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Category Archives: Heavy Rain and Flooding Issues
Fall 2019 through Winter 2020 Heavy Precipitation Events
By Sheldon Kusselson ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Jan1503Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Jan1215Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Jan0309Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Feb1203Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Feb2103Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Oct1518Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Oct1615Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Oct3015Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Oct3115Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Dec2303Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2019Dec1715Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Mar0315Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Mar0415Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Mar0515Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Mar0515Advect_LPW_ALT_anim.gif ftp://ftp.cira.colostate.edu/ftp/Forsythe/LPW/Anim_GIF/2020Mar0615Advect_LPW_ALT_anim.gif
CIRA ALPW Comparison for Two Northeast US Heavy Precipitation Events
By Sheldon Kusselson ALPW loop of 2019 event: ALPW loop of 2017 event:
Subtropical storm Melissa
By Sheldon Kusselson and Dan Bikos Subtropical storm Melissa exists off the Eastern coastline of the U.S. on 10-11 October 2019, as GOES-16 visible imagery on 11 October shows: http://rammb.cira.colostate.edu/templates/loop_directory.asp?data_folder=training/visit/loops/11Oct19/vis&loop_speed_ms=60 note the lack of deep convection over the center of … Continue reading