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supercell thunderstorms ( Apke et al. 2016 ). Textural patterns at cloud top have also been used to infer updraft strength ( Bedka and Khlopenkov 2016 ). In the presence of strong upper-level flow, some overshoots generate above-anvil cirrus plumes (AACP) downstream from the overshooting top as a result of internal gravity wave breaking and are apparent in visible satellite imagery ( Wang 2003 ; Wang et al. 2016 ; Homeyer et al. 2017 ; Bedka et al. 2018 ). AACPs in visible imagery are responsible for
supercell thunderstorms ( Apke et al. 2016 ). Textural patterns at cloud top have also been used to infer updraft strength ( Bedka and Khlopenkov 2016 ). In the presence of strong upper-level flow, some overshoots generate above-anvil cirrus plumes (AACP) downstream from the overshooting top as a result of internal gravity wave breaking and are apparent in visible satellite imagery ( Wang 2003 ; Wang et al. 2016 ; Homeyer et al. 2017 ; Bedka et al. 2018 ). AACPs in visible imagery are responsible for