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Corrigendum

Corrigendum JUNE 2021 C O R R I G E N D A 1135 a,b,c d c BENJAMIN A. SCHENKEL, ROGER EDWARDS, AND MICHAEL CONIGLIO Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, Oklahoma School of Meteorology, University of Oklahoma, Norman, Oklahoma NOAA/NSSL, Norman, Oklahoma NOAA/SPC, Norman, Oklahoma (Manuscript received 13 April 2021, in final form 30 April 2021) An error was discovered in the inadvertent inclusion of tropical cyclone (TC) motion from both the composite hodographs (Fig. 12) and vertical profiles of TC-relative tangential and radial winds (Fig. 13) computed from radiosondes sampling landfalling TCs in Schenkel et al. (2020). There are two primary reasons why TC motion should have been removed from these figures. First, the inclusion of TC motion makes it impossible to determine whether changes in the total wind field are due to the ambient or TC wind field when Fig. 12 and es- pecially Fig. 13 were focused on differences in the latter. Second, exclusion of TC motion is consistent with previous studies of TC tornadoes (McCaul 1991; Baker et al. 2009)and the response of the TC circulation to ambient deep-tropospheric vertical wind shear (VWS; Zhang et al. 2013; DeHart et al. 2014). http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Weather and Forecasting American Meteorological Society

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1520-0434
eISSN
1520-0434
DOI
10.1175/WAF-D-21-0055.1
Publisher site
See Article on Publisher Site

Abstract

JUNE 2021 C O R R I G E N D A 1135 a,b,c d c BENJAMIN A. SCHENKEL, ROGER EDWARDS, AND MICHAEL CONIGLIO Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, Oklahoma School of Meteorology, University of Oklahoma, Norman, Oklahoma NOAA/NSSL, Norman, Oklahoma NOAA/SPC, Norman, Oklahoma (Manuscript received 13 April 2021, in final form 30 April 2021) An error was discovered in the inadvertent inclusion of tropical cyclone (TC) motion from both the composite hodographs (Fig. 12) and vertical profiles of TC-relative tangential and radial winds (Fig. 13) computed from radiosondes sampling landfalling TCs in Schenkel et al. (2020). There are two primary reasons why TC motion should have been removed from these figures. First, the inclusion of TC motion makes it impossible to determine whether changes in the total wind field are due to the ambient or TC wind field when Fig. 12 and es- pecially Fig. 13 were focused on differences in the latter. Second, exclusion of TC motion is consistent with previous studies of TC tornadoes (McCaul 1991; Baker et al. 2009)and the response of the TC circulation to ambient deep-tropospheric vertical wind shear (VWS; Zhang et al. 2013; DeHart et al. 2014).

Journal

Weather and ForecastingAmerican Meteorological Society

Published: Jun 4, 2021

References