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>2.0.CO;2 . Hong , X. , C. H. Bishop , T. Holt , and L. W. O’Neill , 2011 : Impacts of sea surface temperature uncertainty on the western North Pacific subtropical high (WNPSH) and rainfall . Wea. Forecasting , 26 , 371 – 387 , doi: 10.1175/WAF-D-10-05007.1 . Huddleston , J. N. , and B. W. Stiles , 2000 : A multidimensional histogram rain-flagging technique for SeaWinds on QuikSCAT. Proc. IEEE Int. Conf. on Geoscience and Remote Sensing Symp. 2000 , Honolulu, HI, Institute
>2.0.CO;2 . Hong , X. , C. H. Bishop , T. Holt , and L. W. O’Neill , 2011 : Impacts of sea surface temperature uncertainty on the western North Pacific subtropical high (WNPSH) and rainfall . Wea. Forecasting , 26 , 371 – 387 , doi: 10.1175/WAF-D-10-05007.1 . Huddleston , J. N. , and B. W. Stiles , 2000 : A multidimensional histogram rain-flagging technique for SeaWinds on QuikSCAT. Proc. IEEE Int. Conf. on Geoscience and Remote Sensing Symp. 2000 , Honolulu, HI, Institute
, experiments, and data a. Model description The Scripps Coupled Ocean–Atmosphere Regional (SCOAR) model ( Seo et al. 2007a , 2014 , 2016 ; http://hseo.whoi.edu/scoar ) is a regional coupled climate model that couples the Weather Research and Forecast (WRF; Skamarock et al. 2008 ) Model to the Regional Ocean Modeling System (ROMS; Haidvogel et al. 2000 ; Shchepetkin and McWilliams 2005 ). The interacting boundary layer is based on the bulk formula ( Fairall et al. 1996 ; 2003 ), which calculates the
, experiments, and data a. Model description The Scripps Coupled Ocean–Atmosphere Regional (SCOAR) model ( Seo et al. 2007a , 2014 , 2016 ; http://hseo.whoi.edu/scoar ) is a regional coupled climate model that couples the Weather Research and Forecast (WRF; Skamarock et al. 2008 ) Model to the Regional Ocean Modeling System (ROMS; Haidvogel et al. 2000 ; Shchepetkin and McWilliams 2005 ). The interacting boundary layer is based on the bulk formula ( Fairall et al. 1996 ; 2003 ), which calculates the
the accumulated storm-track value as the month proceeds. This yields a finescale temporal resolution metric that does not require copious model output. This filtering method can also be used on observations that are available only at a daily resolution (e.g., Guo et al. 2009 ). For one component of the analysis, we utilize the technique of Booth et al. (2010) to calculate an estimated surface storm track defined as the region of overlap of the upper quantiles of and T DIFF . Note that Booth
the accumulated storm-track value as the month proceeds. This yields a finescale temporal resolution metric that does not require copious model output. This filtering method can also be used on observations that are available only at a daily resolution (e.g., Guo et al. 2009 ). For one component of the analysis, we utilize the technique of Booth et al. (2010) to calculate an estimated surface storm track defined as the region of overlap of the upper quantiles of and T DIFF . Note that Booth
