Johansson, Daniel J. A.
O’Neill, Brian C.
Tebaldi, Claudia
Häggström, Olle
Article History
Received: 9 September 2014
Accepted: 3 February 2015
First Online: 30 March 2015
Change Date: 14 April 2015
Change Type: Corrigendum
Change Date: 10 June 2015
Change Type: Corrigendum
Change Details: In the version of this Letter originally published, in the third paragraph, the section of text including ‘Our analysis differs... at depths below 700m (refs 5,8,13).’ was unclear and should have been: 'Our analysis differs from previous methodologically related statistical estimates of ECS in that we distinguish observations of global mean near-land surface temperature (GMLST) from those of global mean sea surface temperature (GMSST) and use ocean heat content (OHC) observations continuous over time to a greater depth (2,000m instead of 700 m), a potentially important addition as heat accumulation during the hiatus is thought to be particularly strong at depths below 700m (refs 5,8,13).' Further, in the Methods section, radiative forcing should have been described as effective radiative forcing. These errors have been corrected in all versions of the Letter.
Change Details: In the version of this Letter originally published, ref. 9 was incorrectly cited twice; the sentence including the second occurrence should have read: "In contrast to other studies4, we find that the recovery from Mt Pinatubo is stronger than the cooling caused by the small volcanoes that has occurred since the early 2000s." This error has been corrected in the online versions of the Letter.
Competing interests
: The authors declare no competing financial interests.