2010
DOI: 10.3178/hrl.4.60
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Development of APHRO_JP, the first Japanese high-resolution daily precipitation product for more than 100 years

Abstract: Abstract:We constructed historical (1900-) high-resolution (0.05°× 0.05°) daily precipitation data over the Japanese land area as part of the product of the "Asian Precipitation -HighlyResolved Observational Data Integration Towards Evaluation of the Water Resources" (APHRODITE) project. This product APHRO_JP is derived from rain gauge observations and is intended to accurately represent both mean and extreme values. Due to new interpolation techniques developed in APHRODITE, estimation accuracy for orographic… Show more

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Cited by 135 publications
(101 citation statements)
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References 11 publications
(12 reference statements)
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“…Although R/A overestimates long-term precipitation (Fig. 1c), its short-term (hourly precipitation) quality is high because R/A is designed for disaster-prevention activities (Shimpo 2001b;Kamiguchi et al 2010 This study further confirmed the homogeneity of the 26-yr time series of the maximum hourly precipitation and the maximum SWI (Fig. 2).…”
Section: Methodssupporting
confidence: 67%
See 1 more Smart Citation
“…Although R/A overestimates long-term precipitation (Fig. 1c), its short-term (hourly precipitation) quality is high because R/A is designed for disaster-prevention activities (Shimpo 2001b;Kamiguchi et al 2010 This study further confirmed the homogeneity of the 26-yr time series of the maximum hourly precipitation and the maximum SWI (Fig. 2).…”
Section: Methodssupporting
confidence: 67%
“…6). These differences reach several tens of millimeters per hour which might be caused by the difference of dataset, such as overestimations included in the R/A dataset (Kamiguchi et al 2010). Other candidates are statistical periods, regional frequency analysis, and the uncertainty of estimation in Toyama and Mizuno (2002) and in this study (Fig.…”
Section: Resultsmentioning
confidence: 99%
“…The indices are defined by Frich et al (2002): the maximum number of consecutive dry days (CDD) and the simple daily precipitation intensity index (SDII; calculated by dividing Pav by the total number of wet days). The Pav distributions simulated by MRI-AGCM3.2S and NewRCM are in good agreement with that calculated from the 0.05 -mesh raingauge-based gridded daily precipitation data over the Japanese Islands (APHRO_JP; Kamiguchi et al 2010). MRI-AGCM3.2S simulates some spurious areas that are oversensitive to topography around the central mountainous regions of the Japanese Islands (Fig.…”
Section: Introduction Of the Spectral Nudging Methodssupporting
confidence: 66%
“…The spatial distribution of monthly precipitation was evaluated using data from the Asian Precipitation -Highly-Resolved Observational Data Integration Towards Evaluation of Water Resources (APHRODITE) project (Kamiguchi et al 2010;Yatagai et al 2012). The WRF model provides three-hourly integrated precipitation (mm 3h −1 ); therefore, simulated daily precipitation (mm day −1 ) was obtained by integration of these data and was then averaged to obtain monthly precipitation.…”
Section: Model and Numerical Setupmentioning
confidence: 99%