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Atsushi Hamada and Yukari N. Takayabu

Pacific at 0904 UTC 4 Jun 2014. Colors show reflectivity at the near-surface level (dB Z ). The number of precipitating pixels by setting the minimum detectable reflectivity to 12 and 18 dB Z is indicated in the right-top corner. (b) Horizontal winds at 850 hPa (black) and 500 hPa (red) at 1200 UTC, derived from the Interim European Centre for Medium-Range Weather Forecasts Re-Analysis (ERA-Interim) dataset ( Dee et al. 2011 ). (c) Along-track cross section of reflectivity at the 25th angle bin

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Eun-Kyoung Seo, Sung-Dae Yang, Mircea Grecu, Geun-Hyeok Ryu, Guosheng Liu, Svetla Hristova-Veleva, Yoo-Jeong Noh, Ziad Haddad, and Jinho Shin

representative of summer rainfall around the Korean Peninsula and in East Asia. A 24-h forecast was produced for each case. Initial and boundary conditions were derived from the National Centers for Environmental Prediction Final Analysis data ( Kanamitsu et al. 2002 ). All experiments involved one-way interactive triple-nested domains with a Lambert conformal map projection. The finest grid domain had a resolution of 2 km and was nested in a 6-km-resolution domain, which in turn was nested in an 18-km

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