Ensemble Data Assimilation of GSMaP Precipitation with the - - PowerPoint PPT Presentation

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Ensemble Data Assimilation of GSMaP Precipitation with the - - PowerPoint PPT Presentation

Ensemble Data Assimilation of GSMaP Precipitation with the Nonhydrostatic Global Atmospheric Model NICAM Shunji Kotsuki 1 , Koji Terasaki 1 , Guo-Yuan Lien 1 , Takemasa Miyoshi 1,2 , and Eugenia Kalnay 2 1 Data


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Ensemble ¡Data ¡Assimilation ¡of ¡GSMaP ¡ Precipitation ¡with ¡the ¡Nonhydrostatic ¡ Global ¡Atmospheric ¡Model ¡NICAM

RIKEN-UMD Data Assimilation Conference, Oct 7, 2015@ UMD Shunji Kotsuki1, Koji Terasaki1, Guo-Yuan Lien1, Takemasa Miyoshi1,2, and Eugenia Kalnay2

1Data Assimilation Research Team, RIKEN-AICS, Japan 2University of Maryland, College Park, Maryland, USA

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Shunji Kotsuki

  • Postdoctoral Researcher
  • Background

– Doctor of Engineering at Kyoto-Univ., Japan (in 2013) – Hydrology & water resources

  • Prof. Miyoshi’s Team in RIKEN

– from Jan., 2014 – working on

  • Precipitation DA with NICAM-LETKF
  • Land data assimilation

River discharge simulation

Brief self introduction

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Outline

  • Introduction
  • Gaussian-Transformation
  • DA-cycle experiments
  • Forecast experiments
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Goals

  • To improve NWP using satellite-derived precipitation

data following Lien et al. (2013, 2015a, 2015b)

  • To produce a new precipitation product through data

assimilation

Improvement achieved with GFS-LETKF (U-wind @ 500 hPa) Li Lien en et et al. (2 (2015) ) Radiosondes ONLY Radiosondes+Precip. (No-Transform) Radiosondes+Precip. (Log-Transform) Radiosondes+Precip. (Gaussian-Transform)

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Experimental Setting

  • Numerical Model

– NICAM (Satoh and Tomita 2004, Satoh et al. 2008, 2014)

  • GL6 (approx. 110 km resolution)
  • Observations

– PREPBUFR: only upper sounding data (ADPUPA) – GSMaP/Gauge (Ushio et al. 2009)

  • with Gaussian transformation
  • Data assimilation

– LETKF (Hunt et al. 2007) – NICAM-LETKF (Terasaki et al. 2015) with 36 members

  • 3D-LETKF
  • Localization: 400 km for horizontal & 0.4 log(p) for vertical
  • Relaxation to prior perturbation (Zhang et al. 2004; α = 0.7)
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