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Corrigendum

Corrigendum NOVEMBER 2022 CO RR IG END U M 1835 a a a CAITLYN MCALLISTER, AARON STEPHENS, AND SHAWN M. MILRAD Meteorology Program, Applied Aviation Sciences Department, Embry-Riddle Aeronautical University, Daytona Beach, Florida (Manuscript received 17 August 2022, in final form 30 September 2022) The wet-bulb globe temperature (WBGT) calculation code that we used for our published article (McAllister et al. 2022) had a previously undiscovered temperature unit error in it, resulting in our original WBGT calculations being too low. This affected Figs. 5, 6, and 9, as well as Tables 3 and 5, for all of which we present corrected versions here. In general, the corrections make our trend analy- ses and results more robust and demonstrate that heat stress increases in Florida are even more pro- found than McAllister et al. (2022) originally showed. The results for heat index in McAllister et al. (2022) are completely unaffected. The changes to Figs. 5 and 6 and Table 3 (WBGT trends) are relatively minor and primarily affect WBGT magnitudes, which were previously underestimated. The trends and conclusions discussed in section 3b of McAllister et al. (2022) are largely unchanged, with the following notable exceptions: � Increases in daily maximum WBGT http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Applied Meteorology and Climatology American Meteorological Society

Corrigendum

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1558-8432
eISSN
1558-8432
DOI
10.1175/jamc-d-22-0130.1
Publisher site
See Article on Publisher Site

Abstract

NOVEMBER 2022 CO RR IG END U M 1835 a a a CAITLYN MCALLISTER, AARON STEPHENS, AND SHAWN M. MILRAD Meteorology Program, Applied Aviation Sciences Department, Embry-Riddle Aeronautical University, Daytona Beach, Florida (Manuscript received 17 August 2022, in final form 30 September 2022) The wet-bulb globe temperature (WBGT) calculation code that we used for our published article (McAllister et al. 2022) had a previously undiscovered temperature unit error in it, resulting in our original WBGT calculations being too low. This affected Figs. 5, 6, and 9, as well as Tables 3 and 5, for all of which we present corrected versions here. In general, the corrections make our trend analy- ses and results more robust and demonstrate that heat stress increases in Florida are even more pro- found than McAllister et al. (2022) originally showed. The results for heat index in McAllister et al. (2022) are completely unaffected. The changes to Figs. 5 and 6 and Table 3 (WBGT trends) are relatively minor and primarily affect WBGT magnitudes, which were previously underestimated. The trends and conclusions discussed in section 3b of McAllister et al. (2022) are largely unchanged, with the following notable exceptions: � Increases in daily maximum WBGT

Journal

Journal of Applied Meteorology and Climatology – American Meteorological Society

Published: Nov 15, 2022

References

  • Joint projections of U.S. East Coast sea level and storm surge
    Little, C. M.; Horton, R. M.; Kopp, R. E.; Oppenheimer, M.; Vecchi, G. A.; Villarini, G.
  • The heat is on: Observations and trends of heat stress metrics during Florida summers
    McAllister, C.; Stephens, A.; Milrad, S. M.