of the impact of additional dropsonde observations in the Indian Ocean. Precursory signals are found in various atmospheric phenomena in which the analysis ensemble spread increases prior to the events.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Takeshi Enomoto
Takemasa Miyoshi
Jun Inoue
Qoosaku Moteki
Miki Hattori
Shozo Yamane
author_facet Takeshi Enomoto
Takemasa Miyoshi
Jun Inoue
Qoosaku Moteki
Miki Hattori
Shozo Yamane
author_sort Takeshi Enomoto
title Authors
title_short Authors
title_full Authors
title_fullStr Authors
title_full_unstemmed Authors
title_sort authors
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.4835
http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf
geographic Arctic
Indian
geographic_facet Arctic
Indian
genre Arctic
genre_facet Arctic
op_source http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.4835
http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p055_Enomoto.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766337737316630528