One‐dimensional maximum‐likelihood estimation for spaceborne precipitation radar data assimilation

Spaceborne precipitation radar such as Global Precipitation Measurement (GPM)/dual‐frequency precipitation radar (DPR) provides valuable observations of precipitation systems in three dimensions. Assimilation of GPM/DPR data is becoming an important technique for improving the accuracy of forecastin...

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Bibliographic Details
Published inQuarterly journal of the Royal Meteorological Society Vol. 147; no. 735; pp. 858 - 875
Main Authors Ikuta, Yasutaka, Okamoto, Kozo, Kubota, Takuji
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.01.2021
Wiley Subscription Services, Inc
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Summary:Spaceborne precipitation radar such as Global Precipitation Measurement (GPM)/dual‐frequency precipitation radar (DPR) provides valuable observations of precipitation systems in three dimensions. Assimilation of GPM/DPR data is becoming an important technique for improving the accuracy of forecasting to complement scarce ground‐based observations. This study presents a new, one‐dimensional maximum‐likelihood estimation (1D‐MLE) method developed by the authors that enables the estimation of relative humidity profiles according to a non‐Gaussian probability density function. By assimilating the estimated relative humidity profiles using a four‐dimensional variational (4D‐Var) method, mesoscale precipitation forecasts by the Japan Meteorological Agency (JMA) have been considerably improved. The displacement of forecast precipitation during a severe weather event, in particular, is improved significantly. It was found that forecasting accuracy was maintained for a narrow GPM/DPR swath and low revisit frequency by repeating the assimilation–forecast cycle. Since the effectiveness was confirmed, the JMA began assimilating GPM/DPR data using the 1D‐MLE approach from March 2016. Spaceborne precipitation radar such as GPM/DPR provides valuable observations of three‐dimensional precipitation systems and complements scarce ground‐based observations. This study presents a new, one‐dimensional maximum‐likelihood estimation (1D‐MLE) method for effective assimilation of GPM/DPR that enables the estimation of relative humidity profiles according to a non‐Gaussian probability density function. By assimilating the estimated relative humidity profiles using 4D‐Var, mesoscale precipitation forecasts have been considerably improved.
Bibliography:Funding information
Japan Aerospace Exploration Agency,JAXA EO‐RA2
ISSN:0035-9009
1477-870X
DOI:10.1002/qj.3950