Application of observability Gramian to targeted observation in WRF data assimilation

The optimal observation placement in weather forecast and research (WRF) data assimilation is investigated using a sensitivity analysis method. The method quantifies the sensitivity of observation location to assimilated results as an unobservability index. The empirical observability Gramian matrix...

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Main Authors: Ryoichi Yoshimura, Aiko Yakeno, Takashi Misaka, Shigeru Obayashi
Format: Article
Language:English
Published: Taylor & Francis Group 2020-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
wrf
Online Access:http://dx.doi.org/10.1080/16000870.2019.1697602
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spelling doaj-0f6b243fa55f457c85e28cca9e6985662021-02-18T10:31:39ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography1600-08702020-01-0172111110.1080/16000870.2019.16976021697602Application of observability Gramian to targeted observation in WRF data assimilationRyoichi Yoshimura0Aiko Yakeno1Takashi Misaka2Shigeru Obayashi3Institute of Fluid Science, Tohoku UniversityInstitute of Fluid Science, Tohoku UniversityNational Institute of Advanced Industrial Science and Technology (AIST)Institute of Fluid Science, Tohoku UniversityThe optimal observation placement in weather forecast and research (WRF) data assimilation is investigated using a sensitivity analysis method. The method quantifies the sensitivity of observation location to assimilated results as an unobservability index. The empirical observability Gramian matrix composed from a time series of WRF model outputs is used to obtain the unobservability index in the WRF domain. A three-dimensional variational data assimilation (3 D-VAR) method is employed in the WRF model to assimilate the observations of horizontal winds, whose locations are selected based on the unobservability index. The results from the identical-twin experiments show a correlation between improvement in the assimilated wind field and the magnitude of unobservability index. The temporal variation of the vertical component of vorticity is strongly related to the unobservability index, which confirms that an observation location exhibiting a high unobservability index contributes to error reduction in the data assimilation owing to the reduction in the uncertainty caused by the strong vorticity changes.http://dx.doi.org/10.1080/16000870.2019.1697602targeted observationweather forecastingobservabilitydata assimilationwrf
collection DOAJ
language English
format Article
sources DOAJ
author Ryoichi Yoshimura
Aiko Yakeno
Takashi Misaka
Shigeru Obayashi
spellingShingle Ryoichi Yoshimura
Aiko Yakeno
Takashi Misaka
Shigeru Obayashi
Application of observability Gramian to targeted observation in WRF data assimilation
Tellus: Series A, Dynamic Meteorology and Oceanography
targeted observation
weather forecasting
observability
data assimilation
wrf
author_facet Ryoichi Yoshimura
Aiko Yakeno
Takashi Misaka
Shigeru Obayashi
author_sort Ryoichi Yoshimura
title Application of observability Gramian to targeted observation in WRF data assimilation
title_short Application of observability Gramian to targeted observation in WRF data assimilation
title_full Application of observability Gramian to targeted observation in WRF data assimilation
title_fullStr Application of observability Gramian to targeted observation in WRF data assimilation
title_full_unstemmed Application of observability Gramian to targeted observation in WRF data assimilation
title_sort application of observability gramian to targeted observation in wrf data assimilation
publisher Taylor & Francis Group
series Tellus: Series A, Dynamic Meteorology and Oceanography
issn 1600-0870
publishDate 2020-01-01
description The optimal observation placement in weather forecast and research (WRF) data assimilation is investigated using a sensitivity analysis method. The method quantifies the sensitivity of observation location to assimilated results as an unobservability index. The empirical observability Gramian matrix composed from a time series of WRF model outputs is used to obtain the unobservability index in the WRF domain. A three-dimensional variational data assimilation (3 D-VAR) method is employed in the WRF model to assimilate the observations of horizontal winds, whose locations are selected based on the unobservability index. The results from the identical-twin experiments show a correlation between improvement in the assimilated wind field and the magnitude of unobservability index. The temporal variation of the vertical component of vorticity is strongly related to the unobservability index, which confirms that an observation location exhibiting a high unobservability index contributes to error reduction in the data assimilation owing to the reduction in the uncertainty caused by the strong vorticity changes.
topic targeted observation
weather forecasting
observability
data assimilation
wrf
url http://dx.doi.org/10.1080/16000870.2019.1697602
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AT aikoyakeno applicationofobservabilitygramiantotargetedobservationinwrfdataassimilation
AT takashimisaka applicationofobservabilitygramiantotargetedobservationinwrfdataassimilation
AT shigeruobayashi applicationofobservabilitygramiantotargetedobservationinwrfdataassimilation
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