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Corrigendum

Corrigendum 1AUGUST 2022 CORR IGENDUM 5233 a a AIDEN JÖNSSON AND FRIDA A.-M. BENDER Department of Meteorology and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden (Manuscript received 1 March 2022, in final form 31 May 2022) In the original article by Jonsson and Bender (2022) titled “Persistence and variability of Earth’s interhemispheric albedo symmetry in 19 years of CERES EBAF observations,” an error that was found in the code used to compute time averages reported in section 3a(2) (“Persistence of the symmetry”) left an incomplete year in the averages for the “post-hiatus” (PH) period (March 2013– February 2019). The time-mean hemispheric differences in individual components to the reflected short- wave (SW) radiation at the top of the atmosphere (TOA) that are presented in Fig. 3 of Jonsson and Bender (2022) are therefore incorrect; the corrected version of Fig. 3 is presented here. The spatial distribution of differences in mean F (atmospheric contributions to TOA reflected atm SW radiation) between the PH and the March 2000–February 2013 “hiatus” (H) period presented in Fig. 3b here are nearly the same as in Fig. 3b of Jonss ¨ on and Bender (2022), including the locations of areas with significant differences http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Climate American Meteorological Society

Corrigendum

Jönsson, Aiden; Bender, Frida A.-M.
Journal of Climate , Volume 35 (15): 2 – Aug 1, 2022
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References (1)

Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1520-0442
eISSN
1520-0442
DOI
10.1175/jcli-d-22-0128.1
Publisher site
See Article on Publisher Site

Abstract

1AUGUST 2022 CORR IGENDUM 5233 a a AIDEN JÖNSSON AND FRIDA A.-M. BENDER Department of Meteorology and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden (Manuscript received 1 March 2022, in final form 31 May 2022) In the original article by Jonsson and Bender (2022) titled “Persistence and variability of Earth’s interhemispheric albedo symmetry in 19 years of CERES EBAF observations,” an error that was found in the code used to compute time averages reported in section 3a(2) (“Persistence of the symmetry”) left an incomplete year in the averages for the “post-hiatus” (PH) period (March 2013– February 2019). The time-mean hemispheric differences in individual components to the reflected short- wave (SW) radiation at the top of the atmosphere (TOA) that are presented in Fig. 3 of Jonsson and Bender (2022) are therefore incorrect; the corrected version of Fig. 3 is presented here. The spatial distribution of differences in mean F (atmospheric contributions to TOA reflected atm SW radiation) between the PH and the March 2000–February 2013 “hiatus” (H) period presented in Fig. 3b here are nearly the same as in Fig. 3b of Jonss ¨ on and Bender (2022), including the locations of areas with significant differences

Journal

Journal of Climate – American Meteorological Society

Published: Aug 1, 2022

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